ZONING OF THE ECLOGITE-FACIES METAMORPHISM IN THE CHAMPTOCEAUX NAPPE (ARMORICAN MASSIF, FRANCE)

被引：0

作者：

BALLEVRE, M ^{[1
]}

MARCHAND, J ^{[1
]}

机构：

[1] UNIV NANTES,PETR & MINERAL LAB,F-44072 NANTES,FRANCE

来源：

COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE II | 1991年 / 312卷 / 07期

关键词：

D O I：

暂无

中图分类号：

O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];

学科分类号：

07 ; 0710 ; 09 ;

摘要：

Mineral assemblages within metapelites and metabasites from the lower unit of the Champtoceaux nappe (Armorican massif, France) reveal regionally increasing P-T conditions during the eclogite-facies event. These differences are related to variations in burial depth at the onset of the Hercynian collision.

引用

页码：705 / 711

页数：7

共 28 条

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