The influence of porosity and crack morphology on seismic velocity and permeability in the upper oceanic crust

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

Reference74 articles.

1. DSDP Hole 504B, the first reference section over 1 km through Layer 2 of the oceanic crust;Anderson;Nature,1982

2. 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. ODP Sci. Results,1996

3. Subsurface structure of a submarine hydrothermal system in ocean crust formed at the East Pacific Rise, ODP/IODP Site 1256;Alt;Geochem. Geophys. Geosyst.,2010

4. Permeability of upper oceanic basement on the eastern flank of the Juan de Fuca Ridge determined with drill-string packer experiments;Becker;J. Geophys. Res.,2000

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