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金岭寺—羊山盆地北票组烃源岩特征
引用本文:何保,李茂丰,刘颖鑫.金岭寺—羊山盆地北票组烃源岩特征[J].中国煤炭地质,2008,20(3):25-27.
作者姓名:何保  李茂丰  刘颖鑫
作者单位:何保(东北大学资源与土木工程学院,辽宁,沈阳,110004;辽宁工程技术大学资源与环境学院,辽宁,阜新,123000);李茂丰(辽宁工程技术大学资源与环境学院,辽宁,阜新,123000;吉林东煤地质局102地质队,吉林,梅河口,135000);刘颖鑫(吉林东煤地质局102地质队,吉林,梅河口,135000)
摘    要:通过对采集的岩样进行地球化学综合分析,得出金羊盆地北票组为盆地主要烃源岩,为盆地油气生成提供了物质基础;北票组烃源岩有机质丰度不高,属差一中等烃源岩;干酪根类型以腐殖型为主,成烃母质为陆地高等植物:金羊盆地北票组烃源岩已经进入成烃门限.并处于成熟阶段中的低成熟到中成熟阶段。

关 键 词:金羊盆地  北票组  烃源岩  有机质丰度  有机质类型  有机质成熟度
文章编号:1674-1803(2008)03-0025-03
修稿时间:2008年1月29日

Jinlingsi-Yangshan Basin Beipiao Formation Hydrocarbon Source Rock Characteristics
Institution:He Bao, Li Maofeng,Liu Yingxin (1 .College of Resource and Engineering, Northeastern University, Shenyang 110004; 2.College of Resource and Environment Engineering, Liaoning Technical University, Fuxin 123000; 3. No.102 Exploration Team, Northeastern China Bureau of Coal Geological Exploration, Meihekou, Jilin 135000)
Abstract:In order to evaluate the hydrocarbon source rock in Jinlingsi-Yangshan Basin, based on the geochemical comprehensive analyses of collected rock samples, conclusion are obtained that the Beipiao Formation is the main hydrocarbon source rock and provides the substance foundation for oil and gas formation. The organic abundance of Beipiao Formation hydrocarbon source rock is not very high and belongs to poor to middle grading. Kerogen type is mainly humic, and terrestrial higher plants are the petrologen. The Beipiao Formation hydrocarbon source rock has come into threshold of hydrocarbon forming and belongs to low-middle maturity stage.
Keywords:Jinlingsi-Yangshan Basin  Beipiao Formation  hydrocarbon source rock  organic matter abundance  organic matter type  organic matter maturity
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