Sequence stratigraphic division and evolution of Carboniferous in Tarim Basin
-
摘要: 运用层序地层研究的理论及方法,针对塔里木盆地石炭系东河砂岩开展层序地层研究,探讨在塔里木盆地利用露头—钻井—地震资料为基础的综合层序地层解释方法技术,识别层序边界,建立地层格架。通过野外露头观察、钻井资料分析及地震剖面综合解释方法技术,在石炭系识别出了6个层序。重点对觉马—赛克区东河砂岩段层序进行分析,认为该段是一个穿时岩性地层单元,跨3个层序,即C-SQ1,C-SQ2,C-SQ3,其主体相当各层序的低位—海进域(TST),为一套海岸上超砂岩沉积,是今后的重点勘探目标。Abstract: Sequence stratigraphic studies have been carried out in the Carboniferous Donghe sandstones in the Tarim Basin based on the theories and methodologies of sequence stratigraphy.An integrated technique for sequence stratigraphic interpretation has been discussed by means of outcrop,drilling and seismic data.The technique can be used to identify sequence boundaries and establish stratigraphic frameworks.Through field outcrop observation,drilling data analyses and seismic profile interpretation,we have identified 6 sequences in the Carboniferous.The Donghe sandstone sequence in Juema-Saike region is a diachronous lithostratigraphic unit including 3 sequences:C-SQ1,C-SQ2 and C-SQ3.The main part of the sequence is equivalent to TST.The sandstones consist of coastal onlap deposits and are the key targets for future explorations.
-
Key words:
- Carboniferous /
- Donghe sandstone /
- sequence identification /
- Tarim Basin
-
[1] 吴因业,李熙喆,施和生,等,层序地层学在非构造圈闭勘探中的应用论文集[C].北京:石油工业出版社,2008. [2] 顾家裕,朱筱敏,王贵文,等.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. [3] 威尔格斯C K.层序地层学原理(海平面变化综合分析)[M].徐怀大,魏魁生,洪卫东,等译.北京:石油工业出版社,1992. [4] Van Wagoner J C,Posamentier H W,Mitchum P R,et al.An overview of the fundamentals of sequence stratigraphy and key definitions[J]. SEPM special publication,1988(42):39-45. [5] 李兴平,许国明,李静琏,等.新疆塔里木盆地层序地层格架[J].石油实验地质,1996,18(2):134-145. [6] 王君奇,武涛.塔里木盆地石炭系沉积特征及石油地质意义[J].石油实验地质,1999,21(1):25-29. [7] 蒋小琼,郭建华,管宏林,等.塔里木盆地满西地区石炭系层序地层与沉积体系分析[J].石油实验地质,2004,26(4):333-337. [8] 朱怀诚,罗辉,王启飞,等.论塔里木盆地"东河砂岩"的地质时代[J].地层学杂志,2002,26(3):197-201. [9] 张光亚.塔里木古生代克拉通盆地形成演化与油气[M].北京:地质出版社,2000. -
点击查看大图
计量
- 文章访问数: 3112
- HTML全文浏览量: 52
- PDF下载量: 1018
- 被引次数: 0
下载:
苏公网安备32021102000780号