John, Barbara E. and Cheadle, Michael J. (2010): Deformation and alteration associated with oceanic and continental detachment fault systems; are they similar?

Leg/Site/Hole:
IODP 304 U1309
IODP 305 U1309
Identifier:
2011-004140
georefid

10.1029/2008GM000772
doi

Creator:
John, Barbara E.
University of Wyoming, Department of Geology & Geophysics, Laramie, WY, United States
author

Cheadle, Michael J.
University of Kiel, Leibnitz Institute of Marine Sciences, Germany
author

Identification:
Deformation and alteration associated with oceanic and continental detachment fault systems; are they similar?
2010
In: Rona, Peter A. (editor), Devey, Colin W. (editor), Dyment, Jerome (editor), Murton, Bramley J. (editor), Diversity of hydrothermal systems on slow spreading ocean ridges
American Geophysical Union, Washington, DC, United States
188
175-205
English
Serial
Coverage:Geographic coordinates:
North:30.1100
West:-42.0700East: -42.0600
South:30.1000

Solid-earth geophysics; Atlantic Ocean; Atlantis Massif; basement; bathymetry; Chemehuevi Mountains; crust; decollement; deformation; detachment faults; Expeditions 304/305; extension tectonics; faults; gabbros; igneous rocks; Integrated Ocean Drilling Program; IODP Site U1309; Landsat; metamorphic core complexes; metamorphic rocks; Mid-Atlantic Ridge; mylonites; nesosilicates; North Atlantic; oceanic crust; olivine; olivine group; orthosilicates; plate tectonics; plutonic rocks; remote sensing; rifting; sea-floor spreading; silicates; spreading centers; strain; tectonics; three-dimensional models; topography;

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