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《Geological Survey and Research》 2012-04
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Geochemical characteristics of the Gouhou Formation Shales and Its Geological Significances

SUN Lin-hua(School of Earth Science and Engineering,Suzhou University,Suzhou,Anhui 234000,China)  
Gouhou Formation is important for the study of the tectonic evolution of southeast margin of North China Craton during the period between Pre-Cambrian and Cambrian.Based on the major,as well as trace element geochemical studies of the shales from Gouhou Formation,the following understanding have been obtained.Al2O3-Zr-TiO2 and Zr/Sc-Th/Sc diagrams show that the shales were first order sediments of igneous rocks without recycling,and then their geochemical compositions can be used for provenance evaluation.Diagrams of(SiO2/20)-(Na2O+K2O)-(MgO+TiO2+FeO*),TiO2-Ni,Th-Hf-Co and Hf-La/Th,as well as some ratios of elements(e.g.Co/Th,La/Sc and Zr/Sc),suggest that intermediate to felsic igneous rocks constitute the source rocks in the provenance.The CIA values(62) of them are low,which might have been affected by K-metasomatism,whereas the high CIW values(89) suggest that the source area have undergone intensive weathering.Major oxides,as well as trace elements suggest that their provenance was located in the area with active signature.
【Fund】: 安徽省高校优秀青年人才基金:皖北新元古代硅质灰岩成困研究(2010SQRL190)
【CateGory Index】: P588.21
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