THE ATLANTIC-OCEAN OPENING - EXTENSIONAL REACTIVATION OF PALEOZOIC STRUCTURES

被引：0

作者：

PIQUE, A ^{[1
]}

LAVILLE, E ^{[1
]}

机构：

[1] UNIV CAEN,LAB GEOL NORMANDIE OCCIDENTALE,F-14032 CAEN,FRANCE

来源：

COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE II | 1993年 / 317卷 / 10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：

Comparison of the Upper Triassic-Lower Liassic sedimentary and magmatic rocks of the two sides of the central Atlantic suggests that the Atlantic rift was asymmetrical and controlled by detachment faults. These extensive structures may represent Palaeozoic thrusts reactivated in a extensional regime, following a post-Alleghanian lithospheric delamination.

引用

页码：1325 / 1332

页数：8

共 33 条

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