Evolution of olivine lattice preferred orientation during simple shear in the mantle

Earth and Planetary Science Letters

Volumn 272, Issue 3-4, 2008, Pages 501-512

  Warren, Jessica M ^a   Hirth, Greg ^b   Kelemen, Peter B ^c  

^a MASSACHUSETTS INSTITUTE OF TECHNOLOGY   (United States)

^b WOODS HOLE OCEANOGRAPHIC INSTITUTION   (United States)

^c Department of Earth and Environmental Sciences   (United States)

Author keywords

Josephine Peridotite; Lattice preferred orientation; Mantle anisotropy; Olivine; Shear deformation

Indexed keywords

(1 1 1) ORIENTATION; BOUNDARY SLIDING; ELSEVIER (CO); EVOLUTION (CO); EVOLUTION MODELING; EXPERIMENTAL OBSERVATIONS; EXPERIMENTAL SAMPLES; GRAIN BOUNDARY MIGRATION (GBM); HARZBURGITES; LATTICE PREFERRED ORIENTATION (LPO); SECONDARY PEAK; SEISMIC ANISOTROPY; SHEAR DIRECTION; SHEAR PLANES; SHEAR ZONES; SIMPLE SHEAR; SLIP SYSTEMS; SOUTHWEST (CO); SUBGRAIN ROTATION;

AGRICULTURAL PRODUCTS; ALIGNMENT; CRYSTAL GROWTH; CRYSTALLOGRAPHY; EXCITONS; FABRICS; GRAIN (AGRICULTURAL PRODUCT); GRAIN BOUNDARIES; GRAIN BOUNDARY SLIDING; GRAIN GROWTH; GRAIN SIZE AND SHAPE; INTERNET PROTOCOLS; OLIVINE; SHEARING MACHINES; SILICATE MINERALS;

SHEAR STRAIN;

DEFORMATION MECHANISM; GRAIN BOUNDARY; LATTICE DYNAMICS; MANTLE; OLIVINE; PERIDOTITE; PREFERRED ORIENTATION; RECRYSTALLIZATION; SEISMIC ANISOTROPY; SHEAR STRAIN; SHEAR STRESS;

NORTH AMERICA; OREGON; UNITED STATES;

EID: 48149084276     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2008.03.063     Document Type: Article

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