Structural evolution of preexisting oceanic crust through intraplate igneous activities in the Marcus-Wake seamount chain-Reference-Cited by-同舟云学术

Structural evolution of preexisting oceanic crust through intraplate igneous activities in the Marcus-Wake seamount chain

Published:2010-10 Issue:10 Volume:11 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Kaneda Kentaro¹,Kodaira Shuichi²,Nishizawa Azusa¹,Morishita Taisei¹,Takahashi Narumi²

Affiliation:

1. Hydrographic and Oceanographic Department; Japan Coast Guard; Tsukiji 5-3-1,; Chuo-ku, Tokyo; 104-0045; Japan

2. Institute for Research on Earth Evolution; Japan Agency for Marine-Earth Science and Technology; Showa-machi 3173-25,; Kanazawa-ku, Yokohama; 236-0001; Japan

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

http://www.agu.org/journals/gc/gc1010/2010GC003231/2010GC003231.pdf

Reference81 articles.

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4. Eruption styles of basalt in oceanic spreading ridges and seamounts: Effect of magma temperature and viscosity;Bonatti;J. Geophys. Res.,1988

5. Empirical relations between elastic wavespeeds and density in the Earth's crust;Brocher;Bull. Seismol. Soc. Am.,2005

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