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《Geology in China》 2006-06
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Orogenic-type deposits and their metallogenic model and exploration potential

CHEN Yan-Jing~(1,2)(1. KLMD, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640 Guangdong, China;2. Open Laboratory of Crust and Orogen Evolution, Department of Geology, Peking University, Beijing 100871)  
Identification of a new type mineralization often leads to discovery of a great number of ore deposits and ore provinces.Predicting and identifying new type mineralizations is an important aim of ore deposit study. To date the majority of orogenic-type gold deposits has been well shown by worldwide studies.However,the other commodities of orogenic-type are rarely discussed.This paper addresses the concept of orogenic-type deposits which formed by fluid systems mainly sourced from metamorphic devolatilization.The paper also develops genetic models for orogenic deposits at various scales,including deposit-,orefield/terrain- and province/orogen-scales.The genetic models are linked to a three-stage tectonic evolution of convergent orogens.According to these models,the transition from compression to extension of thickened accretionary or/ and collisional orogens is conducive to mineralizations; and the syn-orogenic ore-systems must be characteristically lagged behind compressional orogenesis.As case studies,orogenic-type silver,lead-zinc, molybdenum and copper deposits are reported in the paper.This implies that China has great potential for orogenic-type deposits.The logics and validity of the metallogenic models are evidenced by introduction of several successful ore deposit prediction.
【Fund】: 国家973项目(2006CB4035008);; 国家自然科学基金项目(40425006和40352003);; 中国科学院地球化学研究所百人计划项目资助
【CateGory Index】: P618.51
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