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辽宁秀水盆地白垩系义县组烃源岩地球化学特征 ——以辽法D1井为例
引用本文:李文博,李晓海,丁秋红,张健,何大祥.辽宁秀水盆地白垩系义县组烃源岩地球化学特征 ——以辽法D1井为例[J].地质与资源,2019,28(4):358-363.
作者姓名:李文博  李晓海  丁秋红  张健  何大祥
作者单位:中国地质调查局沈阳地质调查中心,辽宁沈阳,110034;长江大学,湖北武汉,430000
基金项目:中国地质调查局"松辽盆地外围西部盆地油气基础地质调查"项目(编号DD20160163).
摘    要:对辽宁北部秀水盆地辽法D1井白垩系义县组上部烃源岩的有机质丰度、类型与成熟度及烃源岩厚度等特征分析表明,义县组湖相泥岩在盆地内分布广泛,厚度较大,为秀水盆地的主力烃源岩.义县组烃源岩TOC在1.37%~8.61%之间,平均值为3.70%,为中等-好的烃源岩,有机质类型为Ⅱ1-Ⅱ2型,Ro值较高,分布范围1.08~1.20,指示热演化达到成熟-生油高峰阶段,具有较好的资源潜力.

关 键 词:烃源岩  地球化学  义县组  秀水盆地  辽法D1井  辽宁省
收稿时间:2018-05-07

GEOCHEMISTRY OF THE HYDROCARBON SOURCE ROCKS FROM CRETACEOUS YIXIAN FORMATION IN XIUSHUI BASIN: A Case Study of LF-D1 Well
LI Wen-bo,LI Xiao-hai,DING Qiu-hong,ZHANG Jian,HE Da-xiang.GEOCHEMISTRY OF THE HYDROCARBON SOURCE ROCKS FROM CRETACEOUS YIXIAN FORMATION IN XIUSHUI BASIN: A Case Study of LF-D1 Well[J].Geology and Resources,2019,28(4):358-363.
Authors:LI Wen-bo  LI Xiao-hai  DING Qiu-hong  ZHANG Jian  HE Da-xiang
Institution:1. Shenyang Center of Geological Survey, CGS, Shenyang 110034, China;2. Yangtze University, Wuhan 430000, China
Abstract:The analysis on the organic matter abundance, type, maturity and thickness of the upper source rocks in Cretaceous Yixian Formation of LF-D1 well in Xiushui Basin, northern Liaoning Province, shows that the lacustrine mudstones serve as the main source rocks with wide distribution and large thickness. The TOC of source rocks is 1.37%-8.61%, averagely 3.70%, belonging to medium-good grade. The organic matter types are mainly II1-II2, with high Ro ranging from 1.08 to 1.20, which indicates the thermal evolution reaches mature to oil-generating peak stage with good resources potential.
Keywords:source rock  geochemistry  Yixian Formation  Xiushui Basin  LF-D1 well  Liaoning Province  
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