FAULT ACTIVITY FEATURES OF TONGCHENG FAULT ZONE IN JINHU SAG

ZHANG Xiang-cheng; DAI Jun-sheng; ZOU Juan; WANG Xin-xin; YUE Xi-wei; WU Ya

Volume 20 Issue 4

Dec. 2014

Turn off MathJax

Article Contents

Article Navigation > Journal of Geomechanics > 2014 > 20(4): 424-433

ZHANG Xiang-cheng, DAI Jun-sheng, ZOU Juan, et al., 2014. FAULT ACTIVITY FEATURES OF TONGCHENG FAULT ZONE IN JINHU SAG. Journal of Geomechanics, 20 (4): 424-433.

Citation:

ZHANG Xiang-cheng, DAI Jun-sheng, ZOU Juan, et al., 2014. FAULT ACTIVITY FEATURES OF TONGCHENG FAULT ZONE IN JINHU SAG. Journal of Geomechanics, 20 (4): 424-433.

Citation:

ZHANG Xiang-cheng, DAI Jun-sheng, ZOU Juan, et al., 2014. FAULT ACTIVITY FEATURES OF TONGCHENG FAULT ZONE IN JINHU SAG. Journal of Geomechanics, 20 (4): 424-433.

PDF( 21364 KB)

FAULT ACTIVITY FEATURES OF TONGCHENG FAULT ZONE IN JINHU SAG

Faculty of Earth Science and Technology, China University of Petroleum, Qingdao 266580, Shandong, China

More Information

Received: 2014-07-05
Published: 2014-12-01

Abstract

Abstract

According to the interpretation of information of seismology and geology, structural features of Tongcheng fault zone is analyzed; the features and the stages of tectonic evolution are discussed. The research shows that the Tongcheng fault zone mainly develops NE-SW strike faults. Most faults are formed in the Funing period and Sanduo period. Tilt rotation of the blocks is obvious. The structures of fault block and fault nose are developed. Cenozoic tectonic activity shows alternating strong and weak characteristics, and fault activity is complex. The intensity of fault activity in Funing phase is gradually strengthened, and become relatively weak in Dainan period, In the Sanduo phase fault activity enhances, then fault activity largely discontinues. The differential fluctuation in Tongcheng fault is obvious on both sides of strata. Tectonic evolution of Tongcheng fault zone can be divided into four period: fault block development stage (Funing period), differential fluctuation stage (Dainan and Sanduo period), overthrust folded stage (Late Sanduo period), structure stable stage (Neogene and Quaternary). With the superposition of Wubao movement, Sanduo movement and early influence of basement faults, Tongcheng fault zone causes the development of fault nose structure, complex fault block structure and arc fault trap, which provides good places for oil-gas accumulation.
- Jinhu sag,
- tectonic evolution,
- fault activity,
- fault fall,

FullText(HTML)

References(19)

References

[1]	祝厚勤, 庞雄奇, 王文军.苏北盆地盐城凹陷朱家墩气藏成藏期次研究[J].煤田地质与勘探, 2006, (2):26~29. http://www.cnki.com.cn/Article/CJFDTOTAL-MDKT200602007.htm ZHU Hou-qin, PANG Xiong-qi, WANG Wen-jun. Study on accumulation stage of Zhujiadun gas pool in Yancheng depression, Subei Basin[J]. Coal Geology & Exploration, 2006, (2): 26~29. http://www.cnki.com.cn/Article/CJFDTOTAL-MDKT200602007.htm
[2]	赵勇, 戴俊生.应用落差分析研究生长断层[J].石油勘探与开发, 2003, 30(3):13~15. http://www.cnki.com.cn/Article/CJFDTOTAL-SKYK200303003.htm ZHAO Yong, DAI Jun-sheng. Identification of growth fault by fault fall analysis[J]. Petroleum Exploration and Development, 2003, 30(3): 13~15. http://www.cnki.com.cn/Article/CJFDTOTAL-SKYK200303003.htm
[3]	卢异, 王书香, 陈松, 等.一种断裂活动强度计算方法及其应用[J].天然气地球科学, 2010, 21(4):612~616. http://www.cnki.com.cn/Article/CJFDTOTAL-TDKX201004016.htm LU Yi, WANG Shu-xiang, CHEN Song, et al. Computing method about intensity of fault activity and its application[J]. Natural Gas Geoscience, 2010, 21(4): 612~616. http://www.cnki.com.cn/Article/CJFDTOTAL-TDKX201004016.htm
[4]	陈刚, 戴俊生, 叶兴树, 等.生长指数与断层落差的对比研究[J].西南石油大学报, 2007, 29(3):20~23. http://www.cnki.com.cn/Article/CJFDTOTAL-XNSY200703005.htm CHEN Gang, DAI Jun-sheng, YE Xing-shu, et al. A comparison of the fault growth index with fault throw[J]. Journal of Southwest Petroleum University, 2007, 29(3): 20~23. http://www.cnki.com.cn/Article/CJFDTOTAL-XNSY200703005.htm
[5]	叶兴树, 王伟锋, 戴俊生, 等.东营凹陷沙三-东营期断裂活动特征[J].中国石油大学学报:自然科学版, 2006, 30(4):7~11. http://www.cnki.com.cn/Article/CJFDTOTAL-SYDX200604001.htm YE Xing-shu, WANG Wei-feng, DAI Jun-sheng, et al. Characteristics of fault activities of Sha-3 Member and Dongying periods in Dongying depression[J]. Journal of China University of Petroleum: Natural Science Edition, 2006, 30(4): 7~11. http://www.cnki.com.cn/Article/CJFDTOTAL-SYDX200604001.htm
[6]	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. http://www.cnki.com.cn/Article/CJFDTOTAL-XASY200704009.htm MA Xiao-ming, DAI Jun-sheng. Study on the control faults in south fault terrace of Gao you Sag by fault throw analysis[J]. Journal of Xi'an Shi You University: Natural Science Edition, 2007, 22(4): 31~34. http://www.cnki.com.cn/Article/CJFDTOTAL-XASY200704009.htm
[7]	叶绍东.金湖凹陷铜城断层构造特征与油气成藏[J].地质力学学报, 2012, 18(2):187~194. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20120209&journal_id=dzlxxb YE Shao-dong. Study on the control faults in south fault terrace of Gaoyou sag by fault throw analysis [J]. Journal of Geomechanics, 2012, 18(2): 187~194. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?flag=1&file_no=20120209&journal_id=dzlxxb
[8]	Dahlstrom C D A. Balanced cross sections[J]. Canadian Journal of Earth Sciences, 1969, 6(4): 743~757. doi: 10.1139/e69-069
[9]	De Paor D G. Balanced section in thrust belts part 1: Construction[J]. AAPG Bulletin, 1988, 72(1): 73~90. http://archives.datapages.com/data/bulletns/1988-89/data/pg/0072/0001/0050/0073.htm?q=%2BtextStrip%3Atrap+textStrip%3Aclassification+textStrip%3Alevels
[10]	戴俊生, 李理.油区构造分析[M].青岛:中国石油大学出版社, 2002:92~95. DAI Jun-sheng, LI Li. Structural analysis of oil province[M]. Qingdao: China University of Petroleum Press, 2002:92~95.
[11]	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. http://www.cnki.com.cn/Article/CJFDTOTAL-XAGX200301007.htm WANG Yun-suo, LIU Ya-zhou, ZHANG Xiao-yi, et al. Flow diagram and the geological significance of balance section[J]. Journal of Chang'an University: Earth Science Edition, 2003, 25(1): 28~32. http://www.cnki.com.cn/Article/CJFDTOTAL-XAGX200301007.htm
[12]	戴俊生, 马欣本, 王志云, 等.闵桥油田阜宁组的构造特征和构造演化[J].大地构造与成矿学, 2002, 26(2):126~130. http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK200202002.htm DAI Jun-sheng, MA Xin-ben, WANG Zhi-yun, et al. Tectonic characteristic and tectonic evolution of the Funing Formation in Minqiao oilfield[J]. Geotectonic et Metallogenia, 2002, 26(2): 126~130. http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK200202002.htm
[13]	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. http://www.cnki.com.cn/Article/CJFDTOTAL-XASY200902012.htm WANG Xia-tian, DAI Jun-sheng, XIE Jun-yu. Structural characteristics and structural evolution of Shanian Block area in Gaoyou sag[J]. Journal of Xi'an Shiyou University: Natrual Science, 2009, 24(2): 43~46. http://www.cnki.com.cn/Article/CJFDTOTAL-XASY200902012.htm
[14]	王福焕, 王振宇, 张云峰, 等.轮古东奥陶系断裂特征及其对油气成藏的控制[J].中国石油勘探, 2011, 16(1):15~20. http://www.cnki.com.cn/Article/CJFDTOTAL-KTSY201101002.htm WAGN Fu-huan, WANG Zhen-yu. ZHANG Yun-feng, et al. Fault characteristics and their controlling roles to hydrocarbon pool-formation of Ordovician in eastern Lungu[J]. China Petroleum Exploration, 2011, 16(1): 15~20. http://www.cnki.com.cn/Article/CJFDTOTAL-KTSY201101002.htm
[15]	于俊吉, 罗群, 张多军, 等.北部湾盆地海南福山凹陷断裂特征及其对油气成藏的控制作用[J].石油实验地质, 2004, 26(3):241~248. doi: 10.11781/sysydz200403241 YU Jun-ji, LUO Qun, ZHANG Duo-jun, et al. Characteristics of faults in the Fushan depression of Hainan, the Beibuwan Basin and their controlling roles to hydrocarbon pool-formation[J]. Petroleum Geology & Experiment, 2004, 26(3): 241~248. doi: 10.11781/sysydz200403241
[16]	蔡佑星.济阳坳陷断裂发育特征及其对油气成藏的控制作用[J].天然气地球科学, 2008, 19(1):56~61. doi: 10.11764/j.issn.1672-1926.2008.01.56 CAI You-xing. Characteristics of fault developed in Jiyang sag and its control over hydrocarbon migration and accumulation[J]. Natural Gas Geoscience, 2008, 19(1): 56~61. doi: 10.11764/j.issn.1672-1926.2008.01.56
[17]	方向, 江波, 张永庶.柴达木盆地西部地区断裂构造与油气聚集[J].石油与天然气地质, 2006, 27(1):56~61. doi: 10.11743/ogg20060110 FANG Xiang, JIANG Bo, ZHANG Yong-shu. Faulted structure and hydrocarbon accumulation in western Qaidam basin[J]. Oil & Gas Geology, 2006, 27(1): 56~61. doi: 10.11743/ogg20060110
[18]	刘世丽, 胡爱玉, 李书瑜.金湖凹陷石港断裂带断层封闭性研究[J].海洋石油, 2007, 26(4): 34~38. http://www.cnki.com.cn/Article/CJFDTOTAL-TTSD201303010.htm LIU Shi-li, HU Ai-yu, LI Shu-yu. Study on the faults sealing properties of Shigang fault zone in Jinhu Depression[J]. Offshore Oil, 2007, 26(4): 34~38. http://www.cnki.com.cn/Article/CJFDTOTAL-TTSD201303010.htm
[19]	能源, 漆家福, 张春峰, 等.金湖凹陷断裂特征及其石油地质意义[J].大地构造与成矿学, 2012, 36(1):16~23. http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201201006.htm NENG Yuan, QI Jia-fu, ZHANG Chun-feng, et al. Structural features of the Jinhu sag in the Subei Basin and its petroleum geological significance[J]. Geotectonica Et Metallogenia, 2012, 36(1): 16~23. http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201201006.htm