收稿日期: 2003-10-15
修回日期: 2003-11-17
网络出版日期: 2004-02-20
SEDIMENTARY FACIES OF THE FORTH SUB-MEMBER OF THE SHANSHAN FORMATION AT SHANLE OIL AND GAS FIELD IN TUHA BASIN
Received date: 2003-10-15
Revised date: 2003-11-17
Online published: 2004-02-20
古莉,于兴河,万玉金,杜秀芳,帅勇乾,闫伟鹏 . 冲积扇相储层沉积微相分析――以吐哈盆地鄯勒油气田第三系气藏为例[J]. 天然气地球科学, 2004 , 15(1) : 82 -86 . DOI: 10.11764/j.issn.1672-1926.2004.01.82
By using the geological, log and seismic data,the type s of the micro-facies of the Shanshan formation in Shale oil and gas field in T uha basin were studied, and the distribution of the micro-facies of the forth s ub-member was analyzed. The results show that the Shanshan formation belongs to the middle fan of alluvial fan deposits, which can be further divided into 4 su b-faciese, including braided channel, overbank deposits, debris flow and braide d bar. The former two are the main sub-faciese. The analysis of the well testin g data shows that natural gas is mainly dispersed in the micro-facies of braide d channel, secondly in overbank deposits and in braided bars. In the background of being shallow-burried and in relatively young strata, the gas accumulation f avorably occurs in the sand bodies of the braided channel micro-facies.
[1 ] 冯增昭.沉积岩石学 [M ].北京:石油工业出版社,1993.
[2 ] 于兴河碎屑岩系油气储层沉积学 [M ].北京:石油工业出版社,2002.
[3 ] 王志坤,王多云,郑希民,等.陕甘宁盆地陇东地区三叠系延长统长6-长8储层沉积 特征及物性分析 [J ].天然气地球科学,2003,14(5):380-385.
[4 ] 郑浚茂.陆源碎屑沉积环境的粒度标志 [D ].北京:武汉地质学院北京研究生部, 1982.
[5 ] 邓宏文.高分辨率层序地层学——原理及应用 [M ].北京:地质出版社,2002.
[6 ] Reading H G. Sedimentary Environments: Processes, Facies and Stratigraphy 3d [M ]. Blackwell:Scientific Publication, 1996.
/
| 〈 |
|
〉 |