書誌事項
- タイトル別名
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- Compositions of detrital spinels from Lower Cretaceous Sasayama Group, Hyogo Prefecture, Japan: Constraints on source lithology and tectonic setting.
- Compositions of detrital spinels from L
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説明
Sandstones from the Lower Cretaceous Sasayama Group contain chromian spinel and chromian magnetite as accessory minerals. Microprobe analyses show that the chromian spinel has Cr/(Cr+Al) ratios between 0.21 and 0.59, Mg/(Mg+Fe2+) ratios between 0.39 and 0.72, Fe3+/(Fe3+Al+Cr) ratios less than 0.10, and TiO2 contents less than 0.4 wt%. Comparison with spinels from literature suggests that they were derived from Alpine-type peridotite. The lithology of the Alpine-type peridotite was mostly clinopyroxene-bearing harzburgite and/or refractory lherzolite with subordinate cumulates. Chromitite did not contribute detritus to the Sasayama basin.<br> The chemistry of the chromian spinel further suggests that the Alpine-type peridotite source was most probably formed under an oceanic back-arc basin rather than mid-oceanic ridge setting. Chemical compositions of chromian magnetite indicate that the Alpine-type peridotite provenance was subjected to metamorphism of up to the lower amphibolite facies. In comparison with ophiolitic rocks widely distributed north of the study area, no specific provenance is constrained although the ultramafic rocks distributed in the Chugoku Zone are the most likely candidates for provenance.
収録刊行物
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- 岩鉱
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岩鉱 93 (1), 27-41, 1998
一般社団法人 日本鉱物科学会
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詳細情報 詳細情報について
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- CRID
- 1390282681210229120
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- NII論文ID
- 10002089796
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- NII書誌ID
- AN10047992
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- COI
- 1:CAS:528:DyaK1cXit12htrw%3D
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- ISSN
- 18813275
- 09149783
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- NDL書誌ID
- 4446245
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- 本文言語コード
- en
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- データソース種別
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- JaLC
- NDLサーチ
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- 使用不可