Small faults and kink bands in the Nankai accretionary complex: Textural observations from Site 808 of ODP Leg 131
Author:
Publisher
Wiley
Subject
Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1440-1738.1997.tb00169.x/fullpdf
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1. Back-scattered electron imagery of the tectonic fabrics of some fine-grained sediments: Implications for fabric nomenclature and deformation processes
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3. Microfabric and Physical Properties Characteristics of a Consolidated Clay Section: ODP Site 697, Weddell Sea
4. Faultlike features in abyssal plain sediments: Possible dewatering structures
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2. Evidence for mechanical decoupling of the upper plate at the Nankai subduction zone: Constraints from core-scale faults at NantroSEIZE Sites C0001 and C0002;Geochemistry, Geophysics, Geosystems;2013-03
3. Multiple causes of diagenetic fabric anisotropy in weakly consolidated mud, Nankai accretionary prism, IODP Expedition 316;Journal of Structural Geology;2010-12
4. Origin of deformation bands in argillaceous sediments at the toe of the Nankai accretionary prism, southwest Japan;Journal of Structural Geology;2004-02
5. History of metamorphic fluids along outcrop-scale faults in a Paleogene accretionary prism, SW Japan: Implications for prism-scale hydrology;Geochemistry, Geophysics, Geosystems;2003-09
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