How crack porosity and shape control seismic velocities in the upper oceanic crust: Modeling downhole logs from Holes 504B and 1256D-Reference-Cited by-同舟云学术

How crack porosity and shape control seismic velocities in the upper oceanic crust: Modeling downhole logs from Holes 504B and 1256D

Published:2010-04 Issue:4 Volume:11 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Carlson R. L.¹

Affiliation:

1. Department of Geology and Geophysics; Texas A&M University; College Station; Texas; 77843-3115; USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

http://www.agu.org/journals/gc/gc1004/2009GC002955/2009GC002955.pdf

Reference40 articles.

1. Hydrothermal alteration of a section of upper oceanic crust in the eastern equatorial Pacific: A synthesis of results from Site 504 (DSDP legs 69, 70, and 83, and ODP legs 111, 137, 140, and 148);Alt;Proc. Ocean Drill. Program Sci. Results,1996

2. In situ electrical resistivity and bulk porosity of the oceanic crust Costa Rica Rift;Becker;Nature,1982

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