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《EARTH SCIENCE FRONTIERS》 1998-S1
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CONSTRAINTS AND THEIR MECHANISM ON THE PETROGENIC AND METALLOGENIC MODEL FOR COLLISION OROGENESIS

Chen Yanjing(Department of Geology, Peking University, Beijing, 100871)[KH*3/4D]  
Based on analysis of activation and outward movement of materials of the intracontinental subducting slab, the petrogenic and metallogenic model was established for collision orogenesis. In the model, zones of hydrothermal deposits batholithic granites and porphyries develop at the overlapping slab as the distance increasing from the intracontinental subduction geosuture. This paper discusses its zonational variations and mechanisms with changes of angle, speed geothermal gradient and chemical composition of subducting slab, as well as imbrication of multiple intracontinental subduction regimes. The effectivity and rationality of the petrogenic and metallogenic model for collision orogenesis are clearly shown. It provides a theoretical guide for ore exploration in collision orogenic belts or intracontinental subducting areas.
【Fund】: 国家“九五”攀登预研95-预-39号项目 国家“九五”攻关 自然科学基金
【CateGory Index】: P542.2,P628.3
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