Origin of deformation bands in argillaceous sediments at the toe of the Nankai accretionary prism, southwest Japan-Reference-Cited by-同舟云学术

Origin of deformation bands in argillaceous sediments at the toe of the Nankai accretionary prism, southwest Japan

Published:2004-02 Issue:2 Volume:26 Page:221-231
ISSN:0191-8141
Container-title:Journal of Structural Geology
language:en
Short-container-title:Journal of Structural Geology

Author:

Ujiie Kohtaro,Maltman Alex J.,Sánchez-Gómez Mario

Publisher

Elsevier BV

Subject

Geology

Reference24 articles.

1. Rapid nondestructive bulk density and soil-water content determination by computed tomography;Anderson;Soil Science Society of America Journal,1988

2. Orthogneiss, mylonite and non coaxial deformation of granites: the example of the South Armorican Shear Zone;Berthé;Journal of Structural Geology,1979

3. Compacting and dilating shear bands in porous rock: theoretical and experimental conditions;Bésuelle;Journal of Geophysical Research,2001

4. Deformation structures and fluid flow in the toe region of the Nankai accretionary prism;Byrne;Proceedings of the Ocean Drilling Program, Scientific Results,1993

5. Deformation bands from the toe of the Nankai accretionary prism;Karig;Journal of Geophysical Research,1990

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