| 1. |
Fumiko Higashino, Tetsuo Kawakami, Tatsuro Adachi, Masaoki Uno,, Multiple fluid infiltration during post-peak metamorphism in southern Perlebandet, Sør Rondane Mountains, East Antarctica ., The 13th Symposium on Polar Science, 2022.11. |
| 2. |
Tatsuro Adachi, Tetsuo Kawakami, Masaoki Uno, Fumiko Higashino, Pressure-Temperature path of a garnet-biotite-sillimanite gneiss from the Oyayubi ridge, Brattnipene, Sør Rondane Mountains., The 12th Symposium on Polar Science, 2021.11. |
| 3. |
Masaoki Uno, Tetsuo Kawakami, Tatsuro Adachi, Fumiko Higashino, Paleostress inversion in hydro-fractured metamorphic complex using 3D aerophotography images (Sør Rondane Mountains, East Antarctica), The 12th Symposium on Polar Science, 2021.11. |
| 4. |
足立 達朗, 河上 哲生, 宇野 正起, 東野 文子, Two distinct timings of metamorphism detected from Menipa, Sør Rondane Mountains, East Antarctica., 日本地球惑星科学連合2022年大会, 2022.05. |
| 5. |
河上 哲生, 仁木 創太, 鈴木 将晏, 坂田 周平, 足立 達朗, 東野 文子, 宇野 正起, 平田 岳史, Long-lived high-temperature metamorphism followed by clockwise P-T path from Menipa, Sør Rondane Mountains, East Antarctica, 日本地球惑星科学連合2022年大会, 2022.05. |
| 6. |
Tetsuo Kawakami, Tatsuro Adachi, Masaoki Uno, Fumiko Higashino, Noriyoshi Tsuchiya, Traces of fluid movement in the active lower crust of
collision setting observed in the Sør Rondane Mountains,
East Antarctica: A field survey report of JARE61, The 11th Symposium on Polar Science, 2020.12. |
| 7. |
Masaoki Uno, Tetsuo Kawakami, Tatsuro Adachi, Fumiko Higashino, Noriyoshi Tsuchiya, Petrological characteristics of granulite/amphibolite-facies "bleached" hydration zones caused by fluid infiltration along fractures at middle crustal conditions in the Sør Rondane Mountains, East Antarctica, The 11th Symposium on Polar Science, 2020.12. |
| 8. |
Tatsuro Adachi, Tetsuo Kawakami, Masaoki Uno, Fumiko Higashino, Noriyoshi Tsuchiya, Contrasting P-T records of the metamorphic rocks at the Oyayubi ridge of Brattnipene, Sør Rondane Mountains, East Antarctica., The 11th Symposium on Polar Science, 2020.12. |
| 9. |
Metamorphic process of the Tromso Nappe in the Scandinavian Caledonides based on P-T-t history of felsic gneiss. |
| 10. |
Andalusite and sillimanite in coarse-grained kyanite-bearing pelitic rocks from the Altai Range, Mongolia. |
| 11. |
Geology of the Cambrian Horei felsic rocks in southern Kitakami Mountains, Japan. |
| 12. |
Paleogeographic consideration to the basement of the Northeast Japan Arc before the opening of the Japan Sea from the viewpoint of the belonging of the Hitachi Cambrian.. |
| 13. |
Formation of biotite-quartz symplectite in Fe-Al rich granulites, north Sør Rondane Mountains, East Antarctica. |
| 14. |
Contrasting pressure-temperature records from the Altai Range, Mongolia; constraints from multiple growth of garnet, aluminosilicates and monazite. |
| 15. |
LA-ICP-MS Zircon U-Pb ages for metamorphic rocks from the Highland and Wanni Complexes, Sri Lanka. |
| 16. |
Deep crustal processs in continental collision orogens inferred from felsite inclusions in granulites. |
| 17. |
U-Pb zircon age and petrochemistry of the granitic rocks from the core of MITI-Kesennuma Oki Well, Japan. |
| 18. |
Partial melting of mafic metamorphic rock in the Main Zone of the Hidaka metamorphic belt in Hokkaido. |
| 19. |
Decompressional metamorphic texture of mafic granulite in Brattnipene, Sør Rondane Mountains, East Antarctica. |
| 20. |
Amphibolite-facies metamorphism in the Sor Rondane Mountains, East Antarctica. |
| 21. |
Sr-Nd isotopes compositions of the Hikami granitic Rocks and Paleozoic granitic rocks. |
| 22. |
LA-ICP-MS Zircon U-Pb ages of metamorphic rocks from the central parts of Highland Complex, Sri Lanka. |
| 23. |
High P-T experiments for högbomite-group minerals. |
| 24. |
Clockwise and anti-clockwise metamorphic evolutions from the Altai Mountains in Mongolia. |
| 25. |
Petrology and geochronology of late Cambrian granitic rocks from southern Kitakami Mountains, Japan. |
| 26. |
Petrochemical study of the Hikami Granitic rocks in the south Kitakami Mountains. |
| 27. |
Metamorphic texture of Fe-rich granulites in Vesthaugen, north Sør Rondane Mountains, East Antarctica. |
| 28. |
Source mantle of the Cretaceous magmatism in the North Kyushu and western Ryoke belt. |
| 29. |
Geochronological characteristics of granitic and metagabbroic rocks from the Kurosegawa Tectonic Belt. |
| 30. |
SETIAWAN Nugroho Imam, OSANAI Yasuhito, NAKAN Nobuhiko, ADACHI Tatsuro, YOSHIMOTO Aya, YONEMURA Kazuhiro, Metamorphic evolution of South Sulawesi, Central Java, and South Kalimantan in Indonesia, 日本鉱物科学会年会講演要旨集, 2013.09. |
| 31. |
Geochronology of the metamorphic rocks from east-central Madagascar : constraints on crustal evolution process. |
| 32. |
中野 伸彦, 小山内 康人, 足立 達朗, SATISH-KUMAR M, 大和田 正明, JARGALAN S, BOLDBAATAR Ch, 吉本 紋, SYERYEKHAN K, モンゴル・アルタイ山脈の変成作用とテクトニクス, 日本鉱物科学会年会講演要旨集, 2013.09. |
| 33. |
OSANAI Y., NAKANO N., ADACHI T., OWADA M., SATISH-KUMAR M., JARGALAN S., BOLDBAATAR Ch., YONEMURA K., YOSHIMOTO A., Garnet, Clinopyroxene megacrysts and Garnet-bearing mantle xenoliths from the Tariat Depression, Mongolia, 日本鉱物科学会年会講演要旨集, 2011.09. |
| 34. |
OWADA M., OSANAI Y., NAKANO N., ADACHI T., YONEMURA K., YOSHIMOTO A., JARGALAN S., BOLDBAATAR C., SATISH-KUMAR M., Paleozoic subduction and collision magmatism in west Mongolia : Evidence from geochronology and geochemistry of the intrusive rocks, 日本鉱物科学会年会講演要旨集, 2011.09. |
| 35. |
SATISH-KUMAR M., OSANAI Y., NAKANO N., KAMEI A., JARGALAN S., BOLDBAATAR C., OWADA M., ADACHI T., YONEMURA K., YOSHIMOTO A., Stable isotope study of metacarbonate rocks from western Mongolia : Implications for fluid-rock interaction processes in the Central Asian Orogenic Belt, 日本鉱物科学会年会講演要旨集, 2011.09. |
| 36. |
Petrology and geochronology of pelitic gneisses in the Hanhohiyn Mountains, the northwestern part of Mongolia
Hanhohiyn Mountains is located in the northwestern part of Mongolia. The mountains are mainly composed of marble, meta-quartzite and pelitic gneisses intercalating with lenticular garnet-amphibolite, garnet-orthopyroxene gneiss and so on. Pelitic gneisses are classified into garnet-sillimanite-biotite gneiss, garnet-cordierite-biotite gneiss and garnet-biotite gneiss. These gneisses indicate the peak metamorphic condition of 600-700 degree and 5.5-6 kbar accompanied by decompression. The EPMA U-Th-Pb Monazite ages concentrate between 480-510 Ma which is interpreted as the timing of the peak metamorphism.. |
| 37. |
High-Al-Mg gneisses and related rocks from the Mongolian Altay Mountains
We report results on geochemistry, geochronology, and P-T analyses of high-Al-Mg gneisses from the Mongolian Altay Mountains.. |
| 38. |
Paleozoic subduction and collision magmatism in west Mongolia: Evidence from geochronology and geochemistry of the intrusive rocks
The Central Asian Orogenic Belt (CAOB) resulted from amalgamation of voluminous subduction – accretionary complexes of Late Neoproterozic to Mesozoic time. Mongolia is the heartland of the CAOB and geologically divided into four complexes; continental blocks, subduction complexes, sedimentary basins and Cenozoic cover sequences. The magma activity in the southern part of Lake zone would, therefore, be related to the continental collision event. Considering geochronology and geochemical features of the intrusive rocks, the subduction and collision events occurred in the Lake zone during Cambrian time. Finally, the North China craton collided to the Siberia craton, giving rise to collision-type metamorphism and S-type granite magmatism during Permian time in the Mongolian Altay region.. |
| 39. |
Consideration of tectonics setting to bulk chemical compositions of blueschist from the Kurosegawa tectonic zone in Japan.
We report petrography and bulk chemical compositions of Kurosegawa blueschists from Kyushu, Shikoku and Kii peninsula, and discuss their origin. Blueschists from Yaeyama metamorphic complex will also be discussed.. |
| 40. |
Understanding metamorphic and igneous histories of the Inthanon Belt, western Thailand. |
| 41. |
Inclusions of sector zoned garnet in pelitic gneiss from the Nujiang river area, SW China. |
| 42. |
EPMA dating of monazite in pelitic granulite from Mt. Ukidake, Kyushu. |
| 43. |
小山内 康人, 野木 義史, 豊島 剛志, 外田 智千, 馬場 壮太郎, 中野 伸彦, 足立 達朗, 大和田 正明, 東南極ドロンイングモードランドの東・西ゴンドワナ大陸接合境界, 日本鉱物科学会年会講演要旨集, 2010.09. |
| 44. |
Zircon chemistry in UHT metamorphic rocks : examples from Napier Complex, East Antarctica. |
| 45. |
Consideration of tectonics setting to bulk chemical compositions of blueschist from the Kurosegawa tectonic zone in Japan. |
| 46. |
Geochemical signature and P-T conditions of layered gneiss complex in the Mongolian Altai Mountains: A preliminary report. |
| 47. |
A preliminary report of EPMA dating of metamorphic rocks in the western part of Mongolia.. |
| 48. |
Corundum and quartz in Sør Rondane Mountains, East Antarctica. |
| 49. |
Whole rock geochemistry and mineral assemblage of mafic gneisses in Central Dronning Maud Land, East Antarctica. |
| 50. |
Understanding metamorphic and igneous histories of the Inthanon Belt, western Thailand
Several metamorphic and igneous ages were obtained from the Inthanon Belt, western Thailand.. |
| 51. |
Collision boundary between E- and W-Gondwana in Dronning Maud Land, East Antarctica
Recently the Dronning Maud Land region including the Sør Rondane (SR) Mountains attracts attentions for their tectonic and metamorphic evolutions through the Gondwana Super continent evolution and construction. The region is considered as the main portion of the East-West Gondwana collision during the East Africa-Antarctica Orogen (EAAO: e.g. Jacobs and Thomas, 2004). We suggest that the western and the eastern blocks would be belonging to the EAAO and E-Gondwana, respectively. The final collision boundary between them would have formed during the Pa-African time of 530-550 Ma.. |
| 52. |
Graphite with growth spirals in Mg-Al-rich granulite from the area to the south of Syowa Station, Antarctica. |
| 53. |
Compositional variation of monazite in leucocratic vein from Sor Rondane Mountains, East Antarctica. |
| 54. |
小山内 康人, 豊島 剛志, 外田 智千, 馬場 壮太郎, 中野 伸彦, 足立 達朗, 大和田 正明, 白石 和行, 本吉 洋一, 東南極ドロンイングモードランド・セールロンダーネ山地のパンアフリカン衝突型変成作用, 日本鉱物科学会年会講演要旨集, 2010.04. |
| 55. |
Orthopyroxene- and/or spinel-bearing symplectites in mafic granulite from the Sor Rondane Mountains, East Antarctica. |
| 56. |
Yasuhito Osanai, Tsuyoshi Toyoshima, Sotaro Baba, Tomokazu Hokada, Nobuhiko Nakano, Tatsuro Adachi, Masaaki Owada, Kazuyuki Shiraishi, Yoichi Motoyoshi, Pan-African collision metamorphism in the Sør Rondane Mountains, Eastern Dronning Maud Land, East Antarctica, 第28回極域地学シンポジウム, 2008.10. |
| 57. |
Yasuhito Osanai, Kazuyuki Shiraishi, Tsuyoshi Toyoshima, Masaaki Owada, Sotaro Baba, Tomokazu Hokada, Nobuhiko Nakano, Yoichi Motoyoshi, Tatsuro Adachi, Pan-African Collision Metamorphism in the Sør Rondane Mountains, Eastern Dronning Maud Land, East Antarctica, The Gondwana 13, 2008.09. |
| 58. |
Tatsuro Adachi, Ichiro Iwasaki, Daniel J. Dunkley, Tomokazu Hokada, P-T-t path of the Yoshimi Metamorphic Rocks from the Northeastern Part of the Kanto Mountains, Central Japan, 4th International Symposium on Gondwana to Asia, 2007.11. |
| 59. |
Metamorphic evolution of Sor Rondane Mountains, Doronning Maud Land, East ANtarctica: reconsideration
東南極セールロンダーネ山地に広域的に分布する苦鉄質変成岩類の化学組成により原岩構成に基づき帯区分され，NW-SE方向に帯状配列するA～D帯とENE-WSW方向のE～G帯である． A～D帯の最高変成条件は，約８kbar，900℃が見積もられ，メソパーサイト，転移ピジョン輝石などの超高温変成作用の痕跡もみとめられる．これらの中で，昇温期変成作用の痕跡を残すザクロ石中の残留藍晶石・十字石はA～C帯のみに見出され，後退変成過程では珪線石安定領域から紅柱石の安定な条件に至る．D帯では後退変成作用時に２次的生成された藍晶石−黒雲母−石英共生がみとめられる．一方E～G帯では緑色片岩相から珪線石や十字石−石英共生が安定な角閃岩相の変成条件しか見出されず，後退変成過程で紅柱石が生成されている．これらの３つの異なる変成過程は， SRS形成時の大陸衝突にともなう衝突型変成作用の進行過程で形成されたことが考えられる．. |
| 60. |
Kazumasa Aoki, Tatsuro Adachi, Minoru Kikuchi, Yoshihide Ogasawara, Petrology of UHP calcite marble from the Kokchetav Massif, American Geophysical Union Fall Meeting, 2004.12. |
| 61. |
Yoshihide Ogasawara, Tatsuro Adachi, Kazumasa Aoki, Occurrence of microdiamond in UHP calcite marble from the Kokchetav Massif, American Geophysical Union Fall Meeting, 2004.12. |
| 62. |
Tatsuro Adachi, Yoshihide Ogasawara, Laser Raman study on microdimond in UHP marbles from the Kokchetav Massif, American Geophysical Union Fall Meeting, 2004.12. |
