Chemical Mobility and Mineralogical Variability in Edough Massif Micaschists(Annaba,Northeast Algeria)

被引：0

作者：

Hadjzobir Soraya ^{[1
]}

Bousquet Romain ^{[2
]}

机构：

[1] Department of Geology,Badji Mokhtar University

[2] Institute of Geosciences,University Potsdam

来源：

地学前缘 | 2009年 / S1期

关键词：

isocons; metamorphism; matter transfer; Edough massif; Algeria;

D O I：

暂无

中图分类号：

P574 [矿物的物理化学];

学科分类号：

070901 ;

摘要：

The Edough massif is the easternmost crystalline massif of the Maghrebides which represent the southeastern part of the West Mediterranean orogen.It occurs below the greenschist-facies Tellian units that represent the thrusted Mesozoic to Eocene passive paleomargin of northern Africa deposited on thinned continental crust.The upper unit of the Edough massif is characterized by metasedimentary rocks affected by

引用

页码：212 / 213

页数：2