中朝板块南缘下寒武统煤系炭质泥岩烃源岩评价
Evaluation of the Lower Cambrian coal series battie hydrocarbon source rocks in South of Sino-Korean plate
煤系炭质泥岩又称石煤，是大约5亿年前由藻类或菌类等低等生物在浅海环境下形成的腐泥类煤系岩层。新发现的中朝板块下寒武统煤系炭质泥岩烃源岩位于中朝板块南部，在豫皖两省交界处的雨台山、煤山及王八盖山一带最为发育，地理及行政区划上属于安徽省霍邱县马店镇。该套泥质烃源岩有机碳含量高，有机质类型好，热演化处于湿气—干气阶段。该套烃源岩的发现，对我国目前实施的油气勘探‘稳定东部’战略来说，有着重要的现实意义。
oal series battie was also called as stone coal，it is a kind of sapropelic coal that was formated by algae or fungi in the epeiric sea environment about 5 million years ago. The newly discovered lower Cambrian coal series battie hydrocarbon source rocks is in South of the Sino-Korean plate，and most Developed in the YUTAI hill、COAL hill and the WANGBAGAI hill in the Yu-wan junction，it belong to the Huoqiu town，Anhui provice on Geographical and administrative divisions.this hydrocarbon source rocks have high TOC，good type of organic matter，and it’s also in the combination gas-methane stage. The discovery of this source rocks have a important practical significance to the China\\\\\\\\\\\\\\\\\\\\\\\\\\\\\\\
贾立峰
石油天然气地质、石油天然气勘探
中朝板块煤系炭质泥岩烃源岩
Sino-Korean platecoal series battiehydrocarbon source rocks
贾立峰.中朝板块南缘下寒武统煤系炭质泥岩烃源岩评价[EB/OL].(2008-11-27)[2025-08-21].http://www.paper.edu.cn/releasepaper/content/200811-816.点此复制
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