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
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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.
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页码：705 / 711
页数：7
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