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《EARTH SCIENCE-JOURNAL OF CHINA UNIVERSITY OF GEOSCIENCES》 1999-03
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NATURE AND EVOLUTION OF LATE PALEOZOIC BASALTIC MAGMAS ALONG WESTERN MARGIN OF YANGTZE CRATON: GEOCHEMICAL STUDY OF REE AND TRACE ELEMENTS

Han Yinwen Chen Beiyue Liu Jianhua (Faculty of Earth Sciences, China University of Geosciences, Wuhan430074) Xu Jifeng (Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou510640)  
Emeishan basalt, Longmenshan diabase_prophyrite, and Mojiang diabase_prophyrite in the Late Permian-Early Triassic are important objects of the present paper. A correlation between the basalt in the Mianlüe ophiolite suite and that in the Sanjiang ophiolite suite can be used to suggest, on the bases of the chemical compositions of the rocks, the contents of the REE and trace elements, and the ratio of special elements in these rocks, that the Late Paleozoic basic magmatic activity in the western margin of Yangtze craton can be divided into three evolutionary stages: (1) basaltic magma in Yangtze continent was induced by the subduction of Tethyan oceanic crust; (2) the basaltic magma erupted on a large scale within the Yangtze craton with the subduction of Tethyan oceanic crust, and (3) the magmatic activity turned weaker and weaker until it was extinct within a limited region. The basaltic magma within the Yangtze craton mainly originated from the normal or concentrated mantle. During the initial and final evolutionary stages, part of magma originated from the depleted mantle. The Late Paleozoic basic magma activity in the western margin of the Yangtze craton must have been part of the tectonic changes of the global lithosphere and, therefore, must have been directly correlated with the subduction of Tethyan oceanic plate.
【Fund】: 国家自然科学基金
【CateGory Index】: P595,P595
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