Crustal thickness and Moho character of the fast-spreading East Pacific Rise from 9°42′N to 9°57′N from poststack-migrated 3-D MCS data
Author:
Affiliation:
1. Department of Earth Sciences; Dalhousie University; Halifax Nova Scotia Canada
2. Lamont-Doherty Earth Observatory; Columbia University; Palisades New York USA
3. Woods Hole Oceanographic Institution; Woods Hole Massachusetts USA
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Reference78 articles.
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2. Petrology and magma chamber processes at the East Pacific Rise −9°30′N;Batiza;J. Geophys. Res.,1992
3. Mantle-crust transition zone and origin of wehrlitic magmas: Evidence from the Oman ophiolite;Benn;Tectonophysics,1988
4. Magma chambers in the Oman ophiolite: Fed from the top and the bottom;Boudier;Earth Planet. Sci. Lett.,1996
5. Seismic stratigraphy of the oceanic Moho based on ophiolite models;Brocher;Geology,1985
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