Paleomagnetic constraints on deformation models for uppermost oceanic crust exposed at the Hess Deep Rift: Implications for axial processes at the East Pacific Rise

Author:

Varga Robert J.1,Karson Jeffrey A.2,Gee Jeffrey S.3

Affiliation:

1. Department of Geology; College of Wooster; Wooster Ohio USA

2. Division of Earth and Ocean Sciences; Duke University; Durham North Carolina USA

3. Scripps Institution of Oceanography; University of California, San Diego; 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

Reference85 articles.

1. A test of the geocentric dipole hypothesis from an analysis of the skewness of the central marine magnetic anomaly;Acton;Earth Planet. Sci. Lett.,1996

2. A mechanism for decoupling within the oceanic lithosphere revealed in the Troodos ophiolite;Agar;Nature,1995

3. Spreading structure of the Troodos ophiolite, Cyprus: Some paleomagnetic constraints;Allerton;Geology,1987

4. Structures and magnetic fabrics from the lower sheeted dike complex of Hole 504B reoriented using stable magnetic remanence;Allerton;Proc. Ocean Drill. Programs Sci. Results,1995

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