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《Chinese Geology》 1997-01
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Seismic sounding data along a 420km long profile was collected in 1994. From north to south , the profile goes across three tectonic units, namely North China Block, Dabieshan Orogenic Belt and Yangtze Block By forward modeling, a crust seismic velocity model of vertical layering and horizontal blocks as well as a Poisson's ratio section were obtained. From the seismic experiment associated with geological and geochemical research, the following inferences are drawn. The crust can be divided into three layers. The upper crust exhibits a multiple nappe-sheets structure and, the middle-lower crust, ductile deformed layers. The lower crust of the Dabieshan Belt appears to be acidic in composition as a whole. The Dabieshan's UHP metamorphic rocks are characterized by a typical thin skin sheet structure. Anasynchronous dual subduction mountain-building model and opposite wedging and drawing exhumation machanism of the UHP rocks are suggested. It is quite evident that there exists a mountain root of about 6-8 km deep under the Dabieshan mountain.
【Fund】: 地矿部“八五”深部地质研究专项
【CateGory Index】: F426.1
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