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Missing ophiolitic rocks along the Mae Yuam Fault as the Gondwana-Tethys divide in north-west Thailand
https://doi.org/10.24517/00010923
https://doi.org/10.24517/00010923c3588113-c75f-4123-888c-93e33736b09e
名前 / ファイル | ライセンス | アクション |
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SC-PR-ARAI-S-119.pdf (616.2 kB)
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2017-10-03 | |||||
タイトル | ||||||
タイトル | Missing ophiolitic rocks along the Mae Yuam Fault as the Gondwana-Tethys divide in north-west Thailand | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | journal article | |||||
ID登録 | ||||||
ID登録 | 10.24517/00010923 | |||||
ID登録タイプ | JaLC | |||||
著者 |
Hisada, Ken-ichiro
× Hisada, Ken-ichiro× Sugiyama, Masaaki× Ueno, Katsumi× Charusiri, Punya× Arai, Shoji |
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著者別表示 |
久田, 健一郎
× 久田, 健一郎× 荒井, 章司 |
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書誌情報 |
Island Arc 巻 13, 号 1, p. 119-127, 発行日 2004-03-01 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 1038-4871 | |||||
NCID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA10848628 | |||||
DOI | ||||||
関連タイプ | isIdenticalTo | |||||
識別子タイプ | DOI | |||||
関連識別子 | 10.1111/j.1440-1738.2003.00412.x | |||||
出版者 | ||||||
出版者 | Blackwell Publishing | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | Thailand comprises two continental blocks: Sibumasu and Indochina. The clastic rocks of the Triassic Mae Sariang Group are distributed in the Mae Hong Son-Mae Sariang area, north-west Thailand, which corresponds to the central part of Sibumasu. The clastic rocks yield abundant detrital chromian spinels, indicating a source of ultramafic/mafic rocks. The chemistry of the detrital chromian spinels suggests that they were derived from three different rock types: ocean-floor peridotite, chromitite and intraplate basalt, and that ophiolitic rocks were exposed in the area, where there are no outcrops of them at present. Exposition of an ophiolitic complex denotes a suture zone or other tectonic boundary. The discovery of chromian spinels suggests that the Gondwana-Tethys divide is located along the Mae Yuam Fault zone. Both paleontological and tectonic aspects support this conclusion. © 2004 Blackwell Publishing Asia Pty Ltd. | |||||
著者版フラグ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 |