FORMATION AND DISTRIBUTION OF THE PALEOZOIC MARINE CARBONATE-ROCK POOLS IN CHINA
-
摘要: 中国古生界多套海相烃源岩的叠合分布和中—新生界陆相地层的进一步覆盖,导致古生界油气藏的形成具有多源、多期性,烃源岩主要分布在克拉通盆地和克拉通内裂谷盆地。碳酸盐岩是主要的储集层,泥质岩是主要的区域和局部盖层。构造—热事件作用使得除塔里木盆地以外的盆地烃类相态以干气为主,包括干酪根裂解气和原油裂解气。根据储集层特征,将碳酸盐岩油气藏划分为4类:碳酸盐岩滩油气藏、不整合岩溶油气藏、生物礁油气藏和成岩油气藏。其中碳酸盐岩岩溶油气藏和高能环境下发育的滩相油气藏是最为重要的油气藏类型。断裂、不整合和古隆起控制着油气的空间分布,油气具有跨时代分布的特点。Abstract: The superimposing distribution of many sets of the Paleozoic marine source rocks and the further overlying of the Meso-Cenozoic continental strata resulted in the multi-source and multi-stage formation of the Paleozoic oil and gas pools in China.Hydrocarbon source rocks are distributed in craton basins and in-tracratonic rift basins.Carbonate rocks are major reservoirs, and argillaceous rocks are major local and regional caprocks.The hydrocarbon phases of the basins except for the Tarim Basin are dominated by dry gases including pyrolysis gases from kerogen and crude oil because of tectonic-thermal events.According to the characteristics of reservoirs, carbonate rock pools were divided into four types, that is, carbonate rocky-beach pools, uncomformity-karst pools, biohermal pools and diagenetic pools.Among them, carbonate rocky-karst pools and the beach-phase pools developed in high-energy environments are the most important types of oil and gas pools.Faults, unconformities and paleouplifts control the spatial distribution of oil and gas, and the distribution of oil and gas is diachronous.
-
Key words:
- oil and gas pool /
- carbonate rock /
- marine /
- Paleozoic /
- China
-
[1] 胡见义.海相石油地质综述[J].海相石油地质,1996,2(1):1-5. [2] 周荔青,张淮. 中国海相残留盆地油气成藏系统特征[J]. 石油实验地质,2002,24(6):483-489. [3] 梁狄刚.从塔里木盆地看中国海相地层生油问题(摘要)[J].海相油气地质,2000,5(1-2):83. [4] Zhang S C,Hanson A D,Moldowan J M,et al.Paleozoic oil-source rock correlations in the Tarim Basin,NW China [J].Organic Geochemistry,2000,31:273-286. [5] 赵孟军,张水昌,曾强,等.塔里木盆地石炭系碳酸盐岩烃源岩及其原油特征[J].海相油气地质,2000,5(1-2):23-28. [6] 翟光明.中国石油地质志(卷十)——四川油气区[M].北京:石油工业出版社,1989.224-265. [7] 程克明,王兆云,钟宁宁,等.碳酸盐岩油气生成理论与实践[M].北京: 石油工业出版社,1996:276-308. [8] 窦立荣,徐树宝.油气藏保存条件研究[J]. 大庆石油地质与开发,1992,11(3):6-10. [9] Downey M W.Evaluating seals for hydrocarbon accumulations[J].AAPG,1984,68:1752-1763. [10] 游秀玲.天然气盖层评价方法[J].石油与天然气地质,1991,12(3):261-275. [11] 顾家裕.塔里木盆地沉积层序特征及其演化[M].北京:石油工业出版社,1996:305-359. [12] Zhao M W,H J Behr,H Ahrendt,et al.Thermal and tectonic history of the Ordos Basins,China: Evidence from apatite fission track analysis,vitrinite reflectance,and K-Ar dating [J].AAPG,1996,80(7):1110-1134. [13] 夏新宇.碳酸盐岩生烃与长庆气田气源[M].北京:石油工业出版社,2000. 60-98. [14] Carmalt S W,St John B.Giant oil and gas fields [A].Halbouty M T. Future Petroleum Province Of the World [C].AAPG Memoir 40,1986:11-53. [15] 吕修祥,金之钧.碳酸盐岩油气田分布规律[J].石油学报,2000,21(3):8-12. [16] 戴金星,裴锡古,戚厚发.中国天然气地质学[M].北京:石油工业出版社,1992. 100-180.
计量
- 文章访问数: 843
- HTML全文浏览量: 71
- PDF下载量: 384
- 被引次数: 0