Magnetic anisotropy of serpentinized peridotites from the MARK area: Implications for the orientation of mesoscopic structures and major fault zones-Reference-Cited by-同舟云学术

Magnetic anisotropy of serpentinized peridotites from the MARK area: Implications for the orientation of mesoscopic structures and major fault zones

Published:2002-04 Issue:B4 Volume:107 Page:EPM 4-1-EPM 4-14
ISSN:0148-0227
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res.

Author:

Lawrence Róisín M.¹,Gee Jeffrey S.²,Karson Jeffrey A.¹

Affiliation:

1. Department of Geology; Duke University; Durham North Carolina USA

2. Scripps Institution of Oceanography; La Jolla California USA

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

Reference68 articles.

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2. The Mid-Atlantic Ridge near 45°N, XVI, Serpentinized ultramafic intrusion;Aumento;Can. J. Earth Sci.,1971

3. Magnetic properties, opaque mineralogy and magnetic anisotropies of serpentinized peridotites from ODP Hole 670A near the Mid-Atlantic Ridge;Bina;Phys. Earth Planet. Inter.,1990

4. Origin of extensional core complexes: Evidence from the Mid-Atlantic Ridge at Atlantis Fracture Zone;Blackman;J. Geophys. Res.,1998

5. Serpentinite protrusions in the oceanic crust;Bonatti;Earth Planet. Sci. Lett.,1976

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