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《GEOCHIMICA》 1997-02
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GEOCHRONOLOGY STUDIES OF CRUST-MANTLE INTERACTION AND MINERALIZATION IN THE HONGHE ORE DEPOSIT ZONE

Zou Ri Zhu Bingquan Sun Dazhong Chang Xiangyang (Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640)  
Based on geochronological and Nd model age data, it is indicated that the high metamorphic complexes of Ailaoshan and Yaoshan groups have a bulk age range of 1.35—1.7 Ga, and also there existed amphibolites of late Proterozoic. The light metamorphic zone between the Ailaoshan and Yaoshan groups were mainly composed of Precambrian volcanic rocks and marbles, as well as mingled with MORB of early Indo-Chinese period, which indicated that the initial division of strata proposed by The Yunnan Geological Survey, a suit of Triassic strata, was incorrect. The strong tectonic movements and dynamic metamorphism were occurred during Jinning(800 — 900Ma), Indo-Chinese (265 Ma), Yanshanian (75 — 115 Ma) and Himalayan (28 — 35 Ma) periods. The evidence from geochronology and geological observation shows that the rocks in this area are mainly tectonic rock fragments, instead of normal stratum series, which should be named as the Ailaoshan rock group. Copper mineralization was mainly occurred during Jinning period, and there were Cumigration, reactivation and enrichment during Indo-Chinese, Yanshanian and Himalayan periods.
【Fund】: 国家科学技术委员会攀登计划 中国有色金属工业总公司地质勘察局联合资助
【CateGory Index】: P597.3
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