Fault rotation and core complex formation: Significant processes in seafloor formation at slow-spreading mid-ocean ridges (Mid-Atlantic Ridge, 13°-15°N)

Author:

Smith Deborah K.1,Escartín Javier2,Schouten Hans1,Cann Johnson R.3

Affiliation:

1. Geology and Geophysics Department; Woods Hole Oceanographic Institution; Woods Hole; Massachusetts; 02543; USA

2. Groupe de Geosciences Marines; CNRS - IPGP; 75252; Paris; France

3. School of Earth and Environment; University of Leeds; Leeds; LS2 9JT; UK

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference73 articles.

1. New discoveries at the 12°58′N, 44°52′N, MAR: Professor Logachev-22 cruise, initial results;Beltnenev;InterRidge News,2003

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

3. 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

4. A study of the hydrothermal field at 14°45′N on the Mid-Atlantic Ridge using the MIR submersibles;Bogdanov;BridgeNews,1995

5. Aftershock sequences in the mid-ocean ridge environment: An analysis using hydroacoustic data;Bohnenstiehl;Tectonophysics,2002

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