The effect of hydrothermal alteration on the seismic structure of the upper oceanic crust: Evidence from Holes 504B and 1256D-Reference-Cited by-同舟云学术

The effect of hydrothermal alteration on the seismic structure of the upper oceanic crust: Evidence from Holes 504B and 1256D

Published:2011-09 Issue:9 Volume:12 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/gc1109/2011GC003624/2011GC003624.pdf

Reference49 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. 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

3. Measurements of the permeability of the sheeted dikes in Hole 504B, ODP Leg 111;Becker;Proc. Ocean Drill. Program Sci. Results,1989

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