American Geophysical Union Become an AGU Member
Subscribe to AGU Journals
AGU Home AGU Publications

Read Full Article (file size: 1140508 bytes)    Cited by

JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 108, NO. B9, 2407, doi:10.1029/2002JB002287, 2003

Anisotropy of electrical conductivity record of initial strain at the toe of the Nankai accretionary wedge

Pierre Henry

Laboratoire de Géologie de l'Ecole Normale Supérieure, CNRS UMR 8538, Paris, France


Laurence Jouniaux

Laboratoire de Géologie de l'Ecole Normale Supérieure, CNRS UMR 8538, Paris, France


Elizabeth J. Screaton

Department of Geology, University of Florida, Gainesville, Florida, USA


Sabine Hunze

Geowissenschaftliche Gemeinschaftsaufgaben-GCA, Hannover, Germany


Demian M. Saffer

Department of Geology and Geophysics, University of Wyoming, Laramie, Wyoming, USA


Abstract

An approach based on March's theory is applied to measurements of the anisotropy of electrical conductivity on samples and is used to quantify initial strain at the toe of the Nankai accretionary wedge. A quantitative determination of strain is possible from simple assumptions: passive reorientation of flat pores forming the porous network and existence of a linear relationship between fabric tensor and electrical conductivity tensor. We show that this simple model correctly accounts for the increase of anisotropy with compaction at a reference site located in the trench (Ocean Drilling Program drill Site 1173). At the toe of the accretionary wedge (Site 1174), development of anisotropy in the horizontal plane and concurrent reduction of vertical plane anisotropy are observed. This can be explained by 12% horizontal ductile shortening, occurring after decollement initiation but before slip on imbricate thrust faults. Anisotropy in the underthrust sequence is correctly described by vertical compaction, consistent with decoupled stress states across the decollement. At Site 1174 the magnitude of ductile strain implies at least 75 m slip on the decollement. Ductile shortening is associated with porosity loss, implying partly drained conditions above the decollement.

Received 4 November 2002; accepted 9 May 2003; published 3 September 2003.

Index Terms: 8105 Tectonophysics: Continental margins and sedimentary basins; 3022 Marine Geology and Geophysics: Marine sediments—processes and transport; 8094 Structural Geology: Instruments and techniques; 5109 Physical Properties of Rocks: Magnetic and electrical properties.


Read Full Article (file size: 1140508 bytes)    Cited by

Citation: Henry, P., L. Jouniaux, E. J. Screaton, S. Hunze, and D. M. Saffer (2003), Anisotropy of electrical conductivity record of initial strain at the toe of the Nankai accretionary wedge, J. Geophys. Res., 108(B9), 2407, doi:10.1029/2002JB002287.