Variability in oceanic crustal thickness and structure: Multichannel seismic reflection results from the northern East Pacific Rise-Reference-Cited by-同舟云学术

Variability in oceanic crustal thickness and structure: Multichannel seismic reflection results from the northern East Pacific Rise

Published:1996-08-10 Issue:B8 Volume:101 Page:17951-17975
ISSN:0148-0227
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res.

Author:

Barth G. A.,Mutter J. C.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Link

http://www.agu.org/journals/jb/v101/iB08/96JB00814/96JB00814.pdf

Reference137 articles.

1. DSDP Hole 504B, The first reference section over one kilometer through layer 2 of the oceanic crust;Anderson;Nature,1982

2. An examination of along-axis variation of magma chamber width and crustal structure on the East Pacific Rise between 12°20′N and 13°30′N (abstract);Babcock;Eos Trans. AGU, Fall Meeting Suppl.,1992

3. Barth , G. A. A Marine seismic study of the East Pacific Rise: 8°50′N to 13°30′N New York 1991

4. Plate boundary structures to Moho depths within the 9°03′N and 12°54′N overlapping spreading centers of the East Pacific Rise;Barth;Earth Planet. Sci. Lett.,1994

5. Oceanic crust thickens approaching the Clipperton Fracture Zone;Barth;Mar. Geophys. Res.,1994

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