ON FOLDING AND SHEAR ZONE-DEVELOPMENT - A MESOSCALE STRUCTURAL STUDY ON THE TRANSITION BETWEEN 2 DIFFERENT TECTONIC STYLES

被引：31

作者：

CARRERAS, J ^{[1
]}

CASAS, JM ^{[1
]}

机构：

[1] UNIV BARCELONA,DEPT GEOMORFOL & TECTON,BARCELONA 7,SPAIN

来源：

TECTONOPHYSICS | 1987年 / 135卷 / 1-3期

关键词：

D O I：

10.1016/0040-1951(87)90154-5

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

引用

页码：87 / 98

页数：12

共 31 条

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[3]

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[6] SIGNIFICANCE OF LINEATION AND MINOR FOLDS NEAR MAJOR THRUST FAULTS IN SOUTHERN APPALACHIANS AND BRITISH AND NORWEGIAN CALEDONIDES [J].

BRYANT, B ;

REED, JC .

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[7] EFFECTS OF FOLDING ON C-AXIS FABRICS OF A QUARTZ MYLONITE [J].

CARRERAS, J ;

ESTRADA, A ;

WHITE, S .

TECTONOPHYSICS, 1977, 39 (1-3) :3-24

[8] HERCYNIAN MYLONITE BELTS IN THE EASTERN PYRENEES - AN EXAMPLE OF SHEAR ZONES ASSOCIATED WITH LATE FOLDING [J].

CARRERAS, J ;

JULIVERT, M ;

SANTANACH, P .

JOURNAL OF STRUCTURAL GEOLOGY, 1980, 2 (1-2) :5-9

[9]

Carreras J, 1975, ACTA GEOL HISP, V10, P109

[10]

CARRERAS J, 1979, INT C SHEAR ZONES RO

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