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《Geochimica》 1998-01
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ELEMENT GEOCHEMISTRY OF SHOSHONITIC LAMPROPHYRES IN THE PENGJIAKUANG GOLD DISTRICT,SHANDONG PROVINCE, CHINA

Cheng Xiaojiu; Cheng Jingping; Wang Jianghai(Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640)  
The shoshontic lamprophyres in the Pengjiakuang gold district are characterized by high alkaline, high K_2O / Na_2O ratios, low TiO_2, high and variable Al_2O_3, a strong enrichment in LILE and LREE, and distinct depletion in comparable element (Cr, Co and Ni). These geochemical characteristics clearly indicate that they were derived from the batch partial melting of the enriched mange and fractional crystallization of olivine and clinopyroxene. Based on the geochemical discrimination diagrams proposed by Muller (1993), the shoshonitic lamprophyres were formed in the continental are setting,and could be related to the subduction of Izanaqi oceanic plate beneath the continent of East China in the Yanshanian Period.
【Fund】: 国家和广东省博士后科学基金
【CateGory Index】: P595
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