Detachment shear zone of the Atlantis Massif core complex, Mid-Atlantic Ridge, 30°N-Reference-Cited by-同舟云学术

Detachment shear zone of the Atlantis Massif core complex, Mid-Atlantic Ridge, 30°N

Published:2006-06 Issue:6 Volume:7 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Karson J. A.,Früh-Green G. L.¹,Kelley D. S.²,Williams E. A.³,Yoerger D. R.⁴,Jakuba M.⁴

Affiliation:

1. Department of Earth Sciences, ETH-Zurich; CH-8092; Zürich; Switzerland

2. School of Oceanography; University of Washington; Seattle; Washington; 98195; USA

3. Division of Earth and Ocean Sciences; Duke University; Durham; North Carolina; 27708; USA

4. Woods Hole Oceanographic Institution; Woods Hole; Massachusetts; 02543; USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference61 articles.

1. Orthogneiss, mylonite and noncoaxial deformation of granites: The example of the South American shear zone;Berthe;J. Struct. Geol.,1979

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

3. Seafloor mapping and sampling of the MAR 30°N oceanic core complex-MARVEL (Mid-Atlantic Ridge Vents in Extending Lithosphere) 2000;Blackman;InterRidge Newsl.,2001

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

5. Links between tectonic and serpentinization processes and their consequences for hydrothermal activity (Atlantis Massif, MAR 30°N);Boschi;Geophys. Res. Abstr.,2003

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