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《Journal of Xi'an Shiyou University(Natural Science Edition)》 2010-05
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Geochemical characteristics of the mid-acidity intrusive rocks in Nanhuashan and Xihuashan in the eastern segment of North Qilian Mountains,China

YAO Zhi-gang1,GAO Shan1,WANG Yong-dong2,SHE Gong1(1.College of Petroleum Resources,Xi'an Shiyou University,Xi'an 710065,Shaanxi,China;2.Yanchang Oilfield Limited Company,Yan'an 716000,Shaanxi,China)  
The mid-acidity intrusive rock in the studied area is mainly composed of granite and granodiorite,in which the mass fraction of SiO2 is 66.23% ~ 77.13%,and it is of the association characteristics and the geochemical characteristics of calc-alkaline rock series.In the intrusive rock,trace elements Pb,Sr,and La are enriched,while the elements Cs,Nb and Ti are lean in different degrees,which show the characteristics of mixed source magma.The total content of rare elements is 100.80~121.03 μg/g,which is lower than the world average value of acidic rocks.REE distribution pattern presents right dip type,δEu is in 0.31 ~ 0.33,and there is negative anomaly of Eu,which is similar to the geochemical characteristics of the island-arc granite from the northern Qinling in the Caledonian stage.In a whole,the mid-acidity intrusive rock is produced by the crystallization differentiation of mixed crust-mantle magmatic,which reflects the dive background of trench-arc-basin system in the northern Qilian area in the end of Middle Ordovician.
【Fund】: 陕西省自然科学基金项目(编号:SJ08D03);; 中国博士后科学基金项目(编号:20070420214)
【CateGory Index】: P588.12
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