Deformation and in situ stress in the Nankai Accretionary Prism from resistivity-at-bit images, ODP Leg 196-Reference-Cited by-同舟云学术

Deformation and in situ stress in the Nankai Accretionary Prism from resistivity-at-bit images, ODP Leg 196

Published:2004-01 Issue:2 Volume:31 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

McNeill L. C.¹,Ienaga M.²,Tobin H.³,Saito S.⁴,Goldberg D.⁵,Moore J. C.⁶,Mikada H.⁴

Affiliation:

1. Southampton Oceanography Centre; University of Southampton; Southampton UK

2. Ocean Research Institute; The University of Tokyo; Tokyo Japan

3. Department of Earth and Environmental Science; New Mexico Institute of Mining and Technology; Socorro New Mexico USA

4. Deep Sea Research Center, JAMSTEC; Yokosouka Japan

5. Borehole Research Group, Lamont-Doherty Earth Observatory; Columbia University; Palisades New York USA

6. Department of Earth Sciences; University of California; Santa Cruz California USA

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference13 articles.

1. Fluid flow along potentially active faults in crystalline rock;Barton;Geology,1995

2. Fracture porosity in the décollement zone of Nankai accretionary wedge using Logging While Drilling resistivity data;Bourlange;Earth Planet. Sci. Lett.,2003

3. Relationships among in-situ stress, fractures and faults, and fluid flow: Monterey Formation, Santa Maria Basin, California;Finkbeiner;AAPG Bull.,1997

4. Deformation bands from the toe of the Nankai accretionary prism;Karig;J. Geophys. Res.,1990

5. Sci. Res.;Lallemant,1993

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