ID | 19850 |
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Sort Key | 5
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タイトル(別表記) | 岡山県に分布する白亜紀前期羽山層砕屑物質の供給源:砕屑粒の鉱物化学組成とモード組成から導かれる制約
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フルテキストURL | |
著者 |
アシード ダニエル
Department of Earth Science, University of Ghana
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抄録 | Petrographic and phase chemistry studies of detrital grains were carried out on sandstones from the Lower Cretaceous Hayama Formation, Inner Zone of Southwest Japan, to determine their provenance and the tectonic setting during the early Cretaceous. The results of the modal mineralogy suggest that the Hayama Formation has magmatic arc provenance and that deposition of the sediments took place in the back-arc areas with detritus mostly derived from the magmatic arc and rifted continental margins. The chemical compositions of chromian spinel, chlorite and sphene indicate that significant proportions of the detrital grains were derived from mafic and/or ultramafic sources. The source areas are the mafic and ophiolitic rocks in the Sangun-Renge and Akiyoshi terranes and the felsic volcanic rocks probably from either the Akiyoshi terrane or a source not presently exposed in southwest Japan. However, minor amounts of the detritus were derived from the basement rocks; i.e., carbonates and siliciclastic rocks of the Akiyoshi terrane and the metamorphosed mafic rocks of the Chizu terrane.
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キーワード | modal analysis
sandstone
mineral chemistry
provenance
Hayama Formation
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出版物タイトル |
Okayama University Earth Science Report
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発行日 | 2009-12-25
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巻 | 16巻
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号 | 1号
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出版者 | 岡山大学理学部地球科学教室
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出版者(別表記) | Department of Earth Sciences, Faculty of Science, Okayama University
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開始ページ | 29
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終了ページ | 42
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ISSN | 1340-7414
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NCID | AN10506284
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資料タイプ |
紀要論文
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OAI-PMH Set |
岡山大学
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言語 |
英語
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著作権者 | 岡山大学地球科学研究報告編集委員会
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論文のバージョン | publisher
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査読 |
無し
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NAID | |
Eprints Journal Name | esr
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