Gravity lineaments of the Cocos Plate: Evidence for a thermal contraction crack origin-Reference-Cited by-同舟云学术

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Gravity lineaments of the Cocos Plate: Evidence for a thermal contraction crack origin

Published:2011-07 Issue:7 Volume:12 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Cormier Marie-Helene¹,Gans Kathleen D.²,Wilson Douglas S.³

Affiliation:

1. Department of Geological Sciences; University of Missouri; Columbia; Missouri; 65211; USA

2. U.S. Geological Survey; 345 Middlefield Road,; Menlo Park; California; 94025; USA

3. Department of Earth Science and Marine Science Institute; University of California; Santa Barbara; California; 93106; USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

http://www.agu.org/journals/gc/gc1107/2011GC003573/2011GC003573.pdf

Reference82 articles.

1. An examination of along-axis variation of magma chamber width and crustal structure on the East Pacific Rise between 13°30′N and 12°20′N;Babcock;J. Geophys. Res.,1998

2. Non-hotspot volcano chains originating from small-scale sublithospheric convection;Ballmer;Geophys. Res. Lett.,2007

3. Geological and petrologic evolution of seamounts near the EPR based on submersible and camera study;Batiza;Mar. Geophys. Res.,1989

4. When does small-scale convection begin beneath oceanic lithosphere?;Buck;Nature,1985

5. Convection beneath young oceanic lithosphere: Implications for thermal structure and gravity;Buck;J. Geophys. Res.,1986

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