Waning magmatic activity along the Southern Explorer Ridge revealed through fault restoration of rift topography-Reference-Cited by-同舟云学术

Waning magmatic activity along the Southern Explorer Ridge revealed through fault restoration of rift topography

Published:2013-05 Issue:5 Volume:14 Page:1609-1625
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Deschamps A.¹,Tivey M. A.²,Chadwick W. W.³,Embley R. W.⁴

Affiliation:

1. Université de Brest, CNRS, UMR 6538 Domaines Océaniques, OSU-IUEM, Institut Universitaire Européen de La Mer; 4 Place N. Copernic 29280 Plouzané France

2. Department of Geology and Geophysics; Woods Hole Oceanographic Institution; Woods Hole Massachusetts USA

3. Hatfield Marine Science Center; Oregon State University/CIMRS; Newport Oregon USA

4. NOAA, Pacific Marine Environmental Laboratory; Newport Oregon USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference69 articles.

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3. Beaudoin , Y. C. 2001 Physiology, geology and geochemistry of the southern explorer ridge seafloor hydrothermal site using an integrated GIS database and 3D modeling https://tspace.library.utoronto.ca/bitstream/1807/16006/1/MQ58812.pdf

4. Seismic image of undercrusted serpentine beneath a rifted margin;Boillot;Terra Nova,1992

5. Tectonic evolution of the Explorer-Northern Juan de Fuca region from 8 Ma to the present;Botros;J. Geophys. Res.,1988

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