Geochemical Characteristics and Sedimentary Control of Pinghu Formation(Eocene)Coal-bearing Source Rocks in Xihu Depression,East China Sea Basin  

作　　者：SHEN Yulin QIN Yong CUI Min XIE Guoliang GUO Yinghai QU Zhenghui YANG Tianyang YANG Liu 

机构地区：[1]Key Laboratory of Coalbed Methane and Reservoir Formation Process,Ministry of Education,Xuzhou,Jiangsu 221008,China [2]School of Resources and Geoscience,China University of Mining and Technology,Xuzhou,Jiangsu 221116,China [3]CNOOC Research Institute Co.,Ltd.,Beijing 100028,China [4]College of Energy,Chengdu University of Technology,Chengdu 610059,China [5]Jiangsu Vocational Institute of Architectural Technology,Xuzhou,Jiangsu 221018,China

出　　处：《Acta Geologica Sinica(English Edition)》2021年第1期91-104,共14页地质学报（英文版）

基　　金：Financial support for this work was provided by the National Key Research Program for Science and Technology of China(No.2011ZX05023-001-008);the Priority Academic Program Development of the Jiangsu Higher Education Institutions(PAPD)。

摘　　要：Coal-bearing source rocks of the Pinghu Formation in the Xihu Depression comprise an important material basis of oil and gas resources in the East China Sea Basin.Based on drilling core observation results combined with the analysis and test results of macerals,trace/rare earth elements,and rock pyrolysis,the geochemical characteristics and sedimentary control of coal-bearing source rocks formation are discussed in a high-frequency sequence framework.The results indicate that the macerals composition of the coal-bearing source rocks of the Eocene Pinghu Formation in the Xihu Depression is dominated by vitrinite,with low-medium abundance of exinite and almost no inertinite.The coals and carbonaceous mudstones display higher amounts of total organic carbon(TOC)(14.90%-65.10%),S1+S2(39.24-136.52 mg/g),and IH(191-310 HC/g TOC)respectively,as compared to the mudstones.Organic matter is plotted in typeⅢkerogens and partially in typeⅡ;it is mainly in the low maturity stage.The trace elements results imply that the samples were deposited in a weakly reducing to weakly oxidizing environment and were occasionally affected by seawater.The coal-bearing source rocks were deposited in a relatively oxygen-containing environment.The coal-bearing source rocks development is jointly controlled by the coal accumulation environment,the water conditions affected by ocean currents in offshore basins in China,oxidation-reduction cycles of aqueous media and paleoclimate evolution in a high-frequency sequence framework.

关 键 词：geochemical characteristics coal-bearing source rock high-frequency sequence Pinghu Formation Xihu Depression 

分 类 号：P618.13[天文地球—矿床学]