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《Journal of East China Institute of Technology(Natural Science)》 2011-04
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Geochemical Characteristics and Genesis of Niudai Diabase Dykes in Northern Guangdong Province

CAO Hao-jie1,HUANG Le-zhen1,SHEN Wei-zhou2,LING Hong-fei2,HUANG Guo-long1,DENG Ping3,ZHU Ba1 (1.Research Institute No.290,CNNC,Shaoguan,GD 512026,China;2.School of Earth Sciences and Engineering,Nanjing University,Nanjing,JS 210093,China;3.Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China)  
The Niudai diabase dykes,located in the south of Zhuguang pluton of North Guangdong Province,are characterized with low SiO2(45.04%~48.64%),high TiO2 (2.02%~3.23%) and TFeO (17.00%~19.80%),enrichment in LILE (Rb,Ba) and LREE,relatively high ΣREE(112.1×10-6~132.7×10-6),slightly depletion in Nb and Ta,without negative Eu anomaly.All informations are similar to the basalt from asthenospheric mantle sources.Elements' ratios of incompatible elements,such as Zr/Ba,La/Nb,La/Ta,Ti/Y,Ba/Nb,Th/Nb and Th/La of Niudai diabase are close to the ratios of OIB.The tectonic discrimination diagrams show that the diabases all fall into the range of OIB.The Niudai diabases have Pb isotope (206Pb/204Pb=18.153~18.594,207Pb/204Pb=15.713~15.730,208Pb/204Pb=39.184~39.206) and its εNd(t) ranges from 3.1 to 4.3,close to the scope of OIB.The geochemical characteristics indicate that the origin of Niudai Diabase had both ends of members of mixed characteristics of asthenospher mantle and lithosphere mantle,and the hybrid were related to the melts of overlying lithosphere mantle as asthenospher mantle upwelling.The Niudai diabases are formed while the fast invaded of magma in the tectonic environment that lithospher thinning leaded by asthenosphere mantle upwelling.
【Fund】: 内生金属矿床成矿机制研究国家重点实验室研究项目(2008-I-04);; 教育部科学研究重大项目(306007)
【CateGory Index】: P588.125
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