ORTHO-MICA SCHISTS AS PRODUCTS OF SYNMETAMORPHIC DUCTILE SHEAR DEFORMATION OF GRANITES WITH MASS-TRANSFER - MAIN FEATURES AND EXAMPLES FROM THE VARISCAN FOLD BELT OF SOUTHERN FRANCE

被引:9
作者
CREVOLA, G
机构
关键词
D O I
10.1080/09853111.1987.11105139
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
引用
收藏
页码:207 / 221
页数:15
相关论文
共 93 条
[61]  
MARQUER D, 1986, THESIS RENNES
[62]  
MATTE P, 1986, B SOC GEOL FR, V2, P9
[63]   EXTENSIONAL STRUCTURES IN ANISOTROPIC ROCKS [J].
PLATT, JP ;
VISSERS, RLM .
JOURNAL OF STRUCTURAL GEOLOGY, 1980, 2 (04) :397-410
[64]  
PUPIN JP, 1976, THESIS NICE
[65]   STRAIN VARIATION IN SHEAR BELTS [J].
RAMSAY, JG ;
GRAHAM, RH .
CANADIAN JOURNAL OF EARTH SCIENCES, 1970, 7 (03) :786-+
[66]  
ROQUES M, 1941, MEM EXPL CARTE GEOL
[67]  
SANDER B, 1912, GEOL REICHSANST WIEN, V62, P219
[69]  
SEYLER M, 1983, GEOLOGIE FRANCE, P81
[70]   STRAIN AND SHAPE-FABRIC VARIATIONS ASSOCIATED WITH DUCTILE SHEAR ZONES [J].
SIMPSON, C .
JOURNAL OF STRUCTURAL GEOLOGY, 1983, 5 (01) :61-72