Thermal-mechanical behavior of oceanic transform faults: Implications for the spatial distribution of seismicity-Reference-Cited by-同舟云学术

Thermal-mechanical behavior of oceanic transform faults: Implications for the spatial distribution of seismicity

Published:2010-07 Issue:7 Volume:11 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Roland Emily¹,Behn Mark D.²,Hirth Greg³

Affiliation:

1. MIT-WHOI Joint Program in Oceanography, Department of Marine Geology and Geophysics; Woods Hole Oceanographic Institution; 266 Woods Hole Road,; Woods Hole; Massachusetts; 02540; USA

2. Department of Geology and Geophysics; Woods Hole Oceanographic Institution; 266 Woods Hole Road,; Woods Hole; Massachusetts; 02543; USA

3. Department of Geological Sciences; Brown University; 324 Brook Street,; Providence; Rhode Island; 02912; USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

http://www.agu.org/journals/gc/gc1007/2010GC003034/2010GC003034.pdf

Reference50 articles.

1. Earthquake slip on oceanic transform faults;Abercrombie;Nature,2001

2. Mechanisms of normal fault development at mid-ocean ridges;Behn;J. Geophys. Res.,2002

3. Thermal structure of oceanic transform faults;Behn;Geology,2007

4. Transform fault earthquakes in the North Atlantic: Source mechanisms and depth of faulting;Bergman;J. Geophys. Res.,1988

5. Geodyn. Ser.;Bird,2002

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