THE DEVELOPMENT CHARACTERISTICS OF STRIKE-SLIP FAULTS AND THE ESTIMATION OF STRIKE-SLIP DISPLACEMENTS OF THE EASTERN LIAODONG BAY DEPRESSION

FANG Lu; WU Zhi-ping; LI Wei; ZHANG Jing; XIAO Yao; ZHANG Xi

Volume 23 Issue 3

Jun. 2017

Turn off MathJax

Article Contents

Article Navigation > Journal of Geomechanics > 2017 > 23(3): 459-466

FANG Lu, WU Zhi-ping, LI Wei, et al., 2017. THE DEVELOPMENT CHARACTERISTICS OF STRIKE-SLIP FAULTS AND THE ESTIMATION OF STRIKE-SLIP DISPLACEMENTS OF THE EASTERN LIAODONG BAY DEPRESSION. Journal of Geomechanics, 23 (3): 459-466.

Citation:

PDF( 3376 KB)

THE DEVELOPMENT CHARACTERISTICS OF STRIKE-SLIP FAULTS AND THE ESTIMATION OF STRIKE-SLIP DISPLACEMENTS OF THE EASTERN LIAODONG BAY DEPRESSION

FANG Lu^{1, 2
,},
WU Zhi-ping²,
LI Wei²,
ZHANG Jing²,
XIAO Yao²,
ZHANG Xi²

1.
Tarim Oilfield Company, PetroChina, Korla 841000, China
2.
School of Geosciences, China University of Petroleum, Qingdao 266580, China

More Information

Received: 2016-10-14
Published: 2017-06-28

Abstract

Abstract

Based on plenty of three dimensional seismic data, the horizontal and sectional characteristics of three main strike-slip faults in detail in the eastern Liaodong Bay Depression are described. Different faults have different characteristics and even the same fault has segmented differential features. The overall degree of strike-slip gradually increased from east to west, from north and south to the middle. With the method of physical modeling test, the strike-slip displacements of three main strike-slip faults in the eastern Liaodong Bay depression are estimated. The results show that the strike-slip displacement of Liaozhong Area is larger than that of Liaodong Area, and the strike-slip displacement and average strike-slip speeds of three strike-slip faults are the maximum in the Oligocene, illustrating there were strong strike-slips in the Oligocene.
- strike-slip fault,
- strike-slip displacement,
- physical modeling test,
- Liaodong Bay depression,
- Tan-Lu fault zone

FullText(HTML)

References(28)

References

[1]	余一欣, 周心怀, 徐长贵, 等.渤海辽东湾坳陷走滑断裂差异变形特征[J].石油与天然气地质, 2014, 35(5):632~638. doi: 10.11743/ogg20140507 YU Yi-xin, ZHOU Xin-huai, XU Chang-gui, et al. Differential deformation of strike slip faults in the Liaodongwan Depression, offshore Bohai Bay Basin[J]. Oil & Gas Geology, 2014, 35(5):632~638. doi: 10.11743/ogg20140507
[2]	柳永军, 徐长贵, 吴奎, 等.辽东湾坳陷走滑断裂差异性与大中型油气藏的形成[J].石油实验地质, 2015, 37(5):555~560. doi: 10.11781/sysydz201505555 LIU Yong-jun, XU Chang-gui, WU Kui, et al. Different characteristics of strike-slip faults and the formation of large and medium-scaled oil and gas fields in the Liaodong Bay Depression[J]. Petroleum Geology & Experiment, 2015, 37(5):555~560. doi: 10.11781/sysydz201505555
[3]	漆家福, 邓荣敬, 周心怀, 等.渤海海域新生代盆地中的郯庐断裂带构造[J].中国科学D辑:地球科学, 2008, 38(S1):19~29. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK2008S1003.htm QI Jia-fu, DENG Rong-jing, ZHOU Xin-huai, et al. Structural characteristics of the Tan-Lu fault zone in Cenozoic basins offshore the Bohai Sea[J]. Science in China Series D:Earth Sciences, 2008, 51(S1):20~31. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK2008S1003.htm
[4]	余一欣, 周心怀, 徐长贵, 等.渤海海域新生代断裂发育特征及形成机制[J].石油与天然气地质, 2011, 32(2):273~279. doi: 10.11743/ogg20110216 YU Yi-xin, ZHOU Xin-huai, XU Chang-gui, et al. Characteristics and formation mechanisms of the Cenozoic faults in the Bohai Sea waters[J]. Oil & Gas Geology, 2011, 32(2):273~279. doi: 10.11743/ogg20110216
[5]	柳永军, 朱文森, 杜晓峰, 等.渤海海域辽中凹陷走滑断裂分段性及其对油气成藏的影响[J].石油天然气学报, 2012, 34(7):6~10. http://www.cnki.com.cn/Article/CJFDTOTAL-JHSX201207003.htm LIU Yong-jun, ZHU Wen-sen, DU Xiao-feng, et al. Strike-slip fault subsections and its influence on hydrocarbon accumulation in Liaozhong depression of Bohai sea area[J]. Journal of Oil and Gas Technology, 2012, 34(7):6~10. http://www.cnki.com.cn/Article/CJFDTOTAL-JHSX201207003.htm
[6]	王国纯.郯庐断裂与渤海海域反转构造及花状构造[J].中国海上油气(地质), 1998, 12(5):289~295. http://www.cnki.com.cn/Article/CJFDTOTAL-ZHSD199805000.htm WANG Guo-chun. Relationship of Tanlu fault to the inversion and flower structures in Bohai Bay[J]. China Offshore Oil and Gas (Geology), 1998, 12(5):289~295. http://www.cnki.com.cn/Article/CJFDTOTAL-ZHSD199805000.htm
[7]	Hsiao L Y, Graham S A, Tilander N. Stratigraphy and sedimentation in a rift basin modified by synchronous strike-slip deformation:southern Xialiao basin, Bohai, offshore China[J]. Basin Research, 2010, 22(1):61~78. doi: 10.1111/bre.2010.22.issue-1
[8]	徐长贵.陆相断陷盆地源-汇时空耦合控砂原理:基本思想、概念体系及控砂模式[J].中国海上油气, 2013, 25(4):1~11, 21. http://www.cnki.com.cn/Article/CJFDTOTAL-ZHSD201304002.htm XU Chang-gui. Controlling sand principle of source-sink coupling in time and space in continental rift basin:basic idea, conceptual systems and controlling sand models[J]. China Offshore Oil and Gas, 2013, 25(4):1~11, 21. http://www.cnki.com.cn/Article/CJFDTOTAL-ZHSD201304002.htm
[9]	徐嘉炜.论走滑断层作用的几个主要问题[J].地学前缘, 1995, 2(1/2):125~136. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY502.000.htm XU Jia-wei. Some major problems on strike-slip faulting[J]. Earth Science Frontiers, 1995, 2(1/2):125~136. http://www.cnki.com.cn/Article/CJFDTOTAL-DXQY502.000.htm
[10]	Gilder S A, Leloup P H, Courtillot V, et al. Tectonic evolution of the Tancheng-Lujiang (Tan-Lu) fault via middle Triassic to early Cenozoic Paleomagnetic data[J]. Journal of Geophysical Research, 1999, 104(B7):15365~15390. doi: 10.1029/1999JB900123
[11]	万天丰, 朱鸿.郯庐断裂带的最大左行走滑断距及其形成时期[J].高校地质学报, 1996, 2(1):14~27. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX601.001.htm WAN Tian-feng, ZHU Hong. The maximum sinistral strike-slip and its forming age of Tancheng-Lujiang fault zone[J]. Geological Journal of Universities, 1996, 2(1):14~27. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX601.001.htm
[12]	李玉喜, 罗笃清, 云金表.走滑构造变形量估算方法探讨[J].石油勘探与开发, 1995, 22(1):13~15. http://www.cnki.com.cn/Article/CJFDTOTAL-SKYK501.003.htm LI Yu-xi, LUO Du-qing, YUN Jin-biao. Method of deformation estimiation of the strike-slip structures:a discussion[J]. Petroleum Exploration and Development, 1995, 22(1):13~15. http://www.cnki.com.cn/Article/CJFDTOTAL-SKYK501.003.htm
[13]	蔡东升, 罗毓晖, 姚长华.渤海莱州湾走滑拉分凹陷的构造研究及其石油勘探意义[J].石油学报, 2001, 22(2):19~25. doi: 10.7623/syxb200102004 CAI Dong-sheng, LUO Yu-hui, YAO Chang-hua. Strike-slip and pull-apart structure study and its significance to petroleum exploration on Laizhouwan sag, Bohai area[J]. Acta Petrolei Sinica, 2001, 22(2):19~25. doi: 10.7623/syxb200102004
[14]	余朝华, 韩清华, 董冬冬, 等.莱州湾地区郯庐断裂中段新生代右行走滑位移量的估算[J].天然气地球科学, 2008, 19(1):62~69. doi: 10.11764/j.issn.1672-1926.2008.01.62 YU Chao-hua, HAN Qing-hua, DONG Dong-dong, et al. Estimation of Cenozoic dextral strike-slip displacement of Tan-Lu fault in Laizhou Bay[J]. Natural Gas Geoscience, 2008, 19(1):62~69. doi: 10.11764/j.issn.1672-1926.2008.01.62
[15]	彭文绪, 张如才, 孙和风, 等.古新世以来郯庐断裂的位移量及其对莱州湾凹陷的控制[J].大地构造与成矿学, 2010, 34(4):585~592. http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201004019.htm PENG Wen-xu, ZHANG Ru-cai, SUN He-feng, et al. Displacement of the Tanlu fault since paleocene and its influence on the Laizhou Bay Sag, Bohai bay basin of China[J]. Geotectonica et Metallogenia, 2010, 34(40:585~592. http://www.cnki.com.cn/Article/CJFDTOTAL-DGYK201004019.htm
[16]	徐长贵, 任健, 吴智平, 等.辽东湾坳陷东部地区新生代断裂体系与构造演化[J].高校地质学报, 2015, 21(2):215~222. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX201502005.htm XU Chang-gui, REN Jian, WU Zhi-ping, et al. Cenozoic fault system and tectonic evolution of the eastern Liaodong Bay depression[J]. Geological Journal of China Universities, 2015, 21(2):215~222. http://www.cnki.com.cn/Article/CJFDTOTAL-GXDX201502005.htm
[17]	Riedel W. Zur mechanik geologischer brucherscheinungen[J]. Zentral-blatt fur Mineralogie, Geologie und Paleontologie, 1929, (B):354~368.
[18]	Wilcox R E, Harding T P, Seely D R. Basic wrench tectonics[J]. AAPG Bulletin, 1973, 57(1):74~96.
[19]	Naylor M A, Mandl G, Sijpesteijn C H K. Fault geometries in basement-induced wrench faulting under different initial stress states[J]. Journal of Structural Geology, 1986, 8(7):737~752. doi: 10.1016/0191-8141(86)90022-2
[20]	Dooley T P. Geometries and kinematics of strike-slip fault systems:insights from physical modelling and field studies[D]. London:Royal Holloway, University of London, 1994, 463~470.
[21]	An L J. Development of fault discontinuities in shear experiments[J]. Tectonophysics, 1998, 293(1/2):45~59.
[22]	Horsfield W T. An experimental approach to basement controlled faulting[J]. Geologie en Mijnbouw, 1977, 56:363~370.
[23]	McClay K R. Deformation mechanics in analogue models of extensional fault systems[J]. Geological Society, London, Special Publication, 1990, 54(1):445~453. doi: 10.1144/GSL.SP.1990.054.01.40
[24]	Krantz R W. Measurements of friction coefficients and cohesion for faulting and fault reactivation in laboratory models using sand and sand mixtures[J]. Tectonophysics, 1991, 188(1/2):203~207.
[25]	McClay K, Dooley T. Analogue models of pull-apart basins[J]. Geology, 1995, 23(7):711~714.
[26]	Richard P D, Naylor M A, Koopman A. Experimental models of strike-slip tectonics[J]. Petroleum Geoscience, 1995, 1(1):71~80. doi: 10.1144/petgeo.1.1.71
[27]	McClay K, Bonora M. Analog models of restraining stepovers in strike-slip fault systems[J]. AAPG Bulletin, 2001, 85(2):233~260.
[28]	李伟, 刘超, 张江涛, 等.北部湾盆地迈陈凹陷东部断裂系统成因演化机制的构造物理模拟[J].中国石油大学学报(自然科学版), 2015, 39(3):38~46. http://www.cnki.com.cn/Article/CJFDTOTAL-SYDX201503005.htm LI Wei, LIU Chao, ZHANG Jiang-tao, et al. Structure physical modeling experiment of evolutionary mechanism about fault system in eastern area of Maichen sag, Beibu-gulf Basin[J]. Journal of China University of Petroleum, 2015, 39(3):38~46. http://www.cnki.com.cn/Article/CJFDTOTAL-SYDX201503005.htm