Deformation features of gneiss and UHP eclogite from ductile shear zone and its relation with seismic velocity anisotropy: Evidences from core samples at depth of 680 ∼ 1200m of CCSD

Acta Petrologica Sinica

Volumn 20, Issue 1, 2004, Pages 97-108

  Chen, Yi ^a,b   Jin, ZhenMin ^a   Ou, XinGong ^a   Jin, ShuYan ^a   Xu, HaiJun ^a  

^a CHINA UNIVERSITY OF GEOSCIENCES   (China)

^b INSTITUTE OF GEOLOGY AND GEOPHYSICS   (China)

Author keywords

Anisotropy; Chinese Continental Scientific Drilling (CCSD); Ductile shear zone; Gneiss; Seismic deep reflection; UHP eclogite

Indexed keywords

ACOUSTIC WAVE VELOCITY; ANISOTROPY; METAMORPHIC ROCKS; MICA; QUARTZ; REFLECTION; SEISMIC WAVES; SEISMOLOGY; SHEAR WAVES; STRUCTURAL GEOLOGY; VELOCITY; WAVE PROPAGATION;

CONTINENTAL SCIENTIFIC DRILLINGS; DUCTILE SHEAR ZONE; ECLOGITES; GNEISS; LATTICE PREFERRED ORIENTATION; P- AND S-WAVE VELOCITIES; SHAPE PREFERRED ORIENTATIONS; TEMPERATURE AND PRESSURES;

SHEAR FLOW;

CHINESE CONTINENTAL SCIENTIFIC DRILLING PROJECT; DEFORMATION; ECLOGITE; GNEISS; OROGENIC BELT; SEISMIC ANISOTROPY; SHEAR ZONE; ULTRAHIGH PRESSURE METAMORPHISM;

ASIA; CHINA; DONGHAI; EURASIA; FAR EAST; JIANGSU; SULU BELT;

EID: 84977997077     PISSN: 10000569     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Article

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