Massive, low-temperature hydrothermal flow from a basaltic outcrop on 23 Ma seafloor of the Cocos Plate: Chemical constraints and implications-Reference-Cited by-同舟云学术

Massive, low-temperature hydrothermal flow from a basaltic outcrop on 23 Ma seafloor of the Cocos Plate: Chemical constraints and implications

Published:2008-12 Issue:12 Volume:9 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Wheat C. Geoffrey¹,Fisher Andrew T.²

Affiliation:

1. Global Undersea Research Unit; University of Alaska Fairbanks; P. O. Box 475,; Moss Landing; California; 95039; USA

2. Earth and Planetary Sciences Department and Institute for Geophysics and Planetary Physics; University of California; 1156 High Street, Santa Cruz; California; 95064; USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference64 articles.

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2. Hydrothermal cooling of midocean ridge axes: Do measured and modeled heat fluxes agree?;Baker;Earth Planet. Sci. Lett.,2007

3. large-scale lateral advection of seawater through oceanic crust in the central equatorial Pacific;Baker;Earth Planet. Sci. Lett.,1991

4. Revised tectonic boundaries in the Cocos Plate off Costa Rica: Implications for the segmentation of the convergent margin and for plate tectonic models;Barckhausen;J. Geophys. Res.,2001

5. A geological and geophysical investigation of Baby Bare, locus of a ridge-flank hydrothermal system in the Cascadia Basin;Becker;J. Geophys. Res.,2000

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