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GEOLOGY,GEOCHEMISTRY AND GENESIS OF THE MESOZOIC SHOSHONITIC VOLCANIC ROCKS IN SHANDONG PROVINCE

Qiu Jiansheng Wang Dezi Zhou Jincheng Zen Jiahu (Department of Earth Sciences,Nanjing University,Nanjing 210093)  
The Mesozoic shoshonitic volcanic rocks in Shandong occurred mainly in the terrestrial fault basins along the Yishu deep fault zone and its both sides.These volcanic rocks were formed in the Early Cretaceous epoch (Rb-Sr isochron ages varying from 111.4-119.6 Ma)and constitute mainly trachybasalt-shoshonite-latite-trachyte association.Chemically,they are rich in alkali,especially potassium,and higher in Al 2O 3 and lower in TiO 2 as well as high Fe 2O 3/(Fe 2O 3+FeO) ratios.Moreover,they are notably enriched in highly incompatible lithophile elements,such as Rb,Th,Ba,LREE,etc.and have higher I sr values and quite low ε Nd values.The detailed analysis of their geological-geochemical characeeristics and rock-forming tectonic setting suggest that the formation of the Mesozoic shoshonitic volcanic rocks in Shandong should be originated mainly from the partial-melting of the enriched mantle.
【Fund】: 国家自然科学基金 地质矿产部壳幔体系组成、物质交换及动力学开放研究实验室研究基金
【CateGory Index】: P588.1
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