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二连盆地宝勒根陶海凹陷烃源岩生物标志化合物特征与油源对比
引用本文:陈治军,王志伟,张少清,高怡文,韩长春,李科社.二连盆地宝勒根陶海凹陷烃源岩生物标志化合物特征与油源对比[J].沉积学报,2020,38(2):451-462.
作者姓名:陈治军  王志伟  张少清  高怡文  韩长春  李科社
作者单位:1.陕西延长石油(集团)有限责任公司研究院, 西安 710075
基金项目:自然资源部项目2017YQZYPJ01构造与油气资源教育部重点实验室开放研究基金项目TPR-2018-01
摘    要:二连盆地宝勒根陶海凹陷虽然取得了很好的勘探成果,但油气成藏基础研究还非常薄弱。依据生物标志化合物特征对烃源岩进行分类,在此基础上开展油族划分和油源对比研究。地球化学特征表明,研究区有效烃源岩可划分为三类:第一类烃源岩为腾格尔组一段(K1bt1)中上部“高有机质丰度、低成熟度、高C27甾烷相对含量、高伽马蜡烷含量、低Pr/Ph比值”烃源岩;第二类烃源岩为K1bt1下部“高有机质丰度、中等成熟度、中等C27甾烷相对含量、中等伽马蜡烷含量”烃源岩;第三类烃源岩为阿尔善组(K1ba)“较高有机质丰度、较高成熟度、低C27甾烷相对含量、低伽马蜡烷含量、高Pr/Ph比值”烃源岩。依据生物标志化合物特征,油砂中的原油可划分成4个油族:油族1为K1bt1未熟油,原油来源于第一类烃源岩;油族2为K1bt1成熟油,原油来源于第二类烃源岩;油族3为K1bt1未熟油与K1bt1成熟油的混合油,原油来源于第一类烃源岩和第二类烃源岩;油族4为K1bt1成熟油与K1ba成熟油的混合油,原油来源于第二类烃源岩和第三类烃源岩。从油气来源预测有利区,K1bt1烃源岩所指向的有利区的面积为26.85 km2,K1ba烃源岩所指向的有利区面积为79.30 km2。

关 键 词:烃源岩    生物标志化合物    油族划分    油源对比    宝勒根陶海凹陷    二连盆地
收稿时间:2019-02-01

Biomarker Characteristics of Source Rocks and Oil Source Correlation in Baolegentaohai Sag,Erlian Basin
Institution:1.Research Institute of Yanchang Petroleum(Group) Co. Ltd., Xi'an 710075, China2.Oil and Gas Exploration Company of Yanchang Petroleum(Group) Co. Ltd., Yan'an, Shaanxi 716000, China
Abstract:Although good exploration achievements have been made in Baolegentaohai Sag of Erlian Basin, the basic research on hydrocarbon accumulation is still very weak. In this study, source rocks are classified according to geochemical characteristics, and then oil group division and oil source correlation are carried out according to the characteristics of the biomarker compounds. The results show effective source rocks in the study area can be divided into three types: The first type, in the upper part of K1bt1, is characterized by high organic matter abundance, low maturity, high C27-sterane relative content, high gammacerane content, and low Pr/Ph. The second type, in the lower part of K1bt1, is characterized by high organic matter abundance, medium maturity, and medium gammacerane and C27-sterane relative content. The third type, in K1ba, is characterized by relative high organic matter abundance, high maturity, low C27-sterane content, low gammacerane content, and high Pr/Ph. Crude oil can be divided into four groups: Oil group 1 is K1bt1 immature oil, with hydrocarbons from the first type of source rock. Oil group 2 is K1bt1 mature oil, with hydrocarbons from the second type of source rock. Oil group 3 is a mixture of K1bt1 immature and K1bt1 mature oil, with hydrocarbons from the first and second types of source rocks. Oil group 4 is a mixture of K1bt1 mature and K1ba mature oil, with hydrocarbons from the second and third types of source rocks. In terms of the favorable exploration area prediction by oil and gas sources, the favorable area predicted by K1bt1 source rock is 26.85 km2, and the favorable area predicted by K1ba source rock is 79.30 km2.
Keywords:
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