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《Earthquake》 2002-04
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The main characteristics of deep and superficial fluid pathway at northern edge of west Qinling

SHI Jin, LIU Yaowei(Lanzhou Institute of Seismology, CSB, Lanzhou 730000, China)  
According to the newest research result of global underground fluid network, using the geophysical sounding data and high temperature and highpressure geochemistry experiment results, we have researched the mechanism and main characteristics of the fluid pathway in lithosphere at northern edge of west Qinling. Our results indicate that there is fluid pathway throughout the lithosphere in our researching district with obvious characteristics. Two main factors have played vital role in the forming process: the diapering of the fluid in the asthenosphere and the structure movement. The fluid in the pathway has acted very important operation in heat conducting and this caused a series of complicate geochemistry reaction and material redistribution. The main aspect is: ① dehydration of the rocks in middlelower crust; ② partial melting of rocks; ③ different density rocks differentiate each other, low density material move upward and forming the high velocity and high conductivity layer in middle crust, high density material moving downward and forming the high velocity layer in the bottom of low crust.
【Fund】: 十五"国家科技攻关项目(2001BA601B0203)
【CateGory Index】: P315.72
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