收稿日期: 2010-12-16
修回日期: 2011-01-29
网络出版日期: 2011-08-10
基金资助
国家重大专项(编号:2008ZX05002-006)资助.
Later Hydrocarbon Generation Potential of Upper Paleozoic Source Rock in Southern North China
Received date: 2010-12-16
Revised date: 2011-01-29
Online published: 2011-08-10
陈新军, 胡宗全, 李淑筠 . 华北南部地区上古生界晚期生烃潜力研究[J]. 天然气地球科学, 2011 , 22(4) : 610 -617 . DOI: 10.11764/j.issn.1672-1926.2011.04.610
The upper Paleozoic source rocks include dark mudstone in coal measures,coal,and carbonaceous mudstone in the southern north China.In the primary sedimentary settings,the thickness of Carboniferous and Permian source rocks in the southern north China is larger than that in the north Bohai Bay basin.The upper Paleozoic source rock went through three times of hydrocarbon generation: early Indosinian,Yanshanian,and late Himalayan.In some places (i.e Kaifeng sag,Luoyang\|Yichuan,Hefei basin,Qiuxian-Guanxian sag,Huangkou sag,Tangzhuang\|Shenqiu sag),the hydrocarbon source rock reached the highest thermal maturity and the maximum hydrocarbon generation at the Yanshan Period and ceased the hydrocarbon generation at the Himalayan Period.In the Bohai Bay basin,the late hydrocarbon generation potential of source rocks in the areas of HuiMing,DongPu,DongYing,ZhanHua is large,but general in the areas of Chezheng,north Xinxian sag,Luyi,and Niqiuji.
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