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渤东凹陷北部烃源岩地球化学特征与油源对比
引用本文:郭喜浩,徐国盛,黄晓波,江涛,梁浩然,李长志,李智超.渤东凹陷北部烃源岩地球化学特征与油源对比[J].成都理工大学学报(自然科学版),2022,49(1):48-60.
作者姓名:郭喜浩  徐国盛  黄晓波  江涛  梁浩然  李长志  李智超
作者单位:油气藏地质及开发工程国家重点实验室(成都理工大学),成都610059,中海石油(中国)有限公司天津分公司,天津300459
摘    要:探讨渤海湾盆地渤东凹陷北部多套烃源岩的生烃潜力及其生烃贡献。通过烃源岩有机碳含量测试及岩石热解分析,结果显示东三段、沙一+沙二段、沙三段均发育优质烃源岩,3套烃源岩的干酪根均以Ⅱ1-Ⅱ2型为主,主要处于低成熟阶段。烃源岩GC-MS测试表明它们形成于不同的沉积环境,母质来源各异,表现出明显不同的生物标志物组合特征。东三段以较低伽马蜡烷/C30藿烷(<0.11)、较低ETR(<0.3)和较高C19TT/C23TT(>0.5)为特征,沉积于缺氧-低氧的淡水湖泊环境,具有较多的陆源有机质输入。沙河街组以较高伽马蜡烷/C30藿烷(>0.11)、较高ETR(>0.3)和较低C19TT/C23TT(<0.5)为特征,沉积在缺氧的弱咸化湖泊环境,陆源有机质输入较少。沙三段的沟鞭藻贡献较大,以高4-MSI(>0.17)和高TDSI(>0.35)为特征,与东三段、沙一+沙二段存在明显差异。基于生物标志物参数的主成分分析将原油划分为3类油族:油族A来源于沙三段烃源岩;油族B来源于东三段烃源岩;油族C主要来源于沙一+沙二段烃源岩,次为东三段烃源岩。

关 键 词:渤东凹陷  烃源岩评价  生物标志物组合特征  主成分  油源对比

Geochemical characteristics and oil-source correlation of source rocks in northern Bodong Sag,Bohai Bay,China
GUO Xihao,XU Guosheng,HUANG Xiaobo,JIANG Tao,LIANG Haoran,LI Changzhi,LI Zhichao.Geochemical characteristics and oil-source correlation of source rocks in northern Bodong Sag,Bohai Bay,China[J].Journal of Chengdu University of Technology: Sci & Technol Ed,2022,49(1):48-60.
Authors:GUO Xihao  XU Guosheng  HUANG Xiaobo  JIANG Tao  LIANG Haoran  LI Changzhi  LI Zhichao
Institution:(State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China;Tianjin Branch of CNOOC Ltd., Tianjin 300459, China)
Abstract:The hydrocarbon generation potential and contribution of multiple sets of source rocks in the northern Bodong Sag,Bohai Bay Basin are discussed by measurement of organic carbon content of source rocks and rock pyrolysis analysis.The results show that the third member of the Oligocene Dongying Formation(E3d3),the first to second(E2s1+2)and third(E2s3)members of the Eocene Shahejie Formation all develop high quality source rocks,and the kerogen of the three sets of source rocks is mainly typeⅡ1-Ⅱ2,which is mainly in low maturity stage.GC-MS analysis show that the source rocks were formed in different sedimentary environments and their parent materials came from different sources,showing obviously different biomarker combinations.The E3d3 is considered to be deposited in anoxic-hypoxic freshwater lakes with more terrigenous organic matter input,evidenced by lower gammacerane/C30 hopane(<0.11),lower ETR(<0.3)and higher C19TT/C23TT(>0.5),and the Shahejie Formation is thought to be deposited in anoxic alkaline-alkaline lakes with less input of terrigenous organic matter,evidenced by higher gammacerane/C30 hopane(>0.11),higher ETR(>0.3)and lower C19TT/C23TT(<0.5).The contribution of dinoflagellates in the E2s3 is higher than that in the E3d3 and the E2s1+2,which is characterized by high 4-MSI(>0.17)and TDSI(>0.35).Based on the principal component analysis of biomarker parameters,the crude oil in the study area can be divided into three oil groups:Oil group A comes from the source rock of E2s3;Oil group B comes from E3d3;and the main source of oil group C is E2s1+2,and the secondary source is E3d3.
Keywords:Bodong Sag  source rock evaluation  biomarker assemblages characteristics  principal components  oil-source correlation
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