Lower crustal variability and the crust/mantle transition at the Atlantis Massif oceanic core complex
Author:
Affiliation:
1. Scripps Institution of Oceanography; University of California, San Diego; La Jolla; California; USA
2. Woods Hole Oceanographic Institution; Woods Hole; Massachusetts; USA
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://www.agu.org/journals/gl/gl1024/2010GL045165/2010GL045165.pdf
Reference32 articles.
1. Three-dimensional structure of oceanic core complexes: Effects on gravity signature and ridge flank morphology, Mid-Atlantic Ridge 30°N;Blackman;Geochem. Geophys. Geosyst.,2008
2. Nature of the Moho transition zone in the Oman ophiolite;Boudier;J. Petrol.,1995
3. Seismic reflection imaging of an oceanic detachment fault: Atlantis megamullion (Mid-Atlantic Ridge, 30°10′N);Canales;Earth Planet. Sci. Lett.,2004
4. Seismic evidence for large-scale compositional heterogeneity of oceanic core complexes;Canales;Geochem. Geophys. Geosyst.,2008
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