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《Journal of Chengdu University of Technology》 2002-05
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DYNAMICS OF THE REE MINERALIZATION IN MAONIUPING AREA, SICHUAN PROVINCE: ISOTOPIC GEOCHEMISTRY OF CARBONATITES

WANG Deng-hong 1, YANG Jian-min 1, YAN Sheng-hao 1, CHEN Yu-chuan 2, XU Jue 1 (1. Institue of Mineral Resources, Chinese Academy of Geological Sciences, Beijing; 2. Chinese Academy of Geological Sciences)  
Most of the REE deposits related to alkalic magmatic rocks (including carbonatite) formed in a rift environment. The REE deposit in Maoniuping is an exception. It formed during the Cenozoic orogeny process. The Maoniuping deposit is a large LREE deposit hosted within alkalic complex rocks, with most of the REE minerals distributed in carbonatites. The carbonatite has a well-distributed isotopic composition, 206Pb/ 204Pb=18.162~18.194, 207Pb/ 204Pb=15.536~15.567, 208Pb/ 204Pb=38.283~38.390, 87Sr/ 86Sr=0.70605~0.70691, 143Nd/ 144Nd= 0.512327~0.512436. Such a EMI-type isotopic composition suggests an enriched mantle source for the rare earth elements mineralization and a dynamic process involving mantle materials and tectonics. However, the Maoniuping area was situated at the Longmenshan-Jinpingshan Orogen during its Cenozoic compression process, and the alikalic igneous rocks and carbonatites were intruded at the same time. The underplating and upwelling of mantle materials from a EMI-type source region indicate that the movement of mantle materials and the transport of heat and fluids do have contributed a lot to the building of Longmenshan-Jinpingshan mountains and the formation of REE deposits. So, the plate-collision is not the merely solution to the enigma of the world roof. In fact, the Himalayan movement is the coupling of the crustal compression with the mantle materials and heat injecting up into the thickening crust.
【Fund】: 国家重点基础研究项目 ( G1 9990 4 32 0 3);; 中国地质大调查项目 ( K1 .4 -3-4 )
【CateGory Index】: P597
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