|Table of Contents|

Sequence Stratigraphy and Sedimentary Faces in the Third Member of Shahejie Formation of Huanxiling Area in the West Depression, Liaohe Basin(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2010年第03期
Page:
245-
Research Field:
基础地质与矿产地质
Publishing date:

Info

Title:
Sequence Stratigraphy and Sedimentary Faces in the Third Member of Shahejie Formation of Huanxiling Area in the West Depression, Liaohe Basin
Author(s):
DONG Jie;  CHEN Shi-yue;  LI Cong
(School of Geo-resources and Information, China University of Petroleum, Dongying 257061, Shandong, China)
Keywords:
sedimentary facies;  sublacustrine fan;  fan delta;  the third member of Shahejie Formation;  Huanxiling Area;  Liaohe Basin
PACS:
TE121.3;P539.2
DOI:
-
Abstract:
With the high resolution sequence stratigraphy and the correlation analysis of cores, logs and seismic data, different orders of stratigraphic sequence interface were identified for the third member of Shahejie Formation of Huanxiling Area in the west depression of Liaohe Basin, the stratigraphic framework was built, the types of sedimentary facies, evolution and distribution of the framework were discussed, and the distribution of favorable sedimentary reservoir was forecasted. The results showed that the recognition marks of stratigraphic sequence interface were the significant changes of lithology, color, type of sedimentary facies and electricity character; Shahejie Formation of Huanxiling Area was divided into 6 three-order strata sequences and 12 four-order strata sequences; fan dalta, sublacustrine fan and lacustrine facies were developed in the third member of Shahejie Formation, fan dalta was developed in the upper subsection, sublacustrine fan was widely developed in the middle subsection, deep, littoral and shallow lacustrine facies was mainly developed in the lower subsection; reservoir physical properties of sublacustrine fan in the middle subsection of the third member of Shahejie Formation and fan dalta in the lower subsection were best, and it was the favorable sedimentary reservoir.

References:

[1] Cross T A.Quantitative Dynamic Stratigraphy[M].New Jersey:Prenrice Hall,1990.
[2] Cross T A.Stratigraphic Controls on Reservoir Attributes in Continental Strata [J].Earth Science Frontiers,2000,7(4):322-350.
[3] 邓宏文.美国层序地层研究中的新学派——高分辨率层序地层学[J].石油与天然气地质,1995,16(2):89-97.
[4] 侯维虹,渠永宏,张永庆,等.通过地层沉积过程进行储集层的精细描述[J].石油勘探与开发,2004,31(增刊):106-109.
[5] 田景春,康建威,林小兵,等.台盆沉积体系及层序地层特征研究[J].西南石油大学学报:自然科学版,2007,29(6):39-42.
[6] 范春花,王英民,陈振岩,等.陈家洼陷沙三下亚段层序地层和沉积相分析[J].西南石油大学学报:自然科学版,2009,31(2):31-35.
[7] 李宏伟,朱怡翔,李胜利,等.辽河西部凹陷北部地区隐蔽油气藏预测与成藏机制分析[J].石油勘探与开发,2003,30(1):44-46.
[8] 于福生,吉珍娃,杨 雪,等.辽河盆地西部凹陷北部地区新生代断裂特征与圈闭类型[J].地球科学与环境学报,2007,29(2):149-153.
[9] 张凤奇,庞雄奇,冷济高,等.辽河西部凹陷构造圈闭含油性定量预测模型[J].西南石油大学学报:自然科学版,2009,31(2):27-30.
[10] 陈金龙,张庆龙,于兰兄,等.断层对辽河盆地杜229断块超稠油成藏与生产的影响[J]. 地球科学与环境学报,2006,28(3):48-52.
[11] 许 坤,潘耀丽,彭 峰.辽河盆地下第三系层序分析[J].地层学杂志,1997,21(4):267-274.
[12] 沈守文,彭大钧,颜其彬,等.层序地层学预测隐蔽油气藏的原理和方法[J].地球学报,2000,21(3):300-305.
[13] 徐怀大.层序地层学理论用于我国断陷盆地分析中的问题[J].石油与天然气地质,1991,12(1):52-57.
[14] 郝雪峰.陆相断陷盆地层序地层与成藏单元类比分析——以济阳拗陷为例[J].油气地质与采收率,2007,14(2):16-18.
[15] 邱桂强.陆相断陷盆地高精度层序地层研究现状与思路[J].油气地质与采收率,2005,12(3):1-4.
[16] 樊太亮,李卫东.层序地层应用于陆相油藏预测的成功实例[J].石油学报,1999,20(2):12-17.
[17] 廖兴明,姚继峰,于天庆,等.辽河盆地构造演化与油气[M].北京:石油工业出版社,1996.
[18] 高先志,李敬生,李晓光,等.辽河西部凹陷兴隆台—马圈子地区沙三段层序地层研究[C]∥匡立春,顾家裕,吕焕通,等.油气层序地层学新进展.北京:石油工业出版社,2006:68-69.
[19] 袁 波,陈世悦,袁文芳,等.辽西凹陷欢喜岭地区沙河街组层序格架的建立[J].西南石油大学学报:自然科学版,2008,30(2):27-30.
[20] 李德江,朱筱敏,董艳蕾,等.辽东湾拗陷古近系沙河街组层序地层分析[J].石油勘探与开发,2007,34(6):669-676.
[21] 鞠俊成,张凤莲,喻国凡,等.辽河盆地西部凹陷南部沙三段储层沉积特征及含油气性分析[J].古地理学报,2001,3(1):63-70.
[22] 林会喜,鄢继华,袁文芳,等.渤海湾盆地东营凹陷古近系沙河街组三段沉积相类型及平面分布特征[J].石油实验地质,2005,27(1):55-61.

Memo

Memo:
-
Last Update: 2010-09-20