Fabrics and Seismic Properties of Ophiolites:Implications for Mantle Flow

【Author】

WANG Qin;

【Abstract】

<正>Based on ophiolite sequences,seismic velocities of rocks and seismic profiles of ocean basins,the oceanic crust-mantle boundary can be defined as the contact between the solid,ductile deformed mantle and the oceanic crust formed from magmatic rocks(i.e.,the maficultramafic stratiform plutonic complex).Meanwhile,the seismic Moho constrains the chemical boundary between

【Keywords】

Fabrics and Seismic Properties of Ophiolites:Implications for Mantle Flow;high;

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