Geochemistry and mineral chemistry of Pan-African amphibolites of South Sinai,Egypt

被引：0

作者：

Mohamed El-Tokhi ^{[1
]}

Bahaa Eldin Amin ^{[1
]}

Sulaiman Alabeed ^{[1
]}

Abdulla Musallam ^{[1
]}

机构：

[1] Geology Department,College of Science,United Arab Emirates University

来源：

Chinese Journal of Geochemistry | 2010年 / 29卷 / 03期

关键词：

Pan-African amphibolite; geochemistry; mineral chemistry; Sinai; Egypt;

D O I：

暂无

中图分类号：

P588.125 [];

学科分类号：

070901 ;

摘要：

In the Wadi Feiran area, amphibolites occur as inclusions, bands, linear bodies of variable thickness and irregular lenses in para-geneisses. Chemical evidence indicates that these amphibolites display an igneous origin and were derived from magma essentially of tholelitic rather than alkaline composition; transitional in character between continental and island-arc. The chemistry of amphiboles, related to pressure and temperature conditions of metamorphism, showed that they were formed under low pressure and high temperature conditions.

引用

页码：246 / 254

页数：9

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