塔里木盆地FⅠ17走滑断裂北段奥陶纪差异变形机制

doi:10.7657/XJPG20240403

新疆石油地质 ›› 2024, Vol. 45 ›› Issue (4): 401-408.doi: 10.7657/XJPG20240403

塔里木盆地F_Ⅰ17走滑断裂北段奥陶纪差异变形机制

蔡振忠¹^,²^,³(), 李兵²^,³^,⁴(), 罗枭²^,³^,⁴, 李会元²^,³^,⁴, 李梦勤²^,³^,⁴, 李正阳²^,³^,⁴, 王青红²^,³^,⁴

1.中国石油塔里木油田分公司，新疆库尔勒 841000
2.中国石油天然气集团有限公司深层复杂油气藏勘探开发技术研发中心，新疆库尔勒 841000
3.新疆维吾尔自治区超深层复杂油气藏勘探开发工程研究中心，新疆库尔勒 841000
4.中国石油塔里木油田分公司勘探开发研究院，新疆库尔勒 841000

收稿日期:2024-02-24 修回日期:2024-03-11 出版日期:2024-08-01 发布日期:2024-07-23
通讯作者: 李兵（1995-），男，湖北黄梅人，工程师，硕士，碳酸盐岩油气藏地质，（Tel）0996-2172889（Email）libing1-tlm@petrochina.com.cn
作者简介:蔡振忠（1970-），男，福建莆田人，教授级高级工程师，博士，油气勘探开发，（Email）caizz-tlm@petrochina.com.cn
基金资助:
中国石油前瞻性基础性技术攻关项目(2021DJ1501)

Ordovician Differential Deformation Mechanism of Northern Section of F_Ⅰ17 Strike-Slip Fault, Tarim Basin

CAI Zhenzhong¹^,²^,³(), LI Bing²^,³^,⁴(), LUO Xiao²^,³^,⁴, LI Huiyuan²^,³^,⁴, LI Mengqin²^,³^,⁴, LI Zhengyang²^,³^,⁴, WANG Qinghong²^,³^,⁴

1. Tarim Oilfield Company, PetroChina, Korla, Xinjiang 841000, China
2. R&D Center for Ultra-Deep Complex Reservoir Exploration and Development, CNPC, Korla, Xinjiang 841000, China
3. Xinjiang Engineering Research Center for Ultra-Deep Complex Reservoir Exploration and Development, Korla, Xinjiang 841000, China
4. Research Institute of Exploration and Development, Tarim Oilfield Company, PetroChina, Korla, Xinjiang 841000, China;

Received:2024-02-24 Revised:2024-03-11 Online:2024-08-01 Published:2024-07-23

摘要/Abstract

摘要：

为明确走滑断裂对碳酸盐岩油气成藏的作用，基于三维地震资料，分析F_Ⅰ17走滑断裂北段的发育特征与构造变形过程，结合地质建模，开展走滑断裂形成及演化的砂箱物理模拟。研究区内的F_Ⅰ17走滑断裂可分为南、北2段，南段为近北东—南西走向，主要发育雁列式断裂，奥陶纪一间房组整体以隆升为主，垂向上的变形幅度较大；北段为近北北东—南南西走向，主要发育线性走滑断裂，在奥陶纪一间房组变形微弱，局部地区可见地层微幅度下掉。砂箱物理模拟实验结果表明：线性走滑断裂的主位移带上会形成一系列隆起带，而走向偏转的走滑断裂在南段形成一系列隆起带，在北段则表现为地层下掉；在同一应力条件下，走滑断裂初始走向的差异会导致断裂受力发生变化，进而影响其演化过程。F_Ⅰ17走滑断裂南段的压隆段应力更加集中，局部裂缝和溶洞更发育，油气更为富集，油气勘探效果优于北段。

关键词: 塔里木盆地, 阿满过渡带, 奥陶纪, 走滑断裂, 差异变形机制, 物理模拟

Abstract:

To understand the role of strike-slip faults in hydrocarbon accumulation in carbonate reservoirs, based on 3D seismic data, the development characteristics and tectonic deformation processes of the northern section of the F_Ⅰ17 strike-slip fault in the Tarim basin were analyzed, and a sandbox physical simulation was performed on the formation and evolution of strike-slip faults by using geological modeling. The F_Ⅰ17 strike-slip fault is divided into two sections. The southern section, nearly NE-SW trending, is characterized by en echelon faults, with the Yijianfang formation showing a uplifting feature and significant vertical deformation during the Ordovician period. The northern section, nearly NNE-SSW trending, is dominated by linear strike-slip faults, with the Yijianfang formation exhibiting weak deformation and slight subsidence in local areas during the Ordovician period. Sandbox physical simulation results show that a series of uplift zones formed along the main displacement zone of linear strike-slip faults, while the deflected strike-slip faults formed a series of uplift zones in the southern section and presented strata subsidence in the northern section. Under identical stress conditions, differences in the initial strikes of strike-slip faults lead to the changes in the stress put on the faults, thereby influencing their evolution processes. The southern section of the F_Ⅰ17 strike-slip fault is found with more concentrated stress in compressional uplift zone and more developed fractures and vugs locally, containing richer hydrocarbons. The southern section is expected to be superior in exploration to the northern section.

Key words: Tarim basin, Aman transitional zone, Ordovician period, strike-slip fault, differential deformation mechanism, physical simulation

中图分类号:

TE121.2

蔡振忠, 李兵, 罗枭, 李会元, 李梦勤, 李正阳, 王青红. 塔里木盆地F_Ⅰ17走滑断裂北段奥陶纪差异变形机制[J]. 新疆石油地质, 2024, 45(4): 401-408.

CAI Zhenzhong, LI Bing, LUO Xiao, LI Huiyuan, LI Mengqin, LI Zhengyang, WANG Qinghong. Ordovician Differential Deformation Mechanism of Northern Section of F_Ⅰ17 Strike-Slip Fault, Tarim Basin[J]. Xinjiang Petroleum Geology, 2024, 45(4): 401-408.

图/表 8

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表2

参考文献 34

[1]	HILL M L. San Andreas fault:History of concepts[J]. Geological Society of America Bulletin, 1981,92:112-131.
[2]	SYLVESTER A G. Strike-slip faults[J]. Geological Society of America Bulletin, 1988, 100(11):1666-1703.
[3]	WOODCOCK N H. The role of strike-slip fault systems at plate boundaries[J]. Royal Society of London Philosophical Transactions (Series A), 1986,317:13-29.
[4]	COOPER A F, NORRIS R J. Anatomy,structural evolution,and slip rate of a plate-boundary thrust:The Alpine fault at Gaunt Creek,Westland,New Zealand[J]. Geological Society of America Bulletin, 1994, 106(5):627-633.
[5]	徐嘉炜, 马国锋. 郯庐断裂带研究的十年回顾[J]. 地质论评, 1992, 38(4):316-324.
	XU Jiawei, MA Guofeng. Review of ten years of research on the Tancheng-Lujiang fault zone[J]. Geological Review, 1992, 38(4):316-324.
[6]	朱光, 徐嘉炜, 孙世群. 郯庐断裂带平移时代的同位素年龄证据[J]. 地质论评, 1995, 41(5):452-456.
	ZHU Guang, XU Jiawei, SUN Shiqun. Isotopic age evidence for the timing of strike-slip movement of the Tan-Lu fault zone[J]. Geological Review, 1995, 41(5):452-456.
[7]	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.
	WAN Tianfeng, 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.
[8]	乔秀夫, 张安棣. 华北块体、胶辽朝块体与郯庐断裂[J]. 中国地质, 2002, 29(4):337-345.
	QIAO Xiufu, ZHANG Andi. North China block,Jiao-Liao-Korea block and Tanlu fault[J]. Geology in China, 2002, 29(4):337-345.
[9]	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.
	YU Yixin, ZHOU Xinhuai, XU Changgui, 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.
[10]	刘永江, 葛肖虹, GENSER J, 等. 阿尔金断裂带构造活动的40Ar/39Ar年龄证据[J]. 科学通报, 2003, 48(12):1335-1341.
	LIU Yongjiang, GE Xiaohong, GENSER J, et al. 40Ar/39Ar age evidence for tectonic activity in the Altun fault zone[J]. Chinese Science Bulletin, 2003, 48(12):1335-1341.
[11]	李海兵, 杨经绥, 许志琴, 等. 阿尔金断裂带对青藏高原北部生长、隆升的制约[J]. 地学前缘, 2006, 13(4):59-79.
	LI Haibing, YANG Jingsui, XU Zhiqin, et al. The constraint of the Altyn Tagh fault system to the growth and rise of the northern Tibetan plateau[J]. Earth Science Frontiers, 2006, 13(4):59-79.
[12]	雷超, 任建业, 裴健翔, 等. 莺歌海-琼东南盆地结合部记录的红河断裂带向海延伸及其演化过程[J]. 中国科学:地球科学, 2022, 52(1):81-97.
	LEI Chao, REN Jianye, PEI Jianxiang, et al. Tectonics of the offshore Red River fault recorded in the junction of the Yinggehai and Qiongdongnan basins[J]. Science China Earth Sciences, 2022, 52(1):81-97.
[13]	汪健, 申重阳, 孙文科, 等. 红河断裂带北、中段近期重力变化及深部变形[J]. 地震地质, 2021, 43(6):1537-1562. doi: 10.3969/j.issn.0253-4967.2021.06.011
	WANG Jian, SHEN Chongyang, SUN Wenke, et al. Study on present gravity change and deep crust deformation in the northern and middle sections of the Red River fault zone[J]. Seismology and Geology, 2021, 43(6):1537-1562. doi: 10.3969/j.issn.0253-4967.2021.06.011
[14]	GOGONENKOV G N, TIMURZIEV A I. Strike-slip faults in the west Siberian basin:Implications for petroleum exploration and development[J]. Russian Geology and Geophysics, 2010, 51(3):304-316.
[15]	DENG Shang, LI Huili, ZHANG Zhongpei, et al. Structural characterization of intracratonic strike-slip faults in the central Tarim basin[J]. AAPG Bulletin, 2019, 103(1):109-137. doi: 10.1306/06071817354
[16]	TENG Changyu, CAI Zhongxian, HAO Fang, et al. Structural geometry and evolution of an intracratonic strike-slip fault zone:A case study from the north SB5 fault zone in the Tarim basin,China[J]. Journal of Structural Geology, 2020,140:104159.
[17]	焦方正, 杨雨, 冉崎, 等. 四川盆地中部地区走滑断层的分布与天然气勘探[J]. 天然气工业, 2021, 41(8):92-101.
	JIAO Fangzheng, YANG Yu, RAN Qi, et al. Distribution and gas exploration of the strike-slip faults in the central Sichuan basin[J]. Natural Gas Industry, 2021, 41(8):92-101.
[18]	漆立新. 塔里木盆地顺托果勒隆起奥陶系碳酸盐岩超深层油气突破及其意义[J]. 中国石油勘探, 2016, 21(3):38-51.
	QI Lixin. Oil and gas breakthrough in ultra-deep Ordovician carbonate formations in Shuntuoguole uplift,Tarim basin[J]. China Petroleum Exploration, 2016, 21(3):38-51.
[19]	焦方正. 塔里木盆地顺托果勒地区北东向走滑断裂带的油气勘探意义[J]. 石油与天然气地质, 2017, 38(5):831-839.
	JIAO Fangzheng. Significance of oil and gas exploration in NE strike-slip fault belts in Shuntuoguole area of Tarim basin[J]. Oil & Gas Geology, 2017, 38(5):831-839.
[20]	韩剑发, 苏洲, 陈利新, 等. 塔里木盆地台盆区走滑断裂控储控藏作用及勘探潜力[J]. 石油学报, 2019, 40(11):1296-1310. doi: 10.7623/syxb201911002
	HAN Jianfa, SU Zhou, CHEN Lixin, et al. Reservoir-controlling and accumulation-controlling of strike-slip faults and exploration potential in the platform of Tarim basin[J]. Acta Petrolei Sinica, 2019, 40(11):1296-1310. doi: 10.7623/syxb201911002
[21]	王清华, 杨海军, 汪如军, 等. 塔里木盆地超深层走滑断裂断控大油气田的勘探发现与技术创新[J]. 中国石油勘探. 2021, 26(4):58-71.
	WANG Qinghua, YANG Haijun, WANG Rujun, et al. Discovery and exploration technology of fault-controlled large oil and gas fields of ultra-deep formation in strike slip fault zone in Tarim basin[J]. China Petroleum Exploration, 2021, 26(4):58-71.
[22]	王清华, 杨海军, 李勇, 等. 塔里木盆地富满大型碳酸盐岩油气聚集区走滑断裂控储模式[J]. 地学前缘, 2022, 29(6):239-251. doi: 10.13745/j.esf.sf.2022.8.17
	WANG Qinghua, YANG Haijun, LI Yong, et al. Control of strike-slip fault on the large carbonate reservoir in Fuman,Tarim basin:A reservoir model[J]. Earth Science Frontiers, 2022, 29(6):239-251. doi: 10.13745/j.esf.sf.2022.8.17
[23]	黄诚. 叠合盆地内部小尺度走滑断裂幕式活动特征及期次判别:以塔里木盆地顺北地区为例[J]. 石油实验地质, 2019, 41(3):379-389.
	HUANG Cheng. Multi-stage activity characteristics of small-scale strike-slip faults in superimposed basin and its identification method:A case study of Shunbei area,Tarim basin[J]. Petroleum Geology & Experiment, 2019, 41(3):379-389.
[24]	邬光辉, 马兵山, 韩剑发, 等. 塔里木克拉通盆地中部走滑断裂形成与发育机制[J]. 石油勘探与开发, 2021, 48(3):510-520. doi: 10.11698/PED.2021.03.07
	WU Guanghui, MA Bingshan, HAN Jianfa, et al. Origin and growth mechanisms of strike-slip faults in the central Tarim cratonic basin,NW China[J]. Petroleum Exploration and Development, 2021, 48(3):510-520.
[25]	贾承造, 马德波, 袁敬一, 等. 塔里木盆地走滑断裂构造特征、形成演化与成因机制[J]. 天然气工业, 2021, 41(8):81-91.
	JIA Chengzao, MA Debo, YUAN Jingyi, et al. Structural characteristics,formation & evolution and genetic mechanisms of strike-slip faults in the Tarim basin[J]. Natural Gas Industry, 2021, 41(8):81-91.
[26]	刘军, 廖茂辉, 王来源, 等. 顺北油田顺北4号断裂带中段断控储集体连通性评价[J]. 新疆石油地质, 2023, 44(4):456-464.
	LIU Jun, LIAO Maohui, WANG Laiyuan, et al. Static connectivity evaluation on fault-controlled reservoir system in the middle section of Shunbei No.4 fault zone,Shunbei oilfield[J]. Xinjiang Petroleum Geology, 2023, 44(4):456-464.
[27]	代兰, 邬光辉, 陈鑫, 等. 共轭走滑断裂形成演化的控制因素及物理模拟实验[J]. 新疆石油地质, 2023, 44(1):43-50.
	DAI Lan, WU Guanghui, CHEN Xin, et al. Controlling factors and physical simulation experiments on formation and evolution of conjugate strike-slip faults[J]. Xinjiang Petroleum Geology, 2023, 44(1):43-50.
[28]	王清华. 塔里木盆地17号走滑断裂带北段差异变形与演化特征[J]. 现代地质, 2023:37(5):1136-1145.
	WANG Qinghua. Differential deformation and evolution characteristics of the No.17 strike-slip fault zone in the Tarim basin[J]. Geoscience, 2023:37(5):1136-1145.
[29]	刘强, 张银涛, 陈石, 等. 塔里木盆地走滑断裂发育演化特征精细解析及其地质意义:以富满油田F_Ⅰ17断裂为例[J]. 现代地质, 2023, 37(5):1123-1135.
	LIU Qiang, ZHANG Yintao, CHEN Shi, et al. Development and evolution characteristics of strike-slip faults in Tarim basin and its geological significance:A case study of F_Ⅰ17 fault in Fuman oilfield[J]. Geoscience, 2023, 37(5):1123-1135.
[30]	宋兴国, 陈石, 谢舟, 等. 塔里木盆地富满油田东部走滑断裂发育特征与油气成藏[J]. 石油与天然气地质, 2023, 44(2):335-349.
	SONG Xingguo, CHEN Shi, XIE Zhou, et al. Strike-slip faults and hydrocarbon accumulation in the eastern part of Fuman oilfield,Tarim basin[J]. Oil & Gas Geology, 2023, 44(2):335-349.
[31]	WANG L, MAESTRELLI D, CORTI G, et al. 2021. Normal fault reactivation during multiphase extension:Analogue models and application to the Turkana depression,East Africa[J]. Tectonophysics,2021,811:228870.
[32]	ZWAAN F, CHENIN P, ERRATT D, et al. Competition between 3D structural inheritance and kinematics during rifting:Insights from analogue models[J]. Basin Research, 2022,34:824-854.
[33]	肖阳, 邬光辉, 雷永良, 等. 走滑断裂带贯穿过程与发育模式的物理模拟[J]. 石油勘探与开发, 2017, 44(3):340-348. doi: 10.11698/PED.2017.03.03
	XIAO Yang, WU Guanghui, LEI Yongliang, et al. Analogue modeling of through-going process and development pattern of strike-slip fault zone[J]. Petroleum Exploration and Development, 2017, 44(3):340-348.
[34]	QIU Huabiao, DENG Sheng, CAO Zicheng, et al. The evolution of the complex anticlinal belt with crosscutting strike‐slip faults in the central Tarim basin,NW China[J]. Tectonics, 2019,38:2087-2113.

类型	厚度/ m	密度/ （g·cm^-3）	重力加速度/ （m·s^-2）	黏聚强度/Pa	黏度/ （Pa·s）	速率/ （m·s^-1）
实验模型	1	1.13	9.8	50~500	1.2×10⁴	1×10^-5
地质原型	1×10⁵~5×10⁵	2.30~2.50	9.8	1×10⁷~5×10⁷	1.0×10¹⁹	3×10^-10

位移量/ cm	第一组实验	第二组实验
位移量/ cm	北段与南段一致	北段	南段
1	右阶雁列式断裂（R破裂），地层微幅度隆起	右阶雁列式断裂（R破裂），地层略微下掉	未产生断裂，地层条带状微幅度隆起
2	R破裂长度增大，Y破裂形成并连接R破裂，地层隆起幅度更大	R破裂长度增大，Y破裂形成并连接R破裂，地层下掉幅度增大	右阶排列的R破裂，地层隆起幅度增大
3	R破裂不再活动，Y破裂走滑位移增大	地层下掉幅度显著增大，形成窄而长的地堑	主位移带形成并贯穿褶皱长轴，切割R破裂

塔里木盆地F_Ⅰ17走滑断裂北段奥陶纪差异变形机制

Ordovician Differential Deformation Mechanism of Northern Section of F_Ⅰ17 Strike-Slip Fault, Tarim Basin

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塔里木盆地FⅠ17走滑断裂北段奥陶纪差异变形机制

Ordovician Differential Deformation Mechanism of Northern Section of FⅠ17 Strike-Slip Fault, Tarim Basin

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塔里木盆地F_Ⅰ17走滑断裂北段奥陶纪差异变形机制

Ordovician Differential Deformation Mechanism of Northern Section of F_Ⅰ17 Strike-Slip Fault, Tarim Basin