THE SOURCE ROCKS OF HONGSHUIZHUANG FORMATION IN LINGYUAN AREA OF LIAOXI DEPRESSION: Petroleum Geology and Hydrocarbon Generation Potential
ZONG Wen-ming1, SUN Qiu-shi1, GAO Xiao-yong1, ZHENG Lei2, SHI Lei1, LI Yong-fei1, SUN Shou-liang1, ZHANG Tao1
1. Shenyang Center of China Geological Survey, Shenyang 110034, China; 2. Key Laboratory of Exploration Technology for Oil and Gas Resources/Yangtze University, Wuhan 430100, China
Abstract:The shale of Hongshuizhuang Formation is the dominant source rock of Yanliao rift belt with good hydrocarbon generation potential. However, the study of Hongshuizhuang Formation in Liaoxi Depression is relatively weak, which restricts the study of Meso-Neoproterozoic oil-gas geological conditions and exploration in this area. To reveal the hydrocarbon generation potential and oil-gas preservation conditions of source rocks in the area, geochemical analysis is carried out for samples from LLD2 well and 3 sections in Lingyuan area. The results show that the source rocks of Mesoproterozoic Hongshuizhuang Formation generally have high organic abundance and good hydrocarbon-generating material basis. The organic matter is mainly Ⅰ-Ⅱ1 type, partly Ⅱ2 and Ⅲ types. The Ro distribution ranges from 1.15% to 2.26%, belonging to mature-high mature stage, and some samples are over-mature, which are comprehensively evaluated as medium-good source rocks with good hydrocarbon generation potential. The Hongshuizhuang Formation in Lingyuan area serves as source bed located in favorable reservoir facies belt and can compose two sets of complete source-reservoir-cap assemblages, showing good oil-gas exploration prospects.
宗文明, 孙求实, 郜晓勇, 郑磊, 石蕾, 李永飞, 孙守亮, 张涛. 辽西拗陷凌源地区洪水庄组烃源岩石油地质特征及生烃潜力[J]. 地质与资源, 2022, 31(2): 165-174,196.
ZONG Wen-ming, SUN Qiu-shi, GAO Xiao-yong, ZHENG Lei, SHI Lei, LI Yong-fei, SUN Shou-liang, ZHANG Tao. THE SOURCE ROCKS OF HONGSHUIZHUANG FORMATION IN LINGYUAN AREA OF LIAOXI DEPRESSION: Petroleum Geology and Hydrocarbon Generation Potential. GEOLOGY AND RESOURCES, 2022, 31(2): 165-174,196.
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