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Petrology of peridotite in the western Mirdita ophiolite, Albania: origin of plagioclase peritotite.
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- Inamura Masayuki
- Kanazawa university
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- Morishita Tomoaki
- Kanazawa university
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- Tamura Akihiro
- Kanazawa university
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- Dilek Yildrim
- Miami university
Bibliographic Information
- Other Title
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- アルバニア, ミルディータオフィオライト西帯かんらん岩の岩石学：斜長石かんらん岩の起源
Description
Based on the characteristics of geochemistry of volcanic rocks, Mirdita ophiolite are divided into western Mirdita ophiolite and eastern Mirdita ophiolite. The western part contains MORB-type volcanics, on the other hand, eastern contains SSZ-type volcanics. Gomsiqe massif is composed of mainly lherzolite, gabbro, dunite, orthopyrozenite. Puke massif is composed of mainly highly deformed plagioclase lherzolite, gabbro, troctolite, harzburgite, dunite. It is possible to explain that lherzolite in gomsiqe has experienced 5-13% partial melting. On the other hand, peridotite in puke massif has influenced by melt impregnation.<br>
Journal
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- Abstracts for Annual Meeting of Japan Association of Mineralogical Sciences
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Abstracts for Annual Meeting of Japan Association of Mineralogical Sciences 2012 (0), 217-, 2012
Japan Association of Mineralogical Sciences
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Keywords
Details 詳細情報について
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- CRID
- 1390001205547209344
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- NII Article ID
- 130005468373
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- Text Lang
- ja
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- Data Source
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- JaLC
- CiNii Articles
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- Abstract License Flag
- Disallowed