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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2010-06
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Analysis of ore-bearing potential in the boundary line of Sinian-Cambrian System in the Nanjiang area of Northeast Sichuan,China

PANG Yan-chun1,LIN Li1,MA Ye-qing2,HUANG Yong-huang31.Institute of Sedimentary Geology,Chengdu University of Technology,Chengdu 610059,China;2.Gansu Industrial Vocational and Technical College,Tianshui 741025,China;3.The 404 Geological Team,Sichuan Development Bureau of the Geology and Mineral Resources Exploration,Xichang 615000,China  
A series of black shales appear at the bottom of Cambrian (Majialiang shale) in the Nanjiang area,Northeast Sichuan.The feature of the black shales is similar to that of Niutitang Formation of West Hunan and North Guizhou.They consist of the black carbonaceous shale and siltstone and are rich in laminar pyrite and pyrite concretion.The underlying stratum is Member 3 of Dengying Formation which is composed of microlite-dolomite with black-gray color.The surface of the dolomite has oil seepages evidently.The ore-bearing potential,the lithologic characters and geochemistry are discussed.The quantitative analysis of the metallic elements indicates that in the area there is also the enrichment phenomenon of the nickel-molybdenum-vanadium,especially vanadium,at the bottom of Cambrian.The analysis of lithologic characters and organic carbon content indicates that the features of source rocks come from the third member of Dengying Formation to Majialiang shale.Compared with previous data,it can be summarized that in the area,there are metal-rich mineral layers at the bottom of the Cambrian and oil-generating potential from the third member of Dengying Formation to Majialiang shale.In addition,the metal enrichment and organic carbon content show a positive correlation.This indicates that the metal enrichment is relative to oil migration
【Fund】: 国家自然科学基金资助项目(40743016);; 教育部“高等学校博士学科点专项科研基金”项目(20070616014);; 中国石油化工股份有限公司项目(G0800-06-25-319)
【CateGory Index】: P617
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