|Table of Contents|

Structural Feature and Tectonic Evolution of Western Slope in Jinhu Sag, Subei Basin(PDF)

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

Issue:
2011年第04期
Page:
349-353
Research Field:
基础地质与矿产地质
Publishing date:

Info

Title:
Structural Feature and Tectonic Evolution of Western Slope in Jinhu Sag, Subei Basin
Author(s):
ZHANG Hong-guo1DAI Jun-sheng1WANG Xia-tian2FU Da-wei1
1. School of Geosciences, China University of Petroleum, Qingdao 266555, Shandong, China; 2. Research Institute of Exploration and Development, Xinjiang Oilfield Company, China National Petroleum Corporation, Karamay 834000, Xinjiang, China
Keywords:
structural feature tectonic evolution evolutionary phase fault activity Cenozoic western slope Jinhu Sag Subei Basin
PACS:
TE121.2
DOI:
-
Abstract:
Based on the interpretation of geological and geophysical data in Jinhu Sag, Subei Basin, according to the background and section of regional tectonic evolution, structural feature of Jinhu Sag was described, the stages of tectonic evolution of western slope in the sag were divided, and the characteristics of tectonic evolution were discussed. The results showed that the fault structure developed in western slope of Jinhu Sag; most of the faults were curving, and faults were mainly in small level; combination of fault was mainly extensional, and the trap of fault block developed; tectonic evolution of western slope during the Cenozoic could be divided into slope developing stage(Paleocene Funing Period), differential fluctuation stage(Eocene Dainan-Sanduo Period), overthrust folded stage(Late Eocene Sanduo Period)and structure stable stage(Neogene and Quaternary); Cenozoic tectonic activity was strong and weak in turn; difference of fault activity was significant, and intensity and scale of faulting during Paleocene Funing Period and Eocene Sanduo Period were comparatively strong; faults rose west and descended east during Cenozoic, and it was favorable to accumulate the oil and gas from the deep sag of eastern slope and to form oil/gas reservoir.

References:

[1] 金 强,任怀强,杨少春.金湖凹陷箕状湖盆缓坡未熟油断块油藏的形成[J].石油大学学报:自然科学版,1997,21(2):21-24.
[2] 章 冉,刘红正.金湖凹陷西斜坡地区地震解释方法应用研究[J].石油天然气学报,2009,31(2):283-285.
[3] 戴俊生.构造地质学及大地构造[M].北京:石油工业出版社,2006.
[4] 孙和风,周心怀,彭文绪,等.莱州湾凹陷东部走滑带盐相关构造特征[J].地球科学与环境学报,2008,30(4):380-384.
[5] 郭 涛,张卫海,袁 巍.临南油田街2断块沙三上亚段Ⅴ砂岩组沉积微相研究[J].地球科学与环境学报,2010,32(4):363-367.
[6] 渠 芳,陈清华.对孤岛油田西南缘断层活动性的新认识[J].地球科学与环境学报,2009,31(4):394-399.
[7] 王 平.为什么二、三级断层对油气聚集起控制作用[J].断块油气田,1994,1(5):1-5.
[8] 王运所,刘亚洲,张孝义,等.平衡剖面的制作流程及其地质意义[J].长安大学学报:地球科学版,2003,25(1):28-32.
[9] 戴俊生,冀国胜,马欣本,等.闵桥油田阜宁组的构造特征及构造演化[J].大地构造与成矿学,2002,26(2):126-130.
[10] 王霞田,戴俊生,解俊昱.高邮凹陷沙埝断块区的构造特征和构造演化[J].西安石油大学学报:自然科学版,2009,24(2):43-46.
[11] 马晓鸣,戴俊生.应用落差分析研究高邮凹陷南断阶主控断层[J].西安石油大学学报:自然科学版,2007,22(4):31-34.
[12] 陈 刚,戴俊生,叶兴树,等.生长指数与断层落差的对比研究[J].西南石油大学学报,2007,29(3):20-23.
[13] 于翠玲,曾溅辉.断层幕式活动期和间歇期流体运移与油气成藏特征[J].石油实验地质,2005,27(2):129-133.
[14] 万丛礼,付金华,张 军. 鄂尔多斯西缘前陆盆地构造-热事件与油气运移[J].地球科学与环境学报,2005,27(2):43-47.
[15] 鲁雪松,马淑芳,杨贵丽.苏北盆地金湖凹陷三垛组剥蚀厚度恢复及意义[J].西南石油大学学报:自然科学版,2009,31(4):13-17.
[16] 徐春强,蒋有录,程 奇,等.东濮凹陷濮卫洼陷油气成藏期分析[J].地球科学与环境学报,2010,31(3):257-262.
[17] 孙和风,周心怀,彭文绪.莱州湾凹陷油气成藏动力学特征[J].西安石油大学学报:自然科学版,2009,24(4):27-31.
[18] 段云歌,常象春.临南洼陷岩性油藏成藏动力与含油性分析[J].地球科学与环境学报,2009,31(3):272-276.
[19] 刘 军,刘喜玲,田 骏.苏北盆地金湖凹陷油气运移与聚集规律[J].石油天然气学报,2005,27(6):693-694.

Memo

Memo:
-
Last Update: 2011-12-20