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《Journal of Changchun University of Science and Technology》 2001-01
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MANTLE SOURCE AND TECTONIC SETTINGS FOR THE VOLCANIC ROCKS FROM DANZHOU GROUP IN LONGSHENG AREA, NORTHERN GUANGXI

GE Wen_chun 1,LI Xian_hua 1,LI Zheng_xiang 2,ZHOU Han_wen 3 (1.Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640,China;2.Department of Geology and Geophysics, University of Western Australia, Nedlands WA6009, Austra  
Danzhou group in Longsheng area formed at late Proterozoic era (820～760 Ma), and its Hetong formation is composed of spilite and rhyolite which constitute the bimodal rock association. The source magma of spilite deserved from enriched lower lithospheric mantle which had ever been metasomatized by fluid from subducted slab. Rhyolite and spilite are the products of cogenetic magma through the process of crystallization and differentiation. Bimodal volcanic rocks formed at an extensional setting of continental lithospheric thinning, and related to the activities of mantle plume, which led to the breakup of late Proterozoic Rodinia supercontinent.
【Fund】： 国家杰出青年科学研究基金! ( 4972 5 30 9);; 中国科学院资源与生态环境重大项目!B(KZ95 1-B1- 413)资助
【CateGory Index】： P588.1
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