The use of asymmetric pressure shadows in mylonites to determine the sense of shear-Reference-Cited by-同舟云学术

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The use of asymmetric pressure shadows in mylonites to determine the sense of shear

Published:1988-01 Issue:4 Volume:10 Page:347-360
ISSN:0191-8141
Container-title:Journal of Structural Geology
language:en
Short-container-title:Journal of Structural Geology

Author:

Takagi Hideo,Ito Mayumi

Publisher

Elsevier BV

Subject

Geology

Reference24 articles.

1. Orthogneiss, mylonite and non coaxial deformation of granites: the example of the South Armorican Shear Zone;Berthé;J. Struct. Geol.,1979

2. Metamorphic textures and deformation: A new mechanism for the development of syntectonic porphyroblasts and its implications for interpreting timing relationships in metamorphic rocks;De Wit;Geol. J.,1976

3. Pressure shadows and relative movements in a shear zone;Fairbairn;Trans. Am. Geophys. Union,1950

4. Microtectonic evidence for eastward ductile shear in the Jurassic orogen of SW Japan;Faure;J. Struct. Geol.,1985

5. Distortion of planar structures around rigid spherical bodies;Ghosh;Tectonophysics,1975

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4. The ductile shear zone in granitoid of the Central Anatolian Crystalline Complex, Turkey: Implications for the origins of the Tuzgölü basin during the Late Cretaceous extensional deformation;Journal of Asian Earth Sciences;2009-04

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