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《GEOTECTONICA ET METALLOGENIA》 1999-04
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ON THE MESOZOIC CONTINENTAL ACTIVATION AND ITS MULTIPLE DYNAMICS SYSTEM──TAKING HUNAN PROVINCE AS AN EXAMPLE

LIANG Xin-quan; FAN Wei-ining; LIN Ge; WANG Yue-Jun(Changsha Institute of geotectonics, Academia Sinica, Changsha 410013, China)  
Mesozoic continental activation is an important typical problem in understanding the intracontinental deformation and tectonic evolution. A series of problems including Mesozoic tectonic deformation, large-area magmatism and metallogeny etc. could not be well explained by the Previous hypothesis Of single subduction and collision. An interwoven array of back-thrust and opposite-thrust structural belts were distributed over the Hunan region. It is indicated that at least two sets of tectonic systems of inverse thrust, shear and nappe structules in opposite direction developed. They would be the result of multiple movement deformation during different evolution periods of crustoblocks. So we Proposed a synthetic model affected by composition, accretion-collision, transformation and superimposition of the multiple dynamics system, of which thinning-thickening process of lithosphere brought into by setting convergence-type mantle creep-now is the cmcial reason of Mesozoic continental activation. However, the long-distance effect Of the tectonic setting of the circum--Pacific, the Tethys setting and the margin orogenic belt are the external factors inducing crust movement and deformation.
【Fund】: 中国科学院资源生态环境重点项目
【CateGory Index】: P541
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