DEVELOPMENT OF MYLONITIC SHEAR ZONE WITHIN MILLAS GRANITE (EASTERN PYRENEES) - EVIDENCE OF DUCTILE VARISCAN OR PYRENEAN DEFORMATION

被引：0
|
作者：
SOLIVA, J
PISTRE, S
ARTHAUD, F
BRUNEL, M
机构：
来源：
COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE II | 1992年 / 314卷 / 06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：
Reverse mylonitic shear zone have been evidenced at the southern border of the Millas granitic pluton. Ductile deformation is characterized by East-West trending, steep south dipping mylonitic bands which are several hundred metres thick. Reverse faulting kinematics is consistent with the main compressive stress-field trajectories (sigma-1) determined by brittle microstructures analysis. This ductile deformation is proposed to be the result of the Hercynian and/or Pyrenean shortening.
引用
收藏
页码：611 / 618
页数：8
相关论文
共 33 条
1234