Hydrothermal plumes along segments of contrasting magmatic influence, 15°20′-18°30′N, East Pacific Rise: Influence of axial faulting-Reference-Cited by-同舟云学术

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Hydrothermal plumes along segments of contrasting magmatic influence, 15°20′-18°30′N, East Pacific Rise: Influence of axial faulting

Published:2001-09 Issue:9 Volume:2 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Baker Edward T.¹,Cormier Marie-Helene²,Langmuir Charles H.²,Zavala Karina³

Affiliation:

1. Pacific Marine Environmental Laboratory, NOAA; 7600 Sand Point Way NE, Seattle Washington 98115-6349 USA

2. Lamont-Doherty Earth Observatory; P. O. Box 1000, 61 Route 9W, Palisades New York 10964-1000 USA

3. Lamont-Doherty Earth Observatory; Palisades New York 10964-8000 USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference34 articles.

1. Recent tectonic, magmatic, and hydrothermal activity on the East Pacific Rise between 17°S and 19°S: Submersible observations;Auzende;J. Geophys. Res.,1996

2. Geological indexes of hydrothermal venting;Baker;J. Geophys. Res.,1996

3. MAPR: A new instrument for hydrothermal plume mapping;Baker;RIDGE Events,1997

4. Geophys. Monogr. Ser.;Baker,1995

5. The relationship between near-axis hydrothermal cooling and the spreading rate of midocean ridges;Baker;Earth Planet. Sci. Lett.,1996

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