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《Geochimica》 2011-01
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U-Pb ages,geochemistry and tectonic implications of mafic dyke swarms in Mugua,Chun'an county,Zhejiang Province

LI Fu-lin1,2,ZHOU Han-wen1,2,TANG Zeng-cai3,LI Yi-long1,WANG Fa-xiang3,XU Yu-chen4,QIN Hong-feng1,LUO Wei1 and GUAN Cheng-guo1 1.Faculty of Earth Science,China University of Geosciences,Wuhan 430074,China;2.State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan 430074,China;3.Zhejiang Institute of Geological Survey,Xiaoshan 311203,China;4.Institute of Geochemistry,Chinese Academy of Sciences,Guiyang 550002,China  
The mafic dyke swarms in Mugua-Chun'an area,Zhejiang Province mainly consist of diabase and diabase porphyrite with NW-SE trend.The rocks are mainly tholeiitic according to geochemical analyses.The REE distribution patterns show strong LREE-enrichment,with(La/Yb)N ratios of 5.1-7.6(mean=6.36),indicating a strong fractionation between LREE and HREE and possible residual garnet in the source region.The La/Sm vs.La diagram shows that the mafic dyke swarms in this region are mainly the production of equilibrium partial melting.The Eu anomaly is not obvious(δEu=0.95-1.03,with an average value of 0.99),reflecting that there was no prior plagioclase separation from the source region.Furthermore,the mafic dyke swarms are enriched in LILE(K,Rb,Cs,Ba,Sr) and HFSE(Nb,Ta,Zr,Hf,Ti) compared to mid-ocean ridge basalt.The positive relationship between the compatible elements(Cr,Ni,Co) and MgO indicates that the original magma has undergone fractional crystallization to a certain degree.The LA-ICPMS U-Pb dating of zircons from the mafic dyke swarms yielded a weighted mean age of(135±2) Ma,suggesting these rocks are the products of partial melting of mantle material caused by the lithospheric extension and decompression during the Early Cretaceous after the South China Indosinian intra-continental compressional deformation.This may reflect the southeast margin of the Yangtze Block was in the tectonic environment and geodynamic setting of intense break-up and lithospheric extensional thinning during the Early Cretaceous.
【Fund】: 浙江省国土资源厅项目(2007002);; 国土资源部公益性行业科研专项经费项目(200811015)
【CateGory Index】: P597.3
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