オープンファイル

File No119：vol.127, no. 12

論説：泥ダイアピル周辺の砕屑岩脈の方位解析による広域応力と局所応力の検出：中新統田辺層群の例
安邊啓明・佐藤活志
（vol.127, no.12, p.709-725）

  • Appendix Table 1. Clastic dike data: lithofacies, sub-area, azimuth (clockwise angle from N after correction for declination), and dip.
  • Appendix Table 2. Paleostress analysis data: material, sub-area, detected stress name, azimuth and plunge, and mixing coefficient. Plots are shown in Figures 7–10.
 

File No118：vol.127, no. 12

論説：四国四万十帯カルサイト脈の同位体組成からみた沈み込み帯地震発生深度の流体の起源
内田菜月・村山雅史・松原友輝・坂口有人
（vol.127, no.12, p.701-708

  • Fig. A1. Locations of vein samples with annotations corresponding to sample numbers in Table 1. Base maps are partly modified from the Digital Topographic Map (Geospatial Information Authority of Japan).
 

File No117：vol.127, no. 11

論説：北上山地中西部の中古生代付加体を貫く白亜紀岩脈群の岩相・年代と貫入応 力解析から得られた引張場
内野隆之・羽地俊樹
（vol.127, no.11, p.651-666）

  • Table A1-A3. 
  • Table A1. Detailed information for dike outcrops. Abbreviations: ND (Nedamo Belt); NK (North Kitakami Belt); R. (River); and S. (Stream).
  • Table A2. Instrumentation for LA–ICP–MS analyses.
  • Table A3. U–Pb isotopic data for zircons recovered from the rhyolite. Abbreviations: 2nd st. (secondary standard zircon); and Disc. (discordant data).
 

File No116：vol.127, no. 10

論説：北部九州，尺岳北部に産する火成岩類の熱水変質作用と分化・集積作用を伴 う混合作用における組成変化
江島圭祐
（vol.127, no.10, p.605-619）

 

File No115：vol.127, no. 10

論説：四国西部中新統久万層群の酸性凝灰岩のジルコンU–Pb 年代
新正裕尚・折橋裕二
（vol.127, no.10, p.595-603）

  • Table S1. Summary of LA–ICP–MS operating conditions.
 

File No114：vol.127, no. 9

論説：貝形虫化石群集に基づく新潟県新津丘陵北部域の更新世の古環境変化
山田　桂・楠　慧子・飯田里菜・久須美晨夫
（vol.127, no.9, p.575-591）

  • Table S1. Occurrence list of fossil ostracods from the Niitsu Hills, Niigata Prefecture, central Japan.
 

File No113：vol.127, no. 9

論説：四国北西部，中新統久万層群明神層に含まれる火成岩礫の起源
相田和之・下岡和也・谷　健一郎・楠橋　直・齊藤　哲
（vol.127, no.9, p.563-574）

 

File No112：vol.127, no. 9

論説：湯ノ沢カルデラ，尾開山凝灰岩の高精度・高確度噴出年代の決定
田口春那・折橋裕二・佐々木実・宮嶋佑典・岩野英樹・平田岳史
（vol.127, no.9, p.545-561）

  • Table A1.Results of K–Ar age dating of the Obirakiyama Tuff, Yunosawa Caldera. Data sources: 1) Muraoka and Hase (1990); 2) Muraoka (1991); 3) Metal Mining Agency of Japan (1980); and 4) Nemoto (1998).
  • Fig. A1. Particle size distributions of zircon crystals recovered from five samples of the Obirakiyama Tuff, Yunosawa Caldera.
 

File No111：vol.127, no. 8

報告：九州南部の大隅花崗閃緑岩体に発達する節理系
有留千博・山本啓司
（vol.127, no.8, p.489-495）

  • Table A1. Strike and dip of joints in the Osumi granodiorite batholith. See Fig. 3 for location.
 

File No110：vol.127, no. 8

論説：山陰帯島根県雲南地域に分布する大東花崗閃緑岩の火成活動
野口将志・亀井淳志・鈴木博美・小林夏子
（vol.127, no.8, p.461-478）

　　Appendix 1-5.
  • Appendix 1. Lithofacies distribution within the study area. Base topographic map provided by the Geospatial Information Authority (GSI) of Japan [URL2].
  • Appendix 2. Whole-rock and modal compositions and values of magnetic susceptibility for the Daito granodiorite, Hiyodori granite, and Mue granite.
  • Appendix 3. EPMA data for plagioclase, hornblende, and biotite in the Daito granodiorite.
  • Appendix 4. EPMA data for magnetite in the Daito granodiorite.
  • Appendix 5. Partition coefficients and starting compositions utilized in the Rayleigh fractionation modeling.

 

File No109：vol.127, no. 8

論説：北部九州東部に分布する田川変成岩類の変成作用
柚原雅樹・清浦海里・日�睨�莉亜・外田智千・早坂康隆
（vol.127, no.8, p.447-459）

  • Appendix 1. LA-ICP-MS U-Pb age data for zircon samples from the Tagawa metamorphic rocks (sample 14060710).

 

File No108：vol.127, no. 7

レター：青森県南部，碇ヶ関カルデラ主要構成噴出物（虹貝凝灰岩）のジルコンLAICP- MS U–Pb 年代
相川裕貴・折橋裕二・佐々木　実・中尾魁史・高久雄一
（vol.127, no.7, p.431-436）

  • Appendix 1. Bulk chemical composition of the Nijikai Tuff (sample no. 09081301).
 

File No107：vol.127, no. 7

論説：近畿地方の瀬戸内区に分布する下–中部中新統の生層序と対比
入月俊明・柳沢幸夫・木村萌人・加藤啓介・星　博幸・林　広樹・藤原祐希・赤井一行
（vol.127, no.7, p.415-429）

Figs A1-A4
​Tables A1-A5

  • Table A1. List of fossil ostracods from the Ayugawa and Tsuzuki groups.
  • Table A2. List of fossil diatoms from the Ayugawa and Tsuzuki groups.
  • Table A3. List of fossil diatoms from the Yamabe and Yamagasu groups.
  • Table A4. List of fossil planktonic foraminifers from the Yamagasu Group.
  • Table A5. Data sources for the stratigraphic correlation (Fig. 6) among the selected groups of the Miocene in the Setouchi Geologic Province. Abbreviations: D (diatom), PF (planktonic foraminifera), CN (calcareous nannofossil), R (radiolarian), O (ostracod), Sr (strontium isotope dating), FT (fission track dating), U–Pb (U–Pb dating), and M (magnetostratigraphy).
  • Fig. A1. Photographs of diatom species from the Kaya Tuffaceous Mudstone Member of the Okuyamada Formation, Tsuzuki Group.
  • Fig. A2. Photographs of diatom species from the Yamabe and Yamagasu groups (part 1).
  • Fig. A3. Photographs of diatom species from the Yamabe and Yamagasu groups (part 2).
  • Fig. A4. Photographs of diatom species from the Yamabe and Yamagasu groups (part 3).  
 

File No106：vol.127, no. 6

論説：新島（燃島）の後期更新世末期–完新世の石灰質微化石群集と鹿児島湾奥の古 環境復元
前浜悠太・鹿野和彦・大木公彦・入月俊明・林　広樹
（vol.127, no.6, p.363-376）


Tables A1-A3

  • Table A1. List of fossil benthic foraminifera species in each sample.
  • Table A2. List of fossil planktonic foraminifera species in each sample.
  • Table A3. List of fossil ostracod species in each sample.
 

File No105：vol.127, no. 6

巡検案内書：岐阜県西部・揖斐川町春日地域の火成岩と接触変成岩
榎並正樹・纐纈佑衣・加藤丈典・壷井基裕・丹羽健文
（vol.127, no.6, p.313-331）


Tables S1-S2

  • Table S1. Representative analyses of major constituent minerals in a basic nodule collected from Stop 1d.
  • Table S2 . Whole-rock compositions of lamprophyre collected from Stop 3.
 

File No104：vol.127, no. 5

レター：Discovery of Early Permian tonalite from the high P/T Triassic Suo Metamorphic Complex, Eastern Yamaguchi Prefecture, SW Japan
Kenta Kawaguchi et al
（vol.127, no.5, p.293-304）


Tables S1-S4

  • Table S-1. LA-ICP-MS zircon U–Pb data of consistency standard sample YO1.
  • Table S-2. LA-ICP-MS zircon U–Pb data of three tonalite mylonite samples.
  • Table S-3. LA-ICP-MS detrital zircon U–Pb data of psammitic schist sample.
  • Table S-4. XRF whole-rock chemical compositions of the four tonalite mylonite samples.
 

File No103：vol.127, no. 4

レター：熊本県天草市，前島花崗閃緑岩のジルコンU–Pb 年代
長田充弘・大藤　茂
（vol.127, no.4, p.237-243）


Fig. A1.Tables A1-A2

  • Fig. A1. a) Microphotograph of sample MGD-02 (crosspolarized light). Afs: Alkali feldspar, Bt: biotite, Pl: plagioclase, Qtz: quartz. b) Cathodoluminescence images of the concordant zircons separated from sample MGD-02. The diameter of each spot (with the spot number) is 25 μm. The yellow scale bar is 50 μm.
  • Table A1. The LA-ICPMS analytical conditions for U–Pb dating in this study.
  • Table A2. The U–Pb zircon data in this study. C (D): concordant (discordant) data.
 

File No102：vol.127, no. 2

論説：緑色普通角閃石の主成分および微量成分元素組 成による美浜テフラと四国沖MD012422 コアから検出されたクリプトテフラとの対比と 給源の推定．
古澤　明・佐々木俊法・後藤憲央
（vol.127, no.2, p.91-103）

  • Appendix 1. Glass composition data for StHz and ATHOG of MPI-DING. Abbreviations: average (Av.), standard deviation (SD), uncertainty at 95% confidence level (U), and number of analyses (n). Preferred value data are from Jochum et al. (2006).
 

File No101：vol.127, no. 2

論説：秋田県出羽山地の笹森丘陵に分布する新第三系の地質と珪藻 化石層序
加藤悠爾・柳沢幸夫
（vol.127, no.2, p.105-120）

　　　Table A1. List of diatoms used for diatom bathymetric index Bd2.
　　　Tables A2–A18. Occurrence charts of diatoms from stratigraphic sections A–Z.
 

File No100：vol.127, no. 1

レター：赤石山地中央部の小渋川地域に分布する陸源砕屑岩から得られた前期白亜紀 最末期の砕屑性ジルコン
志村侑亮・中村佳博・常盤哲也・杉本大志・水戸創也
（vol.127, no.1, p.51-58）

　　　Appendixs 1-2
  • Appendix 1. Cathodoluminescence images of concordant zircon grains from samples 17112505 (a–d), OS2-30 (e–i), and 17112502 (j–m). Scale bars are 20 μm. Circles show the locations of analytical spots. Ages of detrital zircons ≤ 1200 Ma and >1200 Ma are 238U–206Pb and 207Pb/206Pb ages, respectively, in Ma. Age uncertainties are given at the 1 σ level.
  • Appendix 2. Analytical operating conditions for LA-ICPMS U–Pb isotopic dating. Appendix 3. LA-ICP-MS U–Pb isotopic data. Discordant data are shaded gray.
 

File No99：vol.127, no. 1

論説：フィッション・トラック熱年代解析およびU–Pb 年代測定に基づいた南九 州せん断帯に分布する破砕帯の活動時期
末岡　茂・島田耕史・照沢秀司・岩野英樹・檀原　徹・小北康弘・平田岳史
（vol.127, no.1, p.25-39）

 

File No98：vol.127, no. 1

論説：八幡浜大島に分布する大島変成岩体のジルコンU–Pb 年代と地体構造上の意義
小山内康人・北野一平・中野伸彦・足立達朗・米村和紘・吉本　紋・宮下由香里・米虫　聡・小松正幸
（vol.127, no.1, p.1-24）

 

File No97：vol.126, no. 11

報告：愛知県設楽地域東部の貫入岩体の全岩化学組成，輝度および変質度
図子田和典・岡村太路・二村康平・束田和弘・竹内　誠
（vol.126, no.11, p.645-654）

  • Appendixs 1-2 
  • Appendix 1.  Photographs of polished surfaces of the samples versus distance from the samples Ft1, Sh1, and Tb1. Ft: Futto; Sh: Shimohara; Tb: Tochibata.
  • Appendix 2.  Whole-rock chemical composition of the trace lements in Futto and Tochibata samples.
  •  

File No96：vol.126, no. 11

レター：紀伊半島西部，和泉層群最上部からの古第三系の発見
磯��行雄・長谷川　遼・益田晴恵・堤　之恭 （vol.126, no.11, p.639-644）

  • Appendix 1.  Methods for zircon separation and U–Pb dating.ジルコン分離およびU–Pb 年代測定手法の説明．
  • Appendix 2.  Example Cathodo-luminescence images of detrital zircons with oscillatory zoning (from Sample KRH) . オシラトリー累帯構造を持つ砕屑性ジルコンのCL像の例（試料KRH）．
  • Appendix 3.  U–Pb age. U–Pb 年代．（Table A1. Sample KRH．試料KRH．/Table A2. Sample MJK．試料MJK．/Table A3. Sample SGD．試料SGD．/Table A4. Sample NTK．試料NTK．/Table A5. Sample TKO2．試料TKO2．/Table A6. Sample SB1．試料SB1．/Table A7. Sample SB2．試料SB2．/Table A8. Sample CCO．試料CCO．/Table A9. Sample SBR．試料SBR．）Table A10. Summary of the youngest age clusters for dated zircons in the nine sandstone samples (n = number of grains). 砂岩９試料中のジルコンが持つ最若年代集団のまとめ (n は粒子数).
  • Appendix 4. Tera-Wasserburg diagrams of U–Pb ages for zircons from all nine sandstone samples. 砂岩９試料中のジルコンU–Pb 年代のコンコーディア図．
  • Appendix 5.  Measurements of secondary standard sample (OD-3). 二次標準試料（OD-3）の測定値．
  •  

File No95：vol.126, no. 11

レター：天草下島北部の中新世貫入岩体の方向と応力解析
牛丸健太郎・山路　敦
（vol.126, no.11, p.631-638）

  • Appendix 1. Locations and orientation data (dip direction and dip) for sheet intrusions and bedding.
 

File No94：vol.126, no. 10

レター：北海道神居古潭変成岩類班渓幌内ユニットからの新たなジルコンU–Pb年代
長田充弘・大藤　茂
（vol.126, no.10, p.597-601）

  • Fig. A1, Tables A1-A2
  • Fig. A1.  a) Photomicrograph (cross-polarized light; scale bar is 300 μm) of sample PKP2 (pelitic schist). Abbreviations Chl: chlorite, Ms: muscovite, Q-A: quartz and albite. b) Cathodoluminescence (CL) images of zircon grains from sample PKP2 with 206Pb/238U ages. Yellow open circles show measurement spots (25 μm). Scale bar is 50 μm. c) Concordia diagram of sample PKP2. Red solid and blue open circles denote concordant and discordant grains, respectively. Abbreviations N: number of concordant and discordant zircon grain. d) Probability density plot of all data (bin width is 50 million year). Abbreviations n: number of concordant zircon grain, YSG: youngest single grain 206Pb/238U age.
  • Table A1. LA-ICPMS analytical conditions for U–Pb dating based on Kouchi et al. (2015).
  • Table A2. The U–Pb zircon data for secondary standard zircons (91500 and OD-3) and sample PKP2. 206Pbc: common 206Pb (%). R: Rejected data, C (D):Concordant (discordant) data.．
 

File No93：vol.126, no. 10

論説：東京都産古生代前期造山帯の断片：関東山地東部， 黒瀬川帯高圧型変斑れい岩および花崗岩類のジルコンU–Pb 年代
沢田　輝・磯��行雄・坂田周平
（vol.126, no.10, p.551-561）

  • Open Online Table 1. Analytical results of zircon U–Pb dating by LA-ICP-MS. Values for f206 indicate the fractional amount of common Pb and those of Conc. indicate concordance between 207Pb/235U and 206Pb/238U ages (%). LA–ICPMS によるジルコンU–Pb 年代測定の結果．f206は測定された206Pb のうちのコモン鉛の割合を示し，Conc. は 207Pb/235U 年代と206Pb/238U 年代の一致率を示す．
 

File No92：vol.126, no. 9

論説：草津白根火山，本白根火砕丘群の地質と形成史
石崎泰男・濁川　暁・亀谷伸子・吉本充宏・寺田暁彦
（vol.126, no.9, p.473-491）

  • Appendix 1-2(PDF)
  • Appendix 1. Sampling locations for whole-rock chemical analyses. Numbers in parentheses correspond to outcrop numbers in Figures 2 and 3.
  • Appendix 2. Whole-rock chemical and modal compositions of the eruption products of the Motoshirane Pyroclastic Cone Group. Sampling locations are shown in Appendix 1. Modal compositions were determined by pointcounting to a total of ~2000 point for each sample. Phenocrysts were defined as those measuring >0.2 mm along their longest axis. Total Fe is expressed as Fe2O3. Loss on ignition (LOI) was measured by igniting the powdered samples at 900°C for 2 h. Abbreviations: Dw = densely welded lava-like section; JB = jointed block; SC = scoria; BB = breadcrust bomb; tr = present in samples but not observed in point counts; nd = not detected.
 

File No91：vol.126, no. 9

論説：鹿児島湾奥，新島に露出す る最上部更新統〜完新統の層序と起源
鹿野和彦・柳沢幸夫・内村公大・奥野　充・中村俊夫
（vol.126, no.9, p.519-535）

  • Figs. S1-S4, Tables S1-S4 
  • Table S1. Occurrence chart of diatoms in the uppermost Pleistocene to Holocene sediments exposed on Shinjima Island.
  • Table S2. List of molluscan fossils collected from the Moeshima Shell Bed, Location 1, and from the Lower Shinjima Silt Bed, Location 3.
  • Table S3. Refractive indices of constituent minerals in the Southern Shinjima Pumice, Shinjima Pumice, and Sakurajima– Satsuma tephra Sz-14.
  • Table S4. Bulk chemical compositions of pumice samples collected from the Moeshima Shell Bed and from the Sz- 12 (S-BP) and Sz-13 (S-AP) tephras at Location 1.
  • Fig. S1. Comparison of previous stratigraphy with the proposed divisions.
  • Fig. S2. Photomicrographs of diatom slides. Scale bar = 50 μm. A = Assemblage F (Sample 12050402, Shinjima Pumice, Location 2); B = Assemblage F (Sample SJ12-01, Shinjima Pumice, Location 4); C = Assemblage F (Sample 15012009, Southern Shnjima Pumice, Location 1); D = Assemblage FM (Sample 12071607, Sz-13 tephra, Location 1); E = Assemblage M (Sample 12070401-1, Upper Shinjima Silt Bed, Location 1); F = Assemblage M (Sampleple 12050411, Lower Shinjima Silt Bed, Location 4). Assemblage F = Freshwater diatom assemblage with very rare marine diatoms, Assemblage FM = Mixed assemblage of freshwater and marine diatoms. Assemblage M = Marine diatom assemblage with rare brackish to freshwater diatoms.
  • Fig. S3. (A) Photograph taken on August 20, 2013 showing the succession from the Shinjima Pumice to the Moeshima Shell Bed exposed at Location 4. The gravelly tuffaceous deposit is ~2.8 m thick. This outcrop is almost completely covered by vegetation. (B) Photograph taken in 1975, showing a normal fault displacing the exposed succession at the same location. Photograph courtesy of Kimihiko Oki.
  • Fig. S4. Photohraph taken on January 21, 1994, showing the succession from the Southern Shinjima Pumice to the Moeshima Shell Bed, exposed at Location 1. The gravelly tuffaceous deposit is ~1.8 m thick. This large outcrop is covered by an embankment, talus, and thick vegetation.
  • Fig. S5. Harker diagrams for the pumices from the Moeshima Shell Bed and the Sz-12 (S-BP) and Sz-13 (SAP) tephras. Numbers 1–8 correspond to the last digit of the sample numbers shown in Table S4. The major element compositions of Sz-5, 7, 8, 9, 10, and 11 and those of Sz-14 are adopted from Takahashi et al. (2011) and Yamamoto et al. (2013).

File No90：vol.126, no. 5

論説：九州北部福岡県筑豊炭田の始新統直方層群下部のジルコンU–Pb 年代
宮田和周・長田充弘・仁木創太・服部健太郎・大林秀行・平田岳史・大藤　茂
（vol.126, no.5, p.251-266）

  • Appendix 1. Photomicrographs of the tuff and tuffaceous rocks (a–d) of the Sanjakugoshaku Formation in plane-polarized (left) and cross-polarized light (right). (a), SARUTA, a tuffaceous mudstone including numerous glass shards; (b), HONDA, a laminated tuffaceous mudstone; (c), MIYAWAKA, a vitric tuff; (d), EBITSU, a vitric tuff including rhyolitic volcanic fragments. Abbreviations: Pl = plagioclase; Qtz = quartz; V = volcanic fragment.
  • Appendix 2. Cathodoluminescence images of the selected zircon grains from the tuff and tuffaceous rocks of the Sanjakugoshaku Formation and 238U–206Pb ages. The circles indicate the spots analyzed via LA-ICPMS.
  • Appendix 3. Analytical settings and standard materials for U–Pb zircon dating.
    Appendix 4. U–Pb zircon data of the tuff and tuffaceous samples from the Sanjakugoshaku Formation, Nogata Group, and standard zircon in this study. Abbreviations: C = concordant grain; D = discordant grain.
  •  

File No89：vol.126, no. 5

報告：新潟県に分布する7 枚の第四紀テフラのLA-ICP-MS によるジルコンU–Pb 年代
伊藤久敏・村松敏雄
（vol.126, no.5, p.285-290）

  • Fig. A1. Locations and outcrop photographs for sampled tephras. a) HK10, b) Odaira, c) Og, d) Yokokura, e) Kimigaeri,
    f) Oguriyama, g) Shimizu Pass. Topographic maps are from the Geospatial Information Authority of Japan.
  • Table A1. LA-ICP-MS zircon U–Pb analytical results for the Niigata tephras. Data in italics (>75% common Pb contamination or >2 Ma) were excluded for further U–Pb analyses.
   

File No88：vol.126, no. 4

論説：埼玉県加治丘陵に分布する下部更新統仏子層の層序と年代の再検討
納谷友規・水野清秀
（vol.126, no.4, p.183–204）

  • Appendix 1.Occurrence of diatoms in the Bushi Formation. 
  • Appendix 2.List of typical tephras and chemical compositions of volcanic glass shards with low TiO2–MgO and high K2O contents in Lower Pleistocene deposits, central Japan.
 

File No87：vol.126, no. 4

報告：紀伊半島中央部に分布する四万十帯白亜系東川コンプレックスから得られた砕屑性ジルコンU–Pb 年代
志村侑亮ほか
（vol.126, no.4, p.223–230）

  • Appendix 1.LA-ICP-MS U–Pb isotopic data. Discordant data are shown in gray color. 206Pbc: common 206Pb (%).
 

File No86：vol.126, no. 3

報告：草津白根火山，白根火砕丘群，弓池マールおよび逢ノ峰火砕丘の岩石学的特徴
亀谷伸子ほか
（vol.126, no.3, p.157-165）

  • Appendix 1.  Whole-rock compositions and modal compositions. Total Fe expressed as Fe2O3. For plotting on Harker diagrams (Fig. 5), FeO* was calculated as FeO + (0.8998×Fe2O3). Mineral and groundmass (glass + microphenocryst + microlite) abundances are in vol% (calculated on a vesicle-free basis) based on >2000 point counts. Loss on ignition (LOI) was measured by igniting the powdered samples at 900°C for 2 h. Abbreviations: Vol. Bl.: volcanic block; tr: present in samples but not observed in point counts; n.d.: not detected.
  •  

File No85：vol.126, no. 3

論説：富士山東方で1.1kaに発生した大規模火山性斜面崩壊
山元孝広ほか
（vol.126, no.3, p.127-136）

  • Supplement 1.Results of major elements composition analysis for volcanic glasses by Energy Dispersive X-ray Spectrometry. 161212c ＝ Kozushima-Tenjyosan tephra. OYM-03-01, g-sample and g1-1 ＝ volcanic glass shards in OYM03. エネルギー分散型エックス線分析による火山ガラスの主成分 組成測定結果．161212c ＝神津島天上山テフラ．OYM-03- 1, g-sample 及びg1-1 ＝ OYM03 中の火山ガラ
  •  

File No84：vol.126, no. 3

論説：三重県志摩半島の黒瀬川帯蛇紋岩中ドレライト岩塊の地球化学と起源
内野隆之
（vol.126, no.3, p.113-125）

  • Appendix Table.  Whole-rock major- and trace-element geochemical data for standard samples (certified reference materials). “Measured” indicates values analyzed in this study, and“ certified” indicates known certified values
  •  

File No83：vol.125, no. 11

報告：赤石山地中央部に分布する秩父帯付加体の砕屑性ジルコンU–Pb 年代
杉本大志ほか
（vol.125, no.11, p.827-832）

  • Appendix 1-5. LA-ICP-MS U–Pb isotopic data. Analyses shown in italics are discordant data. All errors are quoted as 1σ.
  •  

File No82：vol.125, no. 11

論説：富山県に分布する太美山層群のジルコンU–Pb年代
金子一夫ほか
（vol.125, no.11, p.781-792）

  • Appendix. U–Pb isotopic data of the unknown zircon samples and zircon standards (Nancy 91500 and OD- 3). (C) concordant data set; (D) discordant data set; (IC) data from a spot containing an inclusion or a crack; (R) data from a spot containing resin or data from a zircon grain that detached from the resin during laser ablation. Data shown in italics (D, IC, and R in the column labelled “Remarks”) were rejected before calculation of isotopic ages
  •  

File No81：vol.125, no. 9

ノート：看板・新聞折り込み広告と教科書における地図の北を表す記号の使用と大学生の理解
廣木義久
（vol.125, no.9, p.699-705）

File No80：vol.125, no. 9

論説：Excel のソルバー機能を利用した熱力学計算方法：重心座標系の化学式を用いた熱力学計算への適用例
久田公一
（vol.125, no.9, p.635-654）

 

File No79：vol.125, no. 7

論説：富山県八尾地域の新生界年代層序の再検討とテクトニクス
中嶋　健・岩野英樹・檀原　徹・山下　透・柳沢幸夫・谷村好洋・渡辺真人・佐脇貴幸・中西　敏・三石裕之・山科起行・今堀誠一
（vol.125, no.7, p.483-516）

 

File No78：vol.125, no. 6

報告：飛驒山地加賀沢の花崗岩類のジルコンU–Pb 年代
竹内 誠・柴田 賢・カ スイ・山本鋼志
（vol.125, no.6, p.453-459）

  • Appendix 1. U–Pb isotopic data for zircons analyzed in this study. All errors are 2σ. Analyses shown with shading are discordant and are not included in the probability density plots and histograms.

File No77：vol.125, no. 6

報告：愛媛県久万高原町の三波川変成岩類中に新たに見つかった“粗粒な”変塩基性岩体
仲田光輝・楠橋 直・齊藤 哲・大藤弘明・奈良正和
（vol.125, no.6, p.447-452）

  • AFig. S1-Table S2 
  • Fig. S1. Geological route map around the outcrops of the metabasite body. The location of this area is shown in Fig. 1.
  • Fig. S2. Rock sections. (a–d) Color images of (a–d) of Fig.3. (e–i) Metabasite clasts sampled from the basal conglomerate of the Hiwadatoge Formation unconformably overlying the metabasite at outcrop NMMGB003.(j) Metabasite clast sampled from the basal conglomerate of the Hiwadatoge Formation exposed at Nakajo. The location of the outcrop is indicated by the white star (B) in Fig. 1. The scale bars equal 1 cm. 
  • Fig. S3. Photomicrographs of a metabasite sample collected at outcrop NM-MGB002 under (a, c, e, g) plane-polarized  light and (b, d, f, h) cross-polarized light. (a, b) Color images of (a, b) of Fig. 4. The scale bars for (a,b), (c, d) and (e, f) equal 1 mm, and that for (g, h) equals 0.5 mm. Abbreviations: Act, actinolite; Al, albite; Mtx, matrix; Ppc, “ porphyroclast”; Ttn, titanite, Zo, zoisite.
  • Table S1. SEM-EDS data (wt%) for minerals within the metabasite samples collected from outcrop NMMGB002 and the basal conglomerate of the Hiwadatoge Formation (outcrop NM-MGB003; samples NM-HTFg116 and 310). Abbreviations: Chl, chlorite; Phn, phengite; Ttn, titanite.“ –” indicates below the detection limit.
  • Table S2. Whole rock chemical composition (wt%) for the metabasite samples collected from outcrop NMMGB002 and the basal conglomerate of the Hiwadatoge Formation (outcrop NM-MGB003; samples NM-HTFg099 and 100) quantified by XRF.
  •  

File No76：vol.125, no. 6

論説：北部九州白亜紀花崗岩類，添田花崗閃緑岩のU–Pb ジルコン年代とSr・Nd 同位体比組成：添田花崗閃緑岩の再区分
柚原雅樹・亀井淳志・川野良信・岡野 修・早坂康隆・加々美寛雄
（vol.125, no.6, p.405–420）

  • Appendix 1. Whole-rock chemical compositions of the hornblende porphyritic facies of the Irahara Granodiorite.
  •  

File No75：vol.125, no. 5

論説：紀伊半島中央部に分布するジュラ紀秩父付加体と白亜紀四万十付加体の境界周辺の地質構造と 砕屑性ジルコンU–Pb 年代
志村侑亮・常盤哲也・竹内　誠・山本鋼志
（vol.125, no.5, p.349-365）

  • Appendix 1. LA-ICP-MS U–Pb isotopic data. Rejected data are shown in gray color. 206Pbc: common 206Pb (%).
  •  

File No74：vol.125, no. 5

論説：紀伊半島中央部高原川地域の白亜紀付加コンプレックスの砕屑性ジルコンU–Pb 年代
太田明里・竹内　誠・ナドミド バヤルト・山本鋼志
（vol.125, no.5, p.329-347）

  • Appendix 1. U–Pb isotopic data of zircons analyzed in this study. All errors are 2σ. Analyses shown with a shadow are discordant and are not included in the probability density plots and histograms.
  •  

File No73：vol.125, no. 4

論説：岐阜県高山市本郷地域における飛騨外縁帯の砕屑岩層から得られた砕屑性ジルコンのU–Pb 年代とその意義： 森部層およびジュラ系堂殿層（新称）の堆積年代
鈴木敬介・栗原敏之・植田勇人
（vol.125, no.4, p.307-322）

  • Supplementary Figure 1. Map showing the location of sandstone samples selected for petrographic analyses and U–Pb detrital zircon dating (except for sample 0609-03) in the Hongo area.
  • Supplementary Table 1. U–Pb zircon dating results. Abbreviations:Ra = age ratio; σc = concordance error; SE =standard error.
  • Supplementary Table 2. Results of U–Pb zircon dating on the Plešovice standard. Abbreviations: Ra = age ratio;σc = concordance error; SE = standard error.
  •  

File No72：vol.125, no. 4

論説：出羽山地東縁，秋田県角館町周辺の上部漸新統および中新統の層序
細井　淳・工藤　崇・羽地俊樹・岩野英樹・檀原　徹・平田岳史
（vol.125, no.4, p.279-295）

 

File No71：vol.125, no. 2

報告：日高変成帯南部，黄金道路沿いに露出するかんらん石ノーライトの岩石学的特徴
志村俊昭・小島 萌・大橋美由希・山根幹生・Anthony I. S. Kemp
（vol.125, no.2, p.195-200）

  • Table A1. Whole rock chemical compositions and, Sr and Nd isotope ratios of the olivine norite.
 

File No70：vol.125, no. 2

論説：U–Pb zircon dating of the Sanbagawa metamorphic rocks in the Besshi–Asemi-gawa region, central Shikoku, Japan, and tectonostratigraphic consequences.
Aoki, K., Seo, Y., Sakata, S., Obayashi, H., Tsuchiya, Y., Imayama, T., Yamamoto, S. and Hirata, T
（vol.125, no.2, p.183–194）

  • Table A1. LA-ICP-MS U–Pb concordia data from zircon analyses.
 

File No69：vol.125, no. 2

論説：山口県東部、柳井地域に産する領家帯蒲野花崗閃緑岩のマグマ過程． 
池田雄輝・大和田正明・西塚 大・亀井淳志
（vol. 125，no. 2, 167–182）

  • Table A1-A4
  • Table A1. Representative chemical compositions of garnet. FeOT: total Fe. Alm=100*Fe/(Fe+Mn+Mg+Ca), Sps=100*Mn/(Fe+Mn+Mg+Ca), Pyr=100*Mg/(Fe+Mn+Mg+Ca), Grs=100*Ca/(Fe+Mn+Mg+Ca).
  • Table A2. Representative chemical compositions of plagioclase. FeOT: total Fe. An=100*Ca/(Ca+Na+K), Ab=100*Na/(Ca+Na+K), Or=100*K/(Ca+Na+K). Positions from A to A’ correspond to the analytical points shown in Fig. 7.
  • Table A3. Representative chemical composition of biotite.  FeOT: total Fe. Mg# = 100*Mg/(Fe+Mg).
  • Table A4. Representative chemical composition of hornblende. FeOT: total Fe. Mg# = 100*Mg/(Fe+Mg).
 

File No68：vol.125, no. 1

論説：房総半島に分布する上総 層群の広域テフラ−特に上総層群下部におけるテフラ層序と新たな対比−
田村糸子・水野清秀・宇都宮正志・中嶋輝允・山崎晴雄
（vol.125, no.1, p.23-39）

  • Open File(PDF): Sampling locality maps based on the 1:25,000 topographic maps “Onjuku” (a–d), “Kazusa-Ohara” (e), and “Katsuura” (f and g) of the Geographical Survey Institute, Japan.
  •  

File No67：vol.124, no. 12

報告：Geochemical database of Japanese islands for basement rocks: compilation of domestic article
Satoru Haraguchi, Kenta Ueki, Kenta Yoshida, Tatsu Kuwatani, Mika Mohamed, Shunsuke Horiuchi and Hikaru Iwamori
（vol.124, no.12, p.1049-1054）

  • ppendix A (pdf). Articles compiled in the DODAI until the end of 2017.
  • Appendix Table 1 (pdf). Characteristics of worldwide databases, some domestic databases, and the DODAI. (The numbers of references and samples were compiled from EarthChem until the end of 2017).
  • Appendix Table 2 (csv). Compiling geochemical data of DODAI.
 

File No66：vol.124, no. 12

総説：美濃帯層状チャートの堆積寄稿に関する3つの問題
尾上哲治（vol.124, no.12, p.1021-1032）

  • PDF (1.9MB)
    補遺：上部三畳系層状チャートの主要元素分析結果について
  • Fig. A1. Geologic and location maps of the study sections along the Kiso River, central Japan. Modified after Wakita (1988).
  • Fig. A2. Field occurrence of Late Triassic bedded chert at Sakahogi in the Inuyama area in the Mino Belt, Japan. (a) lower Upper Norian (lower Sevatian; Epigondolella bidentata conodont zone) bedded chert. (b) upper Upper Norian (upper Sevatian; Misikella hernsteini conodont zone) bedded chert. Scale bars, 5 cm.
  • Table A1. Major element data for samples from the Sakahogi section. Major element compositions of the Sakahogi chert and claystone samples normalized to 100 wt%.
  • Table A2. Analytical results of major element in reference material (JCh-1) by XRF.
 

File No65：vol.124, no. 11

論説：三重県に分布する中新統一志層群上部の浮遊性有孔虫・珪藻化石層序
大信田彦磨・林　広樹・柳沢幸夫・栗原行人・星　博幸
（vol.124, no.11, p.919-933）

  • Appendix 1. Map showing sample localities. Base map is a topographic map downloaded from the Geospatial Information Authority of Japan (GSI; http://www.gsi.go.jp).
 

File No64：vol.124, no. 11

報告：New geochemical data for back-arc basin basalts from DSDP Leg 58 Sites 442–444 and the ODP Leg 131 Site 808, Shikoku Basin Keywords: Shikoku Basin, back-arc basin basalt, DSDP Leg 58 Site 442–444, ODP Leg 131 Site 808, recent analytical technique
Satoru Haraguchi, Koichiro Fujinaga, Kentaro Nakamura, Yasuhiro Kato, Asuka Yamaguchi, and Teruaki Ishii
（vol.124, no. 11, p.935-940）

Appendix

  • Appendix A. Analytical Methods.
  • Appendix Table 1. Bulk rock composition of samples estimated using XRF for DSDP Leg 58 Sites 442–444 and ODP Leg 131 Site 808.
  • Appendix Table 2. Bulk rock composition of samples estimated using ICP-MS for DSDP Leg 58 Sites 442–444 and ODP Leg 131 Site 808.
 
  •  
 

File No63：vol.124, no. 10

論説：栃木県北部，福島県南部に分布する中期更新世火砕流堆積物群の層序
山田眞嵩・河合貴之・西澤文勝・鈴木毅彦
（vol.124, no. 10，p.837-855）

  • Appendix. Major-element contents of volcanic glass shards obtained by EDS measurement.
 

File No62：vol.124, no. 10

論説：岩手県西和賀町に分布するグリーンタフのジルコンFT およびU–Pb 年代とその意味
細井　淳・中嶋　健・檀原　徹・岩野英樹・平田岳史・天野一男
（vol.124, no. 10，p.819-835）

  • Table A1. Summary of zircon U-Pb data by LA–ICP–MS.
  • Table A2. Summary of zircon FT data.
  •  

File No61：vol.124, no. 9

論説：日本海拡大以来の日本列島の堆積盆テクトニクス
中嶋　健
（vol.124, no. 9，p.693-722）

  • Fig. S1-S2(PDF)
  • Fig. S1. Chronostratigraphic correlations, including inferred paleostress regimes and tectonic events, for the Hokuriku district and the Toyama Trough. The geomagnetic timescale is after ATNTS2012 (Gradstein et al., 2012). Diatom biostratigraphy is after Yanagisawa and Akiba (1998). The Intra Lower Teradomari Unconformity Horizon (ILTU) is after Muramoto et al. (2007).
  • Fig. S2. Tectonostratigraphic and paleoenvironmental relationships in the Sea of Japan from the middle Miocene to the early Pliocene (compiled from: Hanagata et al., 2001; Japanese Association for Petroleum Technology, 2014; Nakajima, 2013; and Sato et al., 1991). The planktonic foraminifera zonation is from Blow (1969) and Maiya (1978), the benthic foraminifera zonation from Maiya (1978), and the nannofossil zonation from Martini (1971) and Sato et al. (1991). Abbreviations: F.O., First occurrence; L.O., Last occurrence; PFSS, Planktonic Foraminiferal Sharp Surface (after Maiya and Inoue, 1981).
 

File No60：vol.124, no. 7

論説：赤石山地四万十帯白亜系赤石層群から得られた砕屑性ジルコンU-Pb年代
常磐哲也・市谷和也・志村侑亮・竹内　誠・山本鋼志
（vol.124, no. 7，p.539-544）

  • Appendix1-5 (PDF)
  • Appendix 1-5. LA-ICP-MS U–Pb isotopic data. Analyses shown in italics are discordant data.
 

File No59：vol.124, no. 6

論説：火山ガラスの主成分および微量元素組成による鹿児島市永田川河口部で掘削 されたボーリングコアに挟まれる火砕流堆積物の識別
古澤　明・大木公彦・宮脇理一郎
（vol.124, no. 6，p.435-447）

  • Appendix1(PDF 681KB)
  • Appendix 1. Glass composition data for Aira-Tn tephra and ATHO-G of MPI-DING Reference Glasses. Av., average; SD, standard deviation; U, uncertainty at the 95% confidence level; n, number of analyses. Preferred values are from Jochum et al. [2006].
     

File No58：vol.124, no. 4

論説：岩手火山における最近1万年間の爆発的噴火履歴の再検討：水蒸気噴火とマグマ噴火の時空間的関連
伊藤順一・濱崎聡志・川辺禎久
（vol.124, no. 4，p.271-296）

  • Appendix1-4(PDF 3.6MB)
  • Appendix 1. XRD diagram.
  • Appendix 2. XRD peak intensities (cps and relative ratio) for analyzed samples. Sm: smectite (peak position is 2θ = 5.4°), Pyr: pyrophyllite (2θ= 9.3°), Kln: kaoline minerals (2θ = 12.3°), Crs: cristobalite (2θ = 21.7°), Qtz: quartz (2θ = 26.6°), Na-Alu: natroalunite (2θ = 30.1°). Peak position and intensity were analyzed using Peak Search for indows (ver. 6.1, Rigaku Corporation).
  • Appendix 3. Log(thickness) versus square root of isopach area for magmatic tephra and pyroclastic surge deposits, with best-fit lines through the data used to calculate the eruption volume. Isopach maps for Iw-W6 c and d, Iw-W6 a and b, Iw-W5, Iw-OdS, Iw-W2b-2, Iw-W2b-1, and Iw-OkS are shown in Fig. 9, and isopachs for Iw-W9, Iw-W8a, Iw-SuS, Iw-SuSr, Iw-KSr, and Iw-KS are from Doi (2000).
  • Appendix 4. List of coefficient of the equation, obtained from linear fits to data using the thickness-dispersion area coordinates in Appendix 3. Eruption volumes for each tephra are calculated after Fierstein and Nathenson (1992). Pyroclastic surge deposits Iw-KSr and Iw-SuSr are plotted alongside (straight lines). A specific gravity of 1.0 is used for scoria fall deposits, 1.5 for fine ash and volcanic sand deposits, and 1.2 for ash and scoria. Eruption ages for each deposit are summarized in Table 4.
 

File No57：vol.124, no.2

論説：2014 年の長野県神城断層地震の前後における新潟県十日町市室野泥火山の溶存ガス濃度と炭素同位体比の変化
柿崎喜宏・シュナイダー グレン・棚橋　学・石田直人・松本　良
（vol.124, no. 2，p.127-140）

  • Open File. 1(mp4 18.4MB） Video taken at the gas-venting crater of Murono mud volcano at ~03:00 PM, 22 November 2014 (~7 hours prior to the 2014 Kamishiro Fault Earthquake). This gasventing crater is also shown in Fig. 1D. This video was taken from the same locality as Open File 2.
  • Open File 2(mp4, 24.8MB)  Video taken at the gas-venting crater of Murono mud volcano at ~09:00 AM, 23 November 2014 (~11 hours following the earthquake).
 

File No56：vol.123, no.12

ノート：走査型X 線分析顕微鏡と画像処理・解析ソフトウェアを用いたモード測定
植木忠正・丹羽正和
（vol.123, no. 12，p.1061-1066）
Appendixs

  • Appendix 1. Example of measurement conditions.
  • Appendix 2. Original data from the element distribution image as measured with an X-ray microscope (XGT-5000).
  • Appendix 3. Comparison with measured values obtained using the point-counting method.
 

File No55：vol.123, no.12

報告：兵庫県北部，山陰海岸ジオパーク猿尾滝付近の中期中新世ラコリス
羽地俊樹・山路　敦
（vol.123, no12，p.1049-1054）
Figs & Tables

  • Fig. A1. Photographs of the Saruodaki Falls. (a) Upper and lower parts of the falls. The rectangle indicates the location of the image in (b). (b) Horizontal sub-layers of the intrusive body, which are recognized by their fracture patterns.
  • Fig. A2. Photomicrographs of mounted zircon grains from the Tsukuriyama Laccolith (top) and the 20 zircons analyzed for U–Pb dating (bottom).
  • Table A1. LA-ICP-MS FT age data of zircons from the Tsukuriyama Laccolith sample.
  • Table A2. LA-ICP-MS U–Pb age data of zircons from the Tsukuriyama Laccolith and a secondary standard (OD-3).
  • Table A3. LA-ICP-MS FT age data of zircons from the Tsukuriyama Laccolith sample.
 

File No54：vol.123, no.12

論説：三重県志摩半島，秩父累帯北帯白木層群の泥岩から得られた中期ジュラ紀放散虫化石と地質対比
内野隆之・鈴木紀毅
（vol.123, no12，p.1015-1033）
Appendix

  • Appendix. Route maps of the radiolarian fossil locations. (A) Location R1, Isobedani River, (B) Location R2, Tsuiji River, (C) Location R3, west of the Kamiji Dam, (D) Location R4, Gochi–Erihara forest road, (E) Locations R5 and R6, Gochi River. C: coherent facies, GATL: Gokasho–Arashima Tectonic Line, R.: river.
 

File No53：vol.123, no.11

論説：紀伊半島中央部に分布する四万十帯白亜系麦谷層の地質と砕屑性ジルコンU-Pb年代
志村侑亮・常磐哲也・竹内　誠・山本鋼志
（vol.123, no11，p.925-937）
Appendix

  • LA–ICP–MS U–Pb isotopic data. Rejected data are shown in gray color, not used in the analyses of the probability density plot and histogram. 206Pbc: common 206Pb.
 

File No52：vol.123, no.10

総説：島弧-大陸地殻深部現象の研究進展：超高温変成作用の精密解析
小山内康人・中野伸彦・足立達朗
（vol.123, no10，p.879-906）
Figs. S1-S4, Table S1

  • Fig. S1. Distribution of the Napier Complex in the Enderby Land and geological map of the Tonagh Island (modified after Osanai et al., 1999a).
  • Fig. S2. Distribution of the Highland Complex in Sri Lanka (modified after Osanai et al., 2016a).
  • Fig. S3. Distribution of the metamorphic complexes in the Kontum Massif (modified after Osanai et al., 2008).
  • Fig. S4. Geological map of the Higo metamorphic Belt (modified after Osanai et al., 2016a).
  • Table S1. Publication list for article on UHT rocks written by Japanese research group.
 

File No51：vol.123, no.9

論説：レーザーアブレーションICP質量分析装置を用いた火山ガラスの分析による十和田カルデラ起源大不動テフラと八戸テフラの識別
古澤　明
（vol.123, no.9，p.765-776）
Appendix 1.
Appendix 1. Analyttical result of AT tephra and ATHO-G glass shards for major element compositions using EDX and trace elemental concentration in AT tephra and ATHO-G glass shards determined by LA-ICP-MS. Av.: average, SD: standard deviation, U: uncertainty at 95% confidence level,n: number of an

File No50：vol.123, no.9

総説：地質温度計圧力計の最近の進展I：変成温度圧力の数値解析
川嵜智佑
（vol.123, no.9，p.699-706）
Supplementary programme 1，2，3
Supplementary programme 1に交点とその誤差を計算 するFORTRAN77 プログラム“Intersection”を載せた． Supplementary programme 2，3 に最小2 乗法を用いた 変成温度圧力とその誤差，任意のP–T 曲線の交点とその誤 差，交点の平均値とその誤差を計算するFORTRAN77 プ ログラム“Weight-free P–T estimate”と“Weighted P–T estimate”を与えた．

File No49：vol.123, no.5

論説：ジルコンU–Pb 年代からみた下部ジュラ系来馬層群の堆積年代
竹内　誠・常盤哲也・熊崎直樹・横田秀晴・山本鋼志
（vol.123, no.5，p.335-350）
Appendix 1.
U–Pb isotope data for zircons analyzed in this study. All errors are 2s. %conc = 100･(238U–206Pb age)/(235U–207Pb age) is a measure of concordance between 238U–206Pb and 235U–207Pb ages. Shading indicates discordant data that are not included in the probability density plots or histograms.
 

File No48：vol.123, no.1

報告：Petrography and whole-rock major and trace element analyses of igneous rocks from Iheya North Knoll, middle Okinawa Trough, SIP Expedition CK14-04 (Exp. 907)
Toru Yamasaki
（vol.123, no.1，p.23-29）
Appendix Table 1 Analytical results of reference materials.
Appendix A: Methods

 

File No47：vol.122, no.12

論説：山形県庄内砂丘に挟まれる2 層の古津波堆積物
山野井　徹・門叶冬樹・加藤和浩・山田　努・鎌田隆史・今野　進
Two tsunami deposits in the Shonai Sand Dunes, northeast Japan
（vol.122, no.12，p.637-652）
Appendix 1. Radiocarbon ages obtained for dateable materials from the event deposits.
 

File No46：vol.122, no.12

論説：紀伊半島に分布する四万十帯凝灰質砂岩の砕屑性ジルコンのU–Pb 年代とその意義
常盤哲也・竹内　誠・志村侑亮・太田明里・山本鋼志
U–Pb ages of detrital zircon from the tuffaceous sandstone of the Shimanto Belt in the Kii
Peninsula
（vol.122, no.12，p.625-635）
Appendix 1〜5. LA-ICP-MS U–Pb isotopic data. Analyses shown in italics are discordant data（probability ≦ 0.1）, and are not included in the probability density pot and histogram.
All errors are quoted at 2σ. 206Pbc：common 206Pb.
 

File No45：vol.122, no.10

論説：岩石学的にみた沼沢火山におけるマグマ溜りの長期的進化とカルデラ形成噴火の準備過程
増渕佳子・石崎泰男・白井智仁・松本亜希子・宮坂瑞穂・中川光弘
Petrological investigation of long-term evolution of magma chambers and preparing processes of caldera-forming eruption, Numazawa volcano, NE Japan
Yoshiko Masubuchi, Yasuo Ishizaki, Tomohito Shirai, Akiko Matsumoto, Mizuho, Amma-Miyasaka and Mitsuhiro Nakagawa
（vol.122, no.10，p.533-550）
Appendix. 1-4
 

File No44：vol.122, no.8

巡検案内書：葉山–嶺岡帯トラバース（第123年学術大会巡検Cコース）
高橋直樹・柴田健一郎・平田大二・新井田秀一
Geologic traverse from the Mineoka Belt to the Hayama Belt, Central Japan
Naoki Takahashi, Kenichiro Shibata, Daiji Hirata and Shuichi Niida
（vol.122, no.8，p.375-395）
Appendix. Caption（PDF）
Appendix. 1〜11（PDF）
Appendix. 12〜21（PDF）

 

File No43：vol.122, no.4

論説：利根川低地における「弥生の小海退」の検証
田辺　晋・堀　和明・百原　新・中島　礼
Verification of the “Yayoi regression” in the Tonegawa Lowland, central Japan
Susumu Tanabe, Kazuaki Hori, Arata Momohara and Rei Nakashima
（vol.122, no.4，p.135-153）
Appendixの一括ダウンロード（PDF;6.3MB）
Fig. A1. Stratigraphic columns of core sediments used in this study.
Fig. A2. Diatom assemblages. Relative abundances of marine–brackish–freshwater species (left) are expressed as percentages of the total number of frustules counted. Relative abundances of freshwater-species ecologies (right) are expressed as percentages of the total number of frustules counted in freshwater species. More than 100 frustules were counted from each sample. Black circles indicate that the counted frustules make up <1% of the total counted frustules.
Fig. A3. Photographs of plant macrofossils. (a) Ruppia rostellata fruit, (b) Najas marina seed, (c) Potamogeton distinctus fruit, (d) Trapa fruit (spine). Scale bar, 1 mm.
Table A1. Locations and penetration depths of sediment cores used in this study.
Table A2. Sea-level index points from Toyama Bay (Fujii,1992). Measured 14C ages were converted into conventional 14C ages using δ13C values of –27.5‰ and 0‰ for plant and shell, respectively.
 

File No42：vol.122, no.3

論説：赤城火山軽石噴火期のマグマ噴出率と組成の変化
山元孝広
Magma-discharge rate and geochemical evolution during the pumice-eruption stage of Akagi Volcano, NE Japan.
Takahiro Yamamoto
（vol.122, no.3，p.109-126）
Appendixの一括ダウンロード（PDF;1.4MB）
Appendix 1. List of outcrops.
Appendix 2. Major element contents of volcanic glass shards. obtaimed by EDX measurements.
Appendix 3. Whole rock chemical compositions of pumices. Major and trace-elements were measured by ICP optical and mass spectrometry.
Appendix 4-1. Thickness contours for the volcanic cone of younger Akagi Volcano.
Appendix 4-2. Thickness contours for the Itoi and Fudo Pumice Flow Deposits.
Appendix 4-3. Thickness contours for the Tanashita Pumice Flow Deposit.
Appendix 4-4. Thickness contours for the Fujiki Pumice Flow Deposit.
Appendix 4-5. Thickness contours for the Wakubara Pumice Flow Deposit.
Appendix 4-6. Thickness contours for the Ogo Pumice Flow Deposit.
Appendix 4-7. Thickness contours for the Toshimaru Pumice Flow Deposit.
Appendix 4-8. Thickness contours for the Nagumo Pumice Flow Deposit.

File No41：vol.122, no.3

論説：歴史時代に噴出した同一火山由来の軽石層の同定：宮崎平野で見出された桜島文明テフラの例
生田正文・丹羽正和・檀原 徹・山下 透・丸山誠史・鎌滝孝信・小林哲夫・黒澤英樹・國分（齋藤）陽子・平田岳史
Identification of pumice derived from historic eruption in the same volcano: Case study for the
Sakurajima-Bunmei tephra in the Miyazaki Plain.
Masafumi Ikuta, Masakazu Niwa, Tohru Danhara, Tohru Yamashita, Seiji Maruyama, Takanobu Kamataki, Tetsuo Kobayashi, Hideki Kurosawa, Yoko Saito-Kokubu and Takafumi Hirata
（vol.122, no.3，p.89-107）
（それぞれの図番号をクリックするとPDFがダウンロードできます）
Table S1. Chemical compositions of volcanic glass shards, determined by LA–ICP–MS.

File No40：vol.121, no.11

論説：四国中央部の中央構造線断層帯川上断層東端部における群列ボーリング調査
池田倫治・辻　智大・後藤秀昭・堤　浩之・興津昌宏・柳田　誠・大野裕記・西坂直樹
Arrayed-boring survey near the eastern end of the Kawakami fault of the Median Tectonic Line Active Fault Zone in central Shikoku, southwest Japan
Michiharu Ikeda, Tomohiro Tsuji, Hideaki Goto, Hiroyuki Tsutsumi, Masahiro Okitsu，Makoto Yanagida, Yuki Ohno and Naoki Nishizaka
（vol.121, no.11，p.403-419）
（それぞれの図番号をクリックするとPDFがダウンロードできます）
Appendix 1. TPhotographs of each core (Br. A to Br. D). Yellow and red dashed outlines indicate Unit 2 and Unit 4, respectively. Unit 4 occurs in Br. A, Br. B and Br. C, but not in Br. D. Small numerals show depth in meters.
Appendix 2. Photographs and unit sub-divisions in the depth range –9.4 to –10.4 m of Br. D. Small numerals show elevation in meters.
 

File No39：vol.121, no.10

論説：房総半島，新第三系安房層群上部のthin-skin 変形と褶曲
古角晃洋・佐藤活志・山路　敦
The thin-skinned deformations and folding of the upper Awa Group (Neogene) in the Boso Peninsula, Japan
Akihiro Kokado, Katsushi Sato and Atsushi Yamaji
（vol.121, no.10，p.359-372）

ファイルダウンロードはこちら
Appendix A. Tuff marker beds originally identified by the author.
Appendix B. Fault-slip data for the Amatsu, Kiyosumi, and Anno formations in the study area. F, ‘full’ fault-slip data which consist of orientations of the fault planes, lineations,and senses of movements; L, ‘line-only’ fault-slip data which lack senses of movements; S, ‘sense-only’ fault-slip data which lack orientations of lineations; N, normal shear sense; R, reverse shear sense; D, dextral shear sense; S,sinistral shear sense; U, unknown shear sense.
Appendix C. Route map in the study area, showing the locations where fault-slip data were obtained.
 

File No38：vol.120, no.7

論説：伊豆大島2013 年ラハールの堆積学的特徴：ラハール堆積物の粒度組成による分類
山元孝広・川辺禎久
Sedimentary characteristics of the Izu-Oshima 2013 lahar: classification of various lahar deposits based on grain-size distribution
Takahiro Yamamoto and Yoshihisa Kawanabe
（vol.120, no.7，p.233-245）

ファイルダウンロードはこちら
Appendix 1. Sample list.

 

File No37：vol.120, no.4

論説：箱根火山群，強羅付近の後カルデラ地質発達史
萬年一剛
Post-caldera geology of Gora Region in Hakone Volcano Group, Japan
Kazutaka Mannen
（vol.120, no.4，p.117-136）

ファイルダウンロードはこちら
Open file 1  Selected pollen diagrams for the #5, #6, #10, #41, and JMA wells. See Fig. 3 for well locations.
Open file 2  Number and percentage of fossil pollen grains in unit 6 of the JMA-V29 borehole.
Open file 3  Fossil diatoms in unit 6 of the JMA-V29 borehole.
Open file 4  Whole-rock major element (wt%) and trace element (ppm) compositions of volcanic clasts in JMA-V29 borehole samples, as determined by XRF.
Open file 5  Whole-rock major element (wt%) and trace element (ppm) compositions of volcanic clasts and lavas samples from boreholes near borehole JMA-V29, as determined by XRF.

 

File No36：vol.120, no.2

論説：Zircon U–Pb age and its geological significance of late Carboniferous and Early Cretaceous adakitic granites from eastern margin of the Abukuma Mountains, Japan
Nobutaka Tsuchiya, Tomoyo Takeda, ,Kenichiro Tani, Tatsuro Adachi, Nobuhiko Nakano, Yasuhito Osanai and Jun-Ichi Kimura
（vol.120, no.2，p.37-51）

ファイルダウンロードはこちら
Open file 1. Petrography of analyzed samples.
Open file 2. Photomicrographs of the‘ Wariyama Sheared Granodiorite.’ A: Medium-grained tonalite (KAKUDA7, PPL); B: medium-grained tonalite (KAKUDA7, CPL); C: medium-grained tonalite (KAKUDA9, PPL); D: medium-grained tonalite (KAKUDA9, CPL); E: coarse-grained quartz diorite (11111322, PPL); F: coarse-grained quartz diorite (11111322, CPL); G: coarse-grained tonalite (11111205, PPL); H: coarsegrained tonalite (11111205, CPL). Abbreviations, Hbl: hornblende; Bt: biotite; Pl: plagioclase; Kfs: K-feldspar; Qtz: quartz; Ttn: titanite; PPL: plain polarized light; CPL: crossed polarized light.
Open file 3. Sampling locality.

File No35：vol.119, no.12

論説：西南北海道，更新世渡島小島火山の地質と岩石学的特徴
小杉安由美・中川光弘・清野寛子
（vol.119, no.12，p.743-758）

ファイルダウンロードはこちら
Appendix 1. Whole-rock chemical compositions of representative samples from the Oshima-Kojima volcano. Unit names are as in Table 1. Sample localities are shown in Fig. 3.
Appendix 2. Sr and Nd isotopic compositions of wholerock samples from the Kariba-yama, Oshima-Oshima, and Megata volcanoes.

File No34：vol.119, no.10

報告：ストラウブ法によるシート状タービダイト層累重様式の定量検出：房総半島中新統−鮮新統清澄層の例
浦本豪一郎・清家一馬
（vol.119, no.10，p.693-698）

ファイルダウンロードはこちら
◯Appendix 1. Equations of the modified Straub method for mesuring the standard deviation of the sedimentation rate within a given measurement time window for the discretized terrestrial outcrop data (Uramoto and Seike, 2012).

File No33：vol.119, no.10

論説：沖縄島および周辺諸島に分布する先新第三系基盤岩類の全岩化学組成と砕屑性ザクロ石化学組成．
宮城直樹・馬場壮太郎・新城竜一
（vol.119, no.10，p.665–678）

ファイルダウンロードはこちら

Table 1. Representative major (oxides: wt.%) and trace elements (in ppm) compositions of sandstones in the study area．
Table 2. Representative major (oxides: wt.%) and trace element (in ppm) compositions of greenstones in the study area．
Table 3. Representative chemical composition of detrital garnet.

File No32：vol.119, no.7

論説：常陸台地における下総層群木下層のテフラ層序と広域対比
大井信三・横山芳春・西連地信男・安藤寿男
（vol.119, no.7，p.488–505）

ファイルダウンロードはこちら
◯Appendix 1. Locations of the studied outcrops.
◯Appendix 2. Average major element chemistry of glass shards in tephra layers from the Kioroshi Formation of the Upper Pleistocene Shimosa Group in the Hitachi Terraces. (a) Br-Sc, Bk-Sc, ArP, Nk-Yt, TAu-3, Ob, TAu-9, OiP, KtP, Tephra 20 (1), and Nm-SB. Refer to Fig. 1 for locations of the tephra samples. n: number of analyses. Standard deviations are shown below the average values. *1: Ooi and Yokoyama (2011), *2 measured by SEM with a wide beam to cover a larger analytical area.

File No31：vol.119, no.7

論説：東北日本，仙岩地熱地域南部，高倉火山の山体形成史とマグマ供給系
中谷咲子・長谷川　健・藤縄明彦・照井肇子
（vol.119, no.7，p.457–473）

ファイルダウンロードはこちら
◯Appendix 1. Petrography of the Takinosawa and Takakurasan lava series. – = not found, E = euhedral, S = subhedral, A = anhedral, IG = intergranular, IS = intersertal.

◯Appendix 2. Sample location map showing sample numbers and localities based on Fig. 5.

 

File No30：vol.119, no.6

論説：和泉山脈地域における和泉層群の有機物熟成と堆積盆の埋没モデル．
清家一馬・平野弘道
（vol.119, no.6，p.397–409）
ファイルダウンロードはこちら
◯Appendix 1. List of samples from the Izumi Mountains, Kinki district, and the Asan Mountains, Shikoku Island. * = Distance from the northern marginal unconformity of the Izumi sedimentary basin; ** = Basin width distance; *** = Distance from Matsuyama (132°42’00” E).

◯Appendix 2. Sample localities of Suzuki (1996) and values of mean random vitrinite reflectance (Rm) converted from maximum vitrinite reflectance (Rmax) values of Suzuki (1996). * = Rm value; ** = Estimates based on Koch and Gunther (1995), using Rm = 0.7469Rmax + 0.2241; *** = Distance from the northern end of the northern marginal facies; **** = Basin width distance; ***** = Distance from Matsuyama (132°42’00” E).

◯Appendix 3. Random vitrinite reflectance (Rr) histograms for 43 samples from the Izumi Group. Class width of each population is 0.05% reflectance; triangles indicate the mean values (Rm) for each sample.

◯Appendix 4. Mean random vitrinite reflectance (Rm) and Rock-Eval Tmax values for the Izumi Group of the Izumi Mountains and the Asan Mountains. Maximum paleotemperatures (Tpeak) were estimated using (A) Tpeak = 104 ln (Rm) + 148 (Barker , 1988), and (B) Tpeak = (ln(Rm) + 1.68)/0.0124 (Barker and Pawlewicz, 1994). Std = standard deviation; “n.d.” denotes not measured.
  　　

File No27：vol.119, no.4

論説：島根県出雲市南方地域における中新統のK–Ar 年代と古地磁気方位
沢田順弘・三代喜弘・今岡照喜・吉田聖典・稲田理沙・久井和徳・近藤　仁・兵頭政幸
 (vol.119, no.4　p.267-284)

ファイルダウンロードはこちら
◯Table 1. Mineral K–Ar ages of analyzed samples from the Miocene in the southern Izumo Basin with the sample number, rock type, formation, occurrence and location (longitude and latitude) of analyzed samples.

◯Table 2. Whole rock K-Ar ages of analyzed samples from the Miocene in the southern Izumo Basin with the sample number, rock type, formation, occurrence and location (longitude and latitude) of analyzed samples.

◯Table 3.Paleomagnetic directions of the Miocene and the Yoshida Plutonic Complex in the Izumo Basin.

◯Table 4. Whole rock K–Ar ages of the Miocene in Ohda and Yasugi cities, Shimane Prefecture(Sawada and Itaya, unpublished data) with the sample number, rock type, formation, occurrence and location (longitude and latitude) of analyzed samples.

付録.　K-Ar年代測定に用いられた岩石試料の記載

File No26：vol.119, no.3

論説：フーリエ解析とフラクタル次元による砕屑物粒形の定量方法と堆積場判別方法の提示
鈴木慶太・酒井邦裕・太田　亨
 (vol.119, no.3　p.205-216)

◯Appendix 1. Scores of each index for all particles obtained during this study.

◯Appendix 2. Output files giving the results of principal component analysis; the PCR file enables the calculation of EF1, EF2, and EF3 scores for any given grain, and the PDF file contains Appendix 2a–e.

File No25：vol.119, no.1

ノート：伸縮自在印刷用フィルムを活用した立体地形モデルの作製とその教材化の試み
伊藤　孝・岡崎智鶴子・芝原暁彦・澤村　寛・三田直樹
 (vol.119, no.1　p.39-44)

ファイルダウンロードはこちら
◯Open File 1. Outline of the preparation techniques used informing a solid geomorphological model covered with mapprinted OK film.

◯Open File 2. View of the laboratory used for classes, focusing on covering a solid geomorphological model with mapprinted OK film, (1) outlining of the procedures involved in OK film covering and examples of potential applications, (2) removal of extraneous OK film with scissors, (3) application of special adhesive onto the cast surface using the index finger, and (4) drying the OK film-covered casts using hairdryers.

◯Open File 3. Timetable for a laboratory class focusing on forming a solid geomorphological model covered with mapprinted OK film, and observation of the model produced during the class in Earth Science Experiment B.

File No24：vol.118, no.11

ノート：213 nm Nd-YAG レーザーアブレーションICP 質量分析装置を用いたジルコンのU-Pb 局所年代分析：SHRIMP データとの整合性の検討
勝部亜矢・早坂康隆・坂口　綾・高橋嘉夫
 (vol.118, no.11　p.762-767)

◯Appendix 1.  LA-ICP-MS isotopic data for standard zircons (Plešovice, SL13, AS3, QGNG).

File No23：vol.118, no.11

論説：北海道日高帯ポロシリオフィオライト北部地域の地質と変成作用
田中真二・木崎健治・宮下純夫
 (vol.118, no.11　p.723-740)

◯Table A1. Representative amphibole analyses showing compositional zoning in porphyroclast cores and rims and in matrix amphiboles within upper schistose amphibolite in the Chiroro River area.
◯Table A2. Representative analyses of amphibole from greenschist, upper schistose amphibolite, and later dolerite dykes in the Chiroro River area.
◯Table A3. Representative analyses of plagioclase from greenschist, upper schistose amphibolite, and later dolerite dykes in the Chiroro River area.

File No22：vol.118, no.6

ノート：野外実習と室内実験を取り入れた学校教員向け巡検の実践報告：地層はぎ取り標本と簡易水路実験の授業での活用を目指して
植木岳雪・伊藤　孝・中野英之・小尾　靖・牧野泰彦
 (vol.118, no.6　p.387-392.)

◯Table A. Questionnaire items.
◯Table B. Reasons given by participants for their choice of the most impressive stop during the excursion.
◯Table C. Improvements to the excursion suggested by participants.
◯Table D. How to use a peel specimen of sediments in a school lesson, as suggested by participants.
◯Table E. How to conduct a simplified flume experiment in a school lesson, as suggested by participants.
◯Table F. Other impressions of the entire excursion from participants.
◯Table G. References on the implementation of earth science education in schools using regional materials.
【Table A–G. PDF】
 

File No28：vol.118, no.4

論説：四国北西部の中央構造線活断層系伊予断層の完新世活動履歴
池田倫治，後藤秀昭，堤　浩之，露口耕治，大野裕記，西坂直樹，小林修二
 (vol.118, no.4　p.220-235.)

◯Table 1. Description of strata exposed on the Miaki trench walls.
◯Table 2. Radiocarbon ages for samples from the Miaki trench site.
◯Table 3. Description of strata exposed on the Ichiba trench walls.
◯Table 4. Radiocarbon ages for samples from the Ichiba trench site.
【Table 1–4】

File No29：vol.118, no.1

論説：LA-ICP-MS U–Pb zircon and FE-EPMA U–Th–Pb monazite dating of pelitic granulites from the Mt. Ukidake area, Sefuri Mountains, northern Kyushu
Adachi, T., Osanai, Y., Nakano, N. and Owada, M.,
 (vol.118, no.1　p.39-52.)

◯Fig. A1. Representative time-resolved isotopic ratio profiles determined by ablation of zircons from Temora (a) and an unknown sample (060101A) (b). In the case of these analyses, isotopic ratios are consistent between 48 to 120 s for the Temora sample and 53 and 120 s for sample 060101A. These portions of data were integrated and then calibrated during age determination.
◯Table A1. Short- and long-term precision of U–Pb isotope ratios and calculated ages of the FC-1 zircon standard.
◯Table A2. U–Pb isotope ratios and calculated ages from analysis of zircons from Temora and the Itoshima granodiorites calibrated against the FC-1 zircon standard.
◯Table A3. Comparison of U–Pb isotope ratios and calculated age data from analysis of the FC-1 zircon with different laser beam diameters.
◯Table A4. Chemical compositions and U–Th–Pb ages of reference monazites.

【Fig. A1，Table 1–4】
 

File No21：vol.117, no.10

総説：地質学における方向データ解析法：円周データの統計学
新井宏嘉
 (vol.117, no.10　p.547-564.)

◯Appendix 1. (PDF) Synthetic circular data (100 random deviates in each case) drawn from circular distributions.
◯Appendix 2. (PDF) Applications of circular statistics software.

 

 

File No20：vol.117, no.8

論説：宮城県沖大地震の前兆を捉えるための深層地下水変動研究：2008年2月〜2009年12月の観測結果
鹿島雄介・南須原美恵・中村隆志・山内常生・大槻憲四郎
 (vol.117, no.8　p.451-467.)

◯Fig. A (PDF)
Hourly data of the groundwater temperature, water level and the precipitation during 2008 and 2009 at the Atago (AT, Fig. Aa), Yamoto (YM, Fig. Ab) and Minamikata (MN, Fig. Ac) observation sites. BAYTAP-G was applied to the hourly data of water level from all observation sites using the barometric pressure as an associate data. The smooth component output from BAYTAP-G is approximated by the linear equations for the data from the AT and YM observation sites, while approximated by a 3rd-order polynomial equation for the data from the MN observation site. The values of water level shown in the figures represent the residuals of the smooth component from these regression equations. Since the raw data of groundwater temperature from all observation sites contains only very small components of the tidal and barometric effects, BAYTAP-G was not applied. The raw data from the AT and YM observation sites and those before April 16, 2009 from the MN observation site were approximated by a 2nd-order polynomial equation, a linear equation and a 4th-order polynomial equation, respectively. The water temperature data after June 12, 2009 from the MN observation site contain the significant daily fluctuations of unknown causes. After they were removed by the Fourier inverse transform, they were approximated by a 2nd-order polynomial equation. The residuals from these regression equations were plotted in the figures. The data of precipitation obtained from the nearby observatories of Japan Meteorological Agency show the time-series clusters. The cumulative precipitations for every cluster are plotted in the figure. Numerals 1, 2, 3 and 4 in circles denote the times of the off-Ibaraki Prefecture earthquake (MJ7.0) on May 8, 2008, Iwate-Miyagi inland earthquake (MJ7.2) on June 14, 2008, off-Fukushima Prefecture earthquake (MJ6.9) on July 19, 2008, and the northern Iwate prefecture coast earthquake on July 24, 2008 (MJ6.8). Note that the observed water level at the MN observation site after the Iwate-Miyagi inland earthquake is 400 mm lower than those shown in Fig. Ac.

 

 

 

 

File No19：vol.117, no.6

論説：噴出物の構成物組成と本質物質の全岩および鉱物組成から見た泥沢火山のBC3400カルデラ形成噴火（泥沢湖噴火）のマグマ供給系
増渕佳子・石崎泰男
 (vol.117, no.6　p.357-376.)

◯Appendix 1. (PDF) Representative modal compositions
Sampling sites and stratigraphic levels are shown in Figs. 1, 2 and 7. Abbreviations: WP, white pumice; GP, gray pumice; BS, black scoria; GS, gray scoria; Pl, plagioclase; Amp, amphibole; Opx, orthopyroxene; Qtz, quartz; Opq, opaque minerals; Xe, xenolith; Ph, phenocryst.
◯Appendix 2. (PDF) Representative whole-rock compositions.
Total Fe expressed as Fe2O3. For plotting on the Harker diagrams (Fig. 7), the FeO* is assumed to be FeO + 0.8998 Fe2O3. Sampling sites and stratigraphic levels are shown in Figs. 1, 2, 3 and 6. Abbreviations: WP, white pumice; GP, gray pumice; BS, black scoria; GS, gray scoria.
◯Appendix 3. (PDF) Representative silicate mineral compositions (core compositions). Abbreviations: WP, white pumice; GP, gray pumice; BS, black scoria; GS, gray scoria.
* An = 100 × Ca/(Ca + Na + K) in cation units.
** Mg# = 100 × Mg/(Mg + Fet) in cation units, where Fet is total Fe, as Fe2+.
◯Appendix 4. (PDF) Composition of coexisting Fe-Ti oxides Abbreviations: WP, white pumice; GP, gray pumice; BS, black scoria; GS, gray scoria; Mag, magnetite; Ilm, ilmenite; XUlv, mole fraction of ulvöspinel; XIlm, mole fraction of ilmenite.
* Calculated using the method of Stormer (1983).
** Calculated using the QUILF 6.42 software package (Anderson et al., 1993) applying technique of Manley and Bacon (2000). The pressure dependence of the geothermometer is slight, and a pressure of 200 MPa was assumed in all calculations.

 

 

 

File No18：vol.117, no.5

 

論説：新潟堆積盆七谷層中に見つかった中期中新世広域テフラ：Kbiテフラと紀伊半島室生火砕流堆積物の対比
工藤　崇・檀原　徹・岩野英樹・山下　透・三輪美智子・平松　力・柳沢幸夫
 (vol.117, no.5　p.277-288.)

◯Fig. 1. Photomicrograph of reddish and colorless zircons from the Kbi tephra.

 

 

 

 

 

 

 

File No17：vol.116, no.10

 

総説：貝形虫の殻のMg/Ca比, Sr/Ca比による古環境推定の現状と問題点
森下知晃・山口龍彦・眞柴久和・神谷隆宏
 (vol.116, no.10　p.523-543.)

◯Appendix 1. (PDF)Results of statistic tests. Abbreviations: S.D. = standard deviation, N = number of analyses, df = degree of freedom. The result of the tests follows: n.s., no significance; *, p<0.05; **, p<0.01．
◯Appendix 2. (PDF)Superfamily, family, locality, Taxon Codes, and references of the examined ostracode taxa.

 

 

 

File No16：vol.115, no.8

 

報告：紀伊半島，中新世火成岩類のアパタイトのフィッション・トラック年代
岩野英樹・檀原　徹・星　博幸
 (vol.115, no.8　p.427-432.)

 

PDF(1.9MB)

◯Fig. A1.Analytical results of the sample MR1-Fl(Ap).
◯Fig. A2.Analytical results of the sample MR70(Ap).
◯Fig. A3.　Analytical results of the sample SKB2(Ap).
◯Fig. A4.　Analytical results of the sample SKB2(Ap)_2.
◯Fig. A5.　Analytical results of the sample SKB2(Ap)_3.
◯Fig. A6.　Analytical results of the sample KSSP(Ap).
◯Fig. A7.　Analytical results of the sample AS01(Ap).
◯Fig. A8.　Analytical results of the sample TG02(Ap).
◯Fig. A9.　Analytical results of the sample KAR-N3(Ap).
◯Fig. A10.　Analytical results of the sample KAR4e(Ap).
◯Fig. A11.　Analytical results of the sample KAR5(Ap).
◯Fig. A12.　Analytical results of the sample KOZA2(Ap)
 

 

File No15：vol.115, no.6

 

論説：夜久野オフィオライト朝来岩体における古生代海洋内島弧地殻の形成と進化過程
隅田祥光・早坂康隆
 (vol.115, no.6　p.266-287.)

 

◯Appendix 1　　Major oxides (in wt. %) and trace elemental abundances (in ppm) for the Yakuno rocks in the Asago body. Total Fe as FeO. Abbreviations: hb mtgb, hornblende metagabbro; amph., amphibolite; qtz monzodiorite, quartz monzodiorite; leuco., leucosome.
Appendix 1-1(PDF) 　　Appendix 1-2(PDF)  　　Appendix 1-3(PDF)
◯Appendix 2　　Mineral–melt partition coefficients. Data sources: Ar Arth (1976); BD Bacon and Druitt (1988); Bi Binderman et al. (1998); Bo Bougault and Hekinian (1974); Do Dostal et al. (1983); DS Dunn and Sen (1994); EG Ewart and Griffin (1994); Fj Fujimaki (1986); Fu Fujimaki et al. (1984); Gi Gill (1981); Gr Green et al. (2000); GP Green and Pearson (1987); I interpolated or extrapolated; Ha Hauri et al. (1994); JN Jang and Naslund (2003); MH Mahood and Hildreth (1983); Ma Martin (1987); MC McCallum and Charette (1978); NS Nagasawa and Schnetzler (1971); NC Nash and Crecraft (1985); Ni Nielsen et al. (1992); PN Pearce and Norry (1979); PS Philpotts and Schnetzler (1970); Ro Rollinson (1993); Si Sisson (1994); SH Stimac and Hickmott (1994); ZB Zack and Brumm (1998)  Mineral abbreviations: pl, plagioclase; hbl, hornblende; cpx, clinopyroxene; opx, orthopyroxene; mt, magnetite; ilm, ilmenite; ol, olivine; spl, spinel; ap, apatite; zir, zircon; bt, biotite.

◯Appendix 3　　Equations used for modeling. The following equations of Allègre and Minster (1978) have been used for the Rayleigh fractional crystallization model:
Cliq = C0FDi–1 and Ccum = C0(1 – FDi)/(1 – F),
where Cliq is weight concentration in the residual liquid, Ccum is weight concentration in the cumulate F is fraction of residual liquid, C0 is weight concentration in the parental liquid and Di is bulk partition coefficient of crystallizing assemblage for the element. Partition coefficients for basalte and basaltic andesite liquid (Appendix 2) were applied for the modeling of first-stage Yakuno rocks (Figs. 10 and 11), and those for the dacite and rhyolite liquids were applied for the modeling of second-stage Yakuno rocks (Figs. 15 and 17).
 The following equation of Shaw (1970) has been used for the equilibrium batch melting model:
CMelt/Ci = 1/(DRS + F(1 – DRS) )
where CMelt is weight concentration in the partial melt, F is fraction of partial melt produced, Ci is weight concentration in the original unmelted solid (i.e. source) and DRS is bulk partition coefficient of the element in the original solid. Partition coefficients for andesite liquid (Appendix 2) were applied for the modeling of partial melting of first-stage Yakuno rocks (Fig. 16).

◯Appendix 4　　Compositions of source (starting material) and partial melts (in wt. %), and modes of run products (in %) for the dehydration melting experiment by Beard and Lofgren (1991).

 

File No14：vol.115, no.2

 

論説：大阪堆積盆地における中部更新統の花粉生層序と古環境変遷
  本郷美佐緒
 (vol.115, no.2　p.64-79.)

 

◯Appendix 1.　 Correlation of sample numbers with depth in core and sediment type. Pollen extraction procedures (A and B) are explained in the text.

◯Appendix 2.　 Composition of pollen and spores included in each sample. Each pollen frequency (%) is based on total sum of pollen of trees and shrubs.

 

File No13：vol.114, no.11

 

論説：改訂「日本列島海底谷系図」—海底谷の地形的特徴と問題点—
  嶋村　清
 (vol.114, no.11　p.560-576)

◯第1図a(JPEG)　日本列島海底谷系図—北海道沖—.　地名は海底谷の名称を示す。1：海盆・凹地、2：海盆底（比深50m以下）（以下、同）

◯第1図b(JPEG)　日本列島海底谷系図—東北日本沖—.　TDSC：富山深海チャネル

◯第1図c(JPEG)　日本列島海底谷系図—関東・中部・近畿沖—.　
AG：安乗口海底谷、AH：浅羽海底谷、AT：阿田和海底谷、DT：大東海底谷、GK：五ヶ所海底谷、HM：浜松海底谷、HO：浜岡海底谷、J：城ヶ島海底谷、KM：木本海底谷、KS：神前（かみさき）海底谷、KO：北尾鷲海底谷、KT：勝浦海底谷、KZ：古座海底谷、MR：布良（めら）海底谷、MS：舞坂口海底谷、NDSC：南海深海チャネル、NG：長島海底谷、NJ：新島海底谷、OM：大室海底谷、OW：尾鷲海底谷、OY：大山沖海底谷、RY：竜洋海底谷、SDSC：潮岬深海チャネル、SG：新宮海底谷、SM：志摩海底谷、SN：佐野海底谷、TJ：太地海底谷、TM：高松海底谷、UK：宇久井海底谷

◯第1図d(JPEG)　日本列島海底谷系図—中国・四国・九州沖—
AG：安乗口海底谷、AH：浅羽海底谷、AT：阿田和海底谷、DT：大東海底谷、GK：五ヶ所海底谷、HM：浜松海底谷、HO：浜岡海底谷、KM：木本海底谷、KS：神前（かみさき）海底谷、KO：北尾鷲海底谷、KZ：古座海底谷、MS：舞坂口海底谷、NG：長島海底谷、OW：尾鷲海底谷、OY：大山沖海底谷、RY：竜洋海底谷、SDSC：潮岬深海チャネル、SG：新宮海底谷、SM：志摩海底谷、SN：佐野海底谷、TJ：太地海底谷、TM：高松海底谷、UK：宇久井海底谷、Oki1〜Oki4：沖ノ島沖1〜4海底谷、地名の後のGは海底谷群を意味する。

 

File No12：vol.114, no.10

 

報告：小断層から推定された鉱床地域の古応力：鹿児島県永野地域の例
  引地原野・山路　敦
 (vol.114, no.10　p.540-545)

 

◯付録第1表．永野地域から得られた断層スリップデータ．擦痕の方向は，山路・大原(2001)の書式で記載．擦痕の方向または変位センスが空欄の行は，不完全データ．（PDF版）

◯付録第1図．永野地域のルートマップ．断層スリップデータ取得地点が，NL1のようにアルファベット2文字と数字とで表されている．断層データは付録第1表．国土地理院発行2万5千分の1地形図「薩摩黒木」，「栗野」，「永野」，「横川」を使用．（PDF版）

File No11：vol.114, no.10

論説：圧縮性ステップにおける破砕帯の構造−岐阜県飛騨市の跡津川断層西部の例−
  丹羽正和・島田耕史・黒澤英樹・三輪敦志
 (vol.114, no.10　p.495-515)

◯付録Fig. 1. 　Typical X-ray diffraction patterns of smear slides for the <2 μm size fractions of the fault clays.  An upper pattern of each figure is treated with ethylene-glycol.  cal: calcite, chl: chlorite, ill: illite, kln: kaolinite, py: pyrite, qtz: quartz, sc: smectite, sd: siderite.（PDF版）

File No10：vol.113, no.7

論説：紀伊半島北部の室生火砕流堆積物と周辺に分布する凝灰岩の対比およびそれらの給源：軽鉱物屈折率を用いたモード分析によるアプローチ
 山下　透・檀原　徹・岩野英樹・星　博幸・川上　裕・角井朝昭・新正裕尚・和田穣隆
 (vol.113, no.7　p.340-352)

◯付録第1図　　紀伊半島に分布する中期中新世珪長質火成岩類から採取した96試料の全鉱物，重鉱物，軽鉱物組合せモード分析結果と，軽鉱物と火山ガラスの屈折率頻度分布．軽鉱物組合せモード分析結果は屈折率範囲を4つに分割し，低屈折率側からカリ長石・低屈折率斜長石(アルバイト〜オリゴクレース)・石英・高屈折率斜長石(アンデシン〜アノーサイト)として表した．（PDF版）

◯付録第2図　　本研究で用いた96試料の試料採取地点．試料名は通番+試料記号で表し，使用した1/25000地形図名もそれぞれ示した．（PDF版）

◯付録第3図　　室生火砕流堆積物試料を採取した百々ルートと龍口ルートのルートマップ．（PDF版）

File No9：vol.113, no.3,

論説：鹿児島県八重山地域の地質と鮮新統郡山層の層位学的研究
内村公大・大木公彦・古澤　明　 (vol.113, no.3 p.95-112.)


◯オープンファイル第1表　珪藻化石産出一覧表　（PDF版）

File No8：vol.112, no.11

論説：日高変成帯主帯に分布する高変成度角閃岩類の原岩推定および北部日高帯緑色岩類との比較
川浪聖志・中野伸彦・小山内康人・加々美寛雄・大和田正明　（vol.112, no.11　p.639-653；特集号「日高衝突帯研究の最近の進歩」）

◯Appendix 1. Bulk chemical compositions of amphibolites and greenstones
Fe2O3*; total Fe as Fe2O3. FeO**; total Fe as FeO. LOI; loss on ignition. XMg=Mg/(Mg+Fe). n.d.; not determined. n.a.; not analyzed.
CHMB: central area of the Hidaka metamorphic Belt, nSHMB: Northern part of southern area of the Hidaka metamorphic Belt, sSHMB: southern part of southern area of the Hidaka metamorphic Belt, Sk: Shimokawa area, Tm: Tomuraushi area, Np: Nipesotsu area, Ot: Okutokachi area, Oc: Ochiai area. SH: Shunbetsu river, KB: Koibokushushibichari river, NNC: Nanashino-sawa river, OG: Ogawara-zawa river, BK: Benikaru-zawa river, SS: Sasshibichari river, NO: Nishuomanai-zawa river, SM: Soematsu-zawa river, HB: Hidakahorobetsu river, SG: Sogabetsu river, MM: Menashuman river, NOB: Niobetsu river, SC: Shirochinomi river, MS: Menashunbetsu river, MK: Mukorobetsu river, PN: Panke river, SN: Shinnosukeshunbetsu river, MKT: Mikitonai river, MKI: Mikiinai river, MN: Menashiesanbetsu river, ON: Onarushibe river, FC: Fuchimi river, RB: Rubeshibe river, NK: Nikanbetsu river, ST: Shiitokachi river, NU: Nupun-Tomuraushi river, NP: Nipesotsu river, OA: Ochiaino-sawa river, SI: Shiisopurachi river, UC: Uchino-sawa river, KN: Kanano-sawa river, TM: Tomamu river.

◯Appendix 2. REE compositions of amphibolites
Abbreviations are same to those in Appendix 1.

File No7：vol.112, no.7

総説：組成データ解析における0値および欠損値の扱いについて
新井宏嘉・太田　亨（vol.112, no.7　p.439-451)

付録1　丸め誤差による0値を置換するプログラムのソースコード．
PDF版
text版
付録2　不適合度を計算するプログラムのソースコード．
PDF版
text版

File No6：vol.112, no.6

ノート：対数比法における規格化成分選定プログラム—Woronow-Love-Schedl法の自動化—
新井宏嘉・太田　亨（vol.112, no.6　p.430-435）

○付録．Woronow-Love-Schedl法を実行するR用プログラムコード．
PDF版
text版

File No5：vol.111, no.5, 小林ほか

能登半島輪島地域の中新統の層序・堆積環境・テクトニクス
 小林博文・山路　敦・増田富士雄（vol.111, no.5　p.000-000)

○第1表．
珪藻化石リスト．保存状況：G, 良好；VP, 極めて不良．含有量：A, 多産；PD, 珪藻貧産出．存否：+, 存在；−, 不在．

File No4：vol.110, no.10, 辻森

組成累帯クロムスピネルからみた青海蛇紋岩メランジュを構成する蛇紋岩の起源
 辻森　樹（vol.110, no.10：特集　飛騨外縁帯研究の進展と展望　p591-597)

○Fig.2 Colored version
Microtexture of chromitite (BOM-03a) and serpentinite (BOM-03b). (A) Photomicrograph of the occurrence of zoned Cr-spinel in chromitite [Plane polarized light = PPL]. (B) Photomicrograph of enlarged view of the inclusion-rich in zoned Cr-spinel in chromitite [PPL]. (C) X-ray image of Fe (Kα) of Cr-spinel grain of (B). (D) X-ray image of Mg (Kα) of (C). (E) X-ray image of Ti (Kα) of (C). (F) X-ray image of Na (Kα) of (C), showing distribution of pargasitic amphibole inclusions. (G) Photomicrograph of the occurrence of zoned Cr-spinel in serpentinite [PPL]. (H) Back-scattered electron image of the zoned Cr-spinel in serpentinite. Scale bars on each image represent 1 mm. Abbreviations: CrSp = Cr-spinel, Atg = antigorite, Mgs = magnesite.

File No3：vol.110, no.8, 高橋・山下

高橋孝三・山下仁司，2004，ラニーニャ時のレディオラリアフラックス：1999年太平洋赤道域西部・中部における時系列変動と海洋環境．（vol.110, no.8 p463-479)

○Open File Table 1.
 Lists of the sampled dates and intervals, fluxes of total Radiolaria and their three subgroups (Nassellaria, Spumellaria, Phaeodaria), and diversity indices.
○Open File Table 2.
 Radiolarian species counts (No. shells per microslide) at Shallow and Deep sediment trap depths at Sites MT1, MT2, MT3, and MT5.
○Open File Table 3.
 Radiolarian species fluxes (No. shells m-2 d-1) at Shallow and Deep sediment traps deployed at Sites MT1, MT2, MT3, and MT5 during January-December 1999 in the western and central equatorial Pacific.
○Open File Table 4.
 Radiolarian species count data obtained from core tops (0-0.5 cm) of the multiple cores recovered at four sediment trap sites. 

File No2：vol.109, no.4, Nomura

 

Ritsuo Nomura,2003, Assessing the roles of artificial vs. natural impacts on brackish lake environments: foraminiferal evidence from Lake Nakaumi, southwest Japan.（vol.109, no.4 ｐ197-214）

○Appendix 1. Quantitative data set for factor analysis and the varimax factor score matrix
○Appendix 2. Calculated ages of each sample.
 The dotted lines indicate the marked depth and year, which are referred to the construction activities.
○Appendix 3. Communality and factor loadings.

 

File No.1：vol.108, no.6, Nomura and Seto

 

Ritsuo Nomura and Koji Seto, 2002, Influence of man-made construction on environmental conditions in brackish Lake Nakaumi,southwest Japan:Foraminiferal evidence.（vol.108, no.6  p394-409）

○Appendix 1: Foraminiferal species identified in this study.(PDF/16KB)
○Appendix 2: Foraminiferal occurrence at H-1.(PDF/10KB)
○Appendix 3: Foraminiferal occurrence at H-2.(PDF/12KB)

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