Geochemistry of basalt from the North Gorda segment of the Gorda Ridge: Evolution toward ultraslow spreading ridge lavas due to decreasing magma supply-Reference-Cited by-同舟云学术

Geochemistry of basalt from the North Gorda segment of the Gorda Ridge: Evolution toward ultraslow spreading ridge lavas due to decreasing magma supply

Published:2008-04 Issue:4 Volume:9 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Davis A. S.¹,Clague D. A.¹,Cousens B. L.²,Keaten R.¹,Paduan J. B.¹

Affiliation:

1. Monterey Bay Aquarium Research Institute; 7700 Sandholdt Road,; Moss Landing; California; 95039-6039; USA

2. Ottawa-Carleton Geoscience Centre, Department of Earth Sciences; Carleton University; 1125 Colonel By Drive,; Ottawa, Ontario; Canada; K1S 5B6

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference76 articles.

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2. Rhyodacites, andesites, ferrobasalts and ocean tholeiites from the Galapagos spreading center;Byerly;Earth Planet. Sci. Lett.,1976

3. The 1996 Gorda Ridge eruption: Geologic mapping, sidescan sonar, and SeaBeam comparison results;Chadwick;Deep Sea Res., Part II,1998

4. Petrology and Sr, Nd, and Pb isotope geochemistry of mid-ocean ridge basalt glasses from the 11°45′N to 15°00′N segment of the East Pacific Rise;Castillo;Geochem. Geophys. Geosyst.,2000

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