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论冀中地区O、C—P凝析气藏的形成条件
引用本文:杨远聪 李延钧 秦建忠 侯荣. 论冀中地区O、C—P凝析气藏的形成条件[J]. 西南石油大学学报(自然科学版), 1991, 13(2): 12-24. DOI: 10.3863/j.issn.1000-2634.1991.02.02
作者姓名:杨远聪 李延钧 秦建忠 侯荣
作者单位:(1.西南石油学院;2.华北石油局〕
摘    要:据凝析油轻烃组成、甲烷及其同系物碳同位素组成、天然气与源岩吸附气指纹时比、双环倍半萜组合特征及地质结构的综合分析,查明O、C—P大多数提析气藏的油气主要来源于石炭—二叠系煤系腐植型有机质,混入了部分下第三系的油气。对石炭—二叠系成烃特点的分析表明,R。=0.6%~1.3%,以成气为主,生油为辅,原始油气比一般大于1OOCm3/t。成熟期的石炭—二叠系有机质的成烃特点和具备油气富集的良好地质条件是O、C—P凝析气藏形成的基本条件。

关 键 词:凝析气藏  碳同位素  轻烃  冀中地区  
收稿时间:1990-03-01

FORMATION CONDITIONS OF O AND C-P CONDENSATE GAS RESERVOIRS IN JIZHONG AREA
Yang Yuan-cong Li Yan-jun Qin Jian-zhong Hou Rong. FORMATION CONDITIONS OF O AND C-P CONDENSATE GAS RESERVOIRS IN JIZHONG AREA[J]. Journal of Southwest Petroleum University(Seience & Technology Edition), 1991, 13(2): 12-24. DOI: 10.3863/j.issn.1000-2634.1991.02.02
Authors:Yang Yuan-cong Li Yan-jun Qin Jian-zhong Hou Rong
Affiliation:(South-west Petroleum Institute;2.North China Petroleum Administration)
Abstract:According to the comprehensive analysis of light hydrocarbon composition of condensates, carbon isotopic composition of methane and its homologues,fingerprint correlation of natural gases with absorbed gases of source rocks, assemblage features of double-cycle serquiterpenes and geologic framework, this paper demonstrates that oil and gas in most O and C-P condensate gas reservoirs mainly come from humic organic matter of C-P coal seams and are mixed with a portion of oil and gas from Paleogene. The authors analyze the characteristics of hydrocarbon generation in C-P, and suggest that gas generation is main,oil generation is subordinate,and original gas-oil ratio is more than 100Cm3/t in general within vitrinite reflectance values of 0.6% —1.3%,The basic formation conditions of O and C-P condensate gas reservoirs are both the characteristics of hydrocarbon generation in C-P coal organic matter during mature stage anp the favorable geologic conditions for oil and gas accumulation.
Keywords:Condensate gas reservoir  Carbon isotope  Light hydrocarbon  Jizhong Area O: Ordovician  C: Carboniferous  P: Permian  N:Paleogence  
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