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中国大中型油气田的主力烃源岩分布特征
引用本文:刘洛夫,金之钧. 中国大中型油气田的主力烃源岩分布特征[J]. 石油学报, 2002, 23(5): 7-13. DOI: 10.7623/syxb200205002
作者姓名:刘洛夫  金之钧
作者单位:石油大学石油天然气成藏机理教育部重点实验室 北京 102249
基金项目:中国石油天然气集团公司“九五”重大科技项目“大、中型油气田成藏定量模式研究”( 96 0 0 0 7)的部分成果
摘    要:中国大中型油气田主力烃源岩的分布在时代、盆地类型、岩性和沉积环境方面都具有多样性。在地质时代上 ,从中元古代到新生代 (泥盆系除外 )均有烃源岩分布 ,最重要的是在中、新生代。在盆地类型上 ,有中、新生代的裂谷盆地、古生代早期的克拉通盆地和晚期的前陆盆地、以及中生代的前陆盆地。不同类型盆地的烃源岩的分布、地质地化特征和生烃潜力差别较大。源岩类型有海相碳酸盐岩、泥岩以及海陆过渡相和陆相泥岩、煤系及碳酸盐岩 ,其中以湖相碎屑岩为主。

关 键 词:中国   大中型油气田  烃源岩   分布  地质时代  盆地类型   岩性  沉积环境  
文章编号:0253-2697(2002)05-0006-08
收稿时间:2001-09-05
修稿时间:2002-2-20 

Distribution of major hydrocarbon source rocks in China's large and medium-sized oil and gas fields
LIU Luo fu JIN Zhijun. Distribution of major hydrocarbon source rocks in China's large and medium-sized oil and gas fields[J]. Acta Petrolei Sinica, 2002, 23(5): 7-13. DOI: 10.7623/syxb200205002
Authors:LIU Luo fu JIN Zhijun
Affiliation:Key Laboratory for Hydrocarbon Accumulation Mechanism in University of Petroleum , Ministry of Education , Beijing 102249 , China
Abstract:Distribution of major source rocks in China's large and medium_sized oil_gas fields is of diversifcation and complexity in geologic age,basin types,lithology and sedimentary environment.These source rocks developed with strata from Middle Proterozoic to Cenozoic(excluding Devonian),among which the Mesozoic and Cenozoic layers are the most important.The basins that developed source rocks include the rift basin of Mesozoic_Cenozoic,the cratonic basin of early Paleozoic,and the foreland basin of Mesozoic and Late Paleozoic.There are quite large differences in distribution,geological and geochemical characteristics and hydrocarbon generation potential of source rocks between different types of basins.The source rocks include the marine carbonate and mudstone,and the transitional and terrestrial mudstone,coal measure strata and carbonate.The major one is lacustrine clastic rock.
Keywords:China  large and medium_sized of oil_gas field  hydrocarbon source rock  distribution  basin type  rock lithology  sedimentary environment  
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