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《Acta Geologica Sinica》 2011-05
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Geochronology and Geochemical Characteristics of the Shujiaidian Intrusion in Tongling, China

WANG Shiwei,ZHOU Taofa,YUAN Feng,FAN Yu,L YuzhuoSchool of Resources and Environmental Engineering,Hefei University of Technology,Hefei,230009  
The Shujiadian intrusion is located in the transition part between the Tongling faulting uplift and the Fanchang faulting basin in the Middle-Lower reaches of the Yangtze River.The rock types of this intrusion include pyroxene diorite,quartz diorite porphyrite,granodiorite porphyry,diorite and diorite porphyrite.This paper studied LA-ICPMS U-Pb dating data of the zircons from pyroxene diorite,and its geochemical compositions and Pb isotope,so as to probe the geochronology,source and evolution of magmas,and tectonic setting of the Shujiadian intrusion.The results indicate that the age of the Shujiadian intrusion is 139.2±2.1Ma(MSWD=2.3,n=12),suggesting that it is part of the magmatic system in the Tongling area,but not the Fanchang volcanic basin.Pyroxene diorite belongs to high potassium series.And the Shujiadian intrusion might derive from the metasomatic enriched mantle (EMΠ).There existed crystal fractionation of minerals such as apatite,amphibole,pyroxene and plagioclase,which also affected by the assimlation of crust materials during the evolution of the magmas.The intrusion formed in a compressional regime.
【Fund】: 国家自然科学基金项目(编号40830426);; 中国地质调查局地质调查工作项目(编号1212011121115);; 安徽省地质公益性地质项目(编号2009-g-22);; 新世纪优秀人才支持计划项目(编号NCET-10-0324)资助的成果
【CateGory Index】: P597.3
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