TRANSCRYSTALLINE SHEAR FRACTURING AND PSEUDOTACHYLITE GENERATION IN A META-ANORTHOSITE (HARRIS, SCOTLAND)

被引:21
作者
MACAUDIERE, J [1 ]
BROWN, WL [1 ]
机构
[1] UNIV NANCY 1,FAC SCI,PETROL GEOCHIM LAB,F-54506 VANDOEUVRE NANCY,FRANCE
关键词
D O I
10.1016/0191-8141(82)90031-1
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:395 / 406
页数:12
相关论文
共 30 条
[1]   MECHANISM OF FRICTIONAL FUSION IN FAULT ZONES [J].
ALLEN, AR .
JOURNAL OF STRUCTURAL GEOLOGY, 1979, 1 (03) :231-&
[2]  
BORG I, 1966, TECTONOPHYSICS, V3, P249, DOI DOI 10.1016/0040-1951(66)90019-9
[3]  
BORGES FS, 1980, J STRUCT GEOL, V2, P273
[4]   DUCTILE SHEAR ZONES IN A META-ANORTHOSITE FROM HARRIS, SCOTLAND - TEXTURAL AND COMPOSITIONAL CHANGES IN PLAGIOCLASE [J].
BROWN, WL ;
MACAUDIERE, J ;
OHNENSTETTER, M .
JOURNAL OF STRUCTURAL GEOLOGY, 1980, 2 (1-2) :281-&
[5]  
FRANCIS PW, 1973, EARLY PRECAMBRIAN SC, P95
[6]  
Griggs D.T., 1960, GEOL SOC AM MEM, V79, P39
[8]  
Heard H. C., 1970, EXPT NATURAL ROCK DE, P375
[9]  
HEYES AJ, 1978, THESIS U LONDON
[10]  
Jehu T.J., 1926, T ROY SOC EDINBURGH, V54, P467, DOI https://doi.org/10.1017/S0080456800027678