The Baric Structures and Exhumation Processes of the Sogauchi Unit in the Sambagawa Belt
Journal of science of the Hiroshima University. Series C, Geology and mineralogy 9 巻 4 号
705-714 頁
1993-07-30 発行
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この文献の参照には次のURLをご利用ください : https://doi.org/10.15027/53129
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JSHUC_9-4_705.pdf
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全文
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タイトル ( eng ) |
The Baric Structures and Exhumation Processes of the Sogauchi Unit in the Sambagawa Belt
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作成者 |
SEKI Sachiyo
HARA Ikuo
SHIOTA Tsugio
HIDE Kei
TAKEDA Kenji
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収録物名 |
Journal of science of the Hiroshima University. Series C, Geology and mineralogy
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巻 | 9 |
号 | 4 |
開始ページ | 705 |
終了ページ | 714 |
抄録 |
The Sogauchi unit is developed as the Sogauchi nappe as a member of primary structure and as the Omogiyama nappe, Terano—Isozu nappe and Saredani—Kabayama—Izushi nappe as members of secondary structure. The baric structures of these nappes have been analyzed on the basis of chemical composition of amphibole in hematite—bearing basic schist. The Sogauchi nappe consists of three subunits as nappes, showing increase of pressure from the lower nappe to the upper nappe and northward increase of pressure for each nappe. The assumed isobaric lines appear to be running in WNW—ESE trend, which is slightly oblique to the general trend of mineral lineation (Lm), and the lower pressure part of each nappe appears to be placed on the western side on the line along Lm. The displacement of the nappes during their subcretion— exhumation appears to have been of westward sense judging from quartz microtextures. The Omogiyama nappe and Saredani—Kabayama —Izushi nappe have been assumed to have been derived as nappes from the northwestern extension (higher pressure parts) of the Sogauchi nappe. However, an alternative model has also been shown for the root of the Saredani — Kabayama —Izushi nappe.
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言語 |
英語
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資源タイプ | 紀要論文 |
出版者 |
HIROSHIMA UNIVERSITY
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発行日 | 1993-07-30 |
出版タイプ | Version of Record(出版社版。早期公開を含む) |
アクセス権 | オープンアクセス |
収録物識別子 |
[ISSN] 0075-4374
[NCID] AA00706718
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