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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.
Copyright 2003 by the American Geophysical Union.
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