THE GEOLOGY AND STRUCTURAL EVOLUTION OF A CALEDONIAN FOLD AND DUCTILE THRUST ZONE, KYLE OF TONGUE REGION, SUTHERLAND, NORTHERN SCOTLAND

被引:55
作者
HOLDSWORTH, RE
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D O I
10.1144/gsjgs.146.5.0809
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P [天文学、地球科学];
学科分类号
07 ;
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页码:809 / 823
页数:15
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共 82 条
[1]  
Barber A. J., 1976, SCOTTISH J GEOLOGY, V20, P35, DOI 10.1144/sjg12010035
[2]  
BARR D, 1986, GEOL SOC AM BULL, V97, P754, DOI 10.1130/0016-7606(1986)97<754:CDTIAP>2.0.CO
[3]  
2
[4]  
Barr D., 1985, MIGMATITES, P225
[5]   ON THE INTERNAL GEOMETRY OF MYLONITE ZONES [J].
BELL, TH ;
HAMMOND, RL .
JOURNAL OF GEOLOGY, 1984, 92 (06) :667-686
[6]  
BRUN JP, 1985, TECTONICS, V5, P215
[7]   GEOLOGICAL CONSTRAINTS, STRUCTURAL EVOLUTION, AND DEEP GEOLOGY OF THE NORTHWEST SCOTTISH CALEDONIDES [J].
BUTLER, RWH ;
COWARD, MP .
TECTONICS, 1984, 3 (03) :347-365
[8]   DESCRIPTION AND ORIGIN OF BANDED DEFORMATION STRUCTURES .1. REGIONAL STRAIN, LOCAL PERTURBATIONS, AND DEFORMATION BANDS [J].
COBBOLD, PR .
CANADIAN JOURNAL OF EARTH SCIENCES, 1977, 14 (08) :1721-1731
[9]   DEVELOPMENT OF SHEATH FOLDS IN SHEAR REGIMES [J].
COBBOLD, PR ;
QUINQUIS, H .
JOURNAL OF STRUCTURAL GEOLOGY, 1980, 2 (1-2) :119-126
[10]  
Coward M.P., 1987, PETROLEUM GEOLOGY NW, P687