Three-dimensional structure of oceanic core complexes: Effects on gravity signature and ridge flank morphology, Mid-Atlantic Ridge, 30°N-Reference-Cited by-同舟云学术

Three-dimensional structure of oceanic core complexes: Effects on gravity signature and ridge flank morphology, Mid-Atlantic Ridge, 30°N

Published:2008-06 Issue:6 Volume:9 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Blackman Donna K.¹,Karner Garry D.²,Searle Roger C.³

Affiliation:

1. Scripps Institution of Oceanography; University of California; San Diego, 9500 Gilman Drive,; La Jolla; California; 92093-0225; USA

2. ExxonMobil; P.O. Box 2189,; Houston; Texas; 77252-2189; USA

3. Department of Geological Sciences; University of Durham; South Road,; Durham; DH1 3LE; UK

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference48 articles.

1. Extremely asymmetric magmatic accretion of oceanic crust at the ends of slow-spreading ridge segments;Allerton;Geology,2000

2. Isostatic compensation of tectonic features of the Mid-Atlantic Ridge: 25-27°S;Blackman;J. Geophys. Res.,1991

3. Origin of extensional core complexes: Evidence from the Mid-Atlantic Ridge at Atlantis fracture zone;Blackman;J. Geophys. Res.,1998

4. Geology of the Atlantis Massif (MAR 30°N): Implications for the evolution of an ultramafic oceanic core complex;Blackman;Mar. Geophys. Res.,2002

5. Blackman , D. K. B. Ildefonse B. E. John Y. Ohara D. J. Miller C. J. MacLeod the Expedition 304/305 Scientists 2006 Oceanic core complex formation, Atlantis Massif Proceedings of the Integrated Ocean Drilling Program 304/305 10.2204/iodp.sp.304305.2004 Integrated Ocean Drill. Program Manage. Int., Inc. College Station, Tex.

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