雷竞技app官方版下载ios-雷竞技官方平台
doi: 10.11781/sysydz202402342
1.
中国石化 石油勘探开发研究院, 北京 102206
2.
中国石化 深部地质与资源重点实验室, 北京 102206
3.
中国石化 河南油田分公司, 河南 南阳 473400
详细信息
中国石化 石油勘探开发研究院, 北京 102206
中国石化 深部地质与资源重点实验室, 北京 102206
中国石化 河南油田分公司, 河南 南阳 473400
Characteristics of Lower Paleozoic strike-slip faults and their significance for oil and gas exploration in Xunyi-Yijun area, Ordos Basin
1.
SINOPEC Petroleum Exploration and Production Research Institute, Beijing 102206, China
2.
Key Laboratory of Deep Geology and Resources, SINOPEC, Beijing 102206, China
3.
Henan Oilfield Company, SINOPEC, Nanyang, Henan 473400, China
SINOPEC Petroleum Exploration and Production Research Institute, Beijing 102206, China
Key Laboratory of Deep Geology and Resources, SINOPEC, Beijing 102206, China
Henan Oilfield Company, SINOPEC, Nanyang, Henan 473400, China
雷竞技官方平台:
近年来随着勘探和认识程度的加深，鄂尔多斯盆地不再被认为是“铁板”一块，盆地内多期多套断裂系统对油气成藏的控制作用越来越受重视。选取盆地南部旬邑—宜君(旬宜)地区，基于最新三维地震资料与钻井资料，应用走滑断裂理论模型，开展了断裂几何学与运动学分析，预测了断裂形成机制，并探讨了其对深层碳酸盐岩成储、成藏的控制作用。旬宜地区发育3套断裂系统，且存在深、浅层脱耦现象，下古生界走滑断裂在剖面上呈高陡直立、倾向摆动、“花”状构造等典型特征，平面上表现为“北西部挤压剪切、中部拉张剪切、主干断裂分段变形”。下古生界走滑断裂经历了两期构造活动，其中晚奥陶世至志留纪活动强度较大，为断层主要发育期，中—晚二叠世活动强度较弱，断层呈继承性走滑，形成北东、北西走向两组左行走滑断裂。鄂尔多斯盆地南部可能存在北东和北西向的基底薄弱带，加里东期Ⅱ幕洋盆俯冲闭合向盆内传递应力，斜向挤压导致旬宜地区基底断裂活化，是下古生界走滑断裂系统形成的主要动力机制。下古生界走滑断裂可有效改善深层碳酸盐岩储层物性，形成岩溶型或构造裂缝型优质储层，沿走滑断裂带形成“上生下储—旁生侧储”型成藏组合，是旬宜地区深层油气勘探值得关注的重点领域。
Abstract:
In recent years, the Ordos Basin has undergone a reevaluation, transitioning from a perception of a single block to a focus on understanding the influence of multiple stages and fault systems on hydrocarbon accumulation. This study utilizes the latest 3D seismic and drilling data alongside a theoretical model of strike-slip fault to analyze fault geometry and kinematics in the Xunyi-Yijun area of the basin's southern region. The mechanisms of fault formation are predicted and the related impacts on the formation and accumulation of deep carbonate rocks are also discussed. The results indicate the presence of three fault systems in the Xunyi-Yijun area, with decoupling between deep and shallow layers. The Lower Paleozoic strike-slip faults exhibit distinct characteristics, including high vertical structure, dip swing, and a "flower-shaped" structure in the section. The faults display "compression shear in the northwest, tension shear in the center, and segmental deformation on trunk fractures" on their planes.Moreover, the Lower Paleozoic strike-slip faults experienced two stages of tectonic activities with greater intensity observed from the Late Ordovician to the Silurian, marking the primary period of fault development. The activity intensity during the Middle to Late Permian was relatively weaker, with faults exhibiting inherited strike-slip characteristics. These faults formed two groups, one with a NE strike and the other with a NW strike. Additionally, during the second stage of the Caledonian period, ocean subduction and closure lead to stress being transferred to the basin interior. It is believed that the NE and NW strike basement weak zones existed in the southern Ordos Basin. As a result, the Lower Paleozoic strike-slip fault system likely formed due to the activation of oblique compression. This fault system has the potential to enhance the physical properties of deep carbonate reservoirs and create high-quality karst or tectonic fracture reservoirs in the Xunyi-Yijun area. Moreover, The formation of the "upper source and lower reservoir-lateral source and lateral reservoir" combination along the strike-slip fault belt is an area of interest for deep oil and gas exploration in the Xunyi-Yijun region.
图 1 鄂尔多斯盆地旬宜地区构造位置(a)与地层综合柱状图(b)
Figure 1. Structural location (a) and stratigraphic histogram (b) of Xunyi-Yijun area, Ordos Basin
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图 2 鄂尔多斯盆地旬宜地区典型地震解释剖面
剖面位置见图 1a。
Figure 2. Typical interpreted seismic section of Xunyi-Yijun area, Ordos Basin
图 3 鄂尔多斯盆地旬宜地区寒武系底界相干属性(a)和断裂分布(b)
Figure 3. Coherent attribute (a) and fault distribution (b) of bottom of Cambrian in Xunyi-Yijun area, Ordos Basin
图 4 鄂尔多斯盆地旬宜地区1号断裂带平面分段与典型剖面构造样式
断裂带位置见图 3。
Figure 4. Plane segments and structural styles of typical sections for No.1 fault belt in Xunyi-Yijun area, Ordos Basin
图 5 鄂尔多斯盆地旬宜地区2号断裂带平面分段与典型剖面构造样式
断裂带位置见图 3。
Figure 5. Plane segments and structural styles of typical sections for No. 2 fault belt in Xunyi-Yijun area, Ordos Basin
图 6 鄂尔多斯盆地旬宜地区2号走滑断裂带关键界面垂向断距统计
编号位置见图 5。
Figure 6. Plots of vertical separation at key interfaces along No.2 strike-slip fault belt in Xunyi-Yijun area, Ordos Basin
图 7 鄂尔多斯盆地旬宜地区走滑断裂运动学模式
a, b.里德尔剪切走滑模型；c.尾端马尾状收缩叠瓦扇模型；d.走滑叠接段应变模型。
Figure 7. Kinematic models of strike-slip faults in Xunyi-Yijun area, Ordos Basin
图 8 鄂尔多斯盆地旬宜地区下古生界走滑断裂形成机制示意
Figure 8. Formation mechanism of strike-slip faults in Lower Paleozoic, Xunyi-Yijun area, Ordos Basin
图 9 鄂尔多斯盆地旬宜地区马家沟组不同类型储层特征
a.XY2井，岩心，2 986.1 m，风化壳溶洞发育；b.XY1井，岩心，3 174.8 m，顺高角度裂缝向下发育溶蚀孔洞，方解石充填；c, d.XY1井，岩心，3 177.1 m，高角度裂缝发育，缝面方解石胶结；e.J1井，岩心，3 158.7 m，近垂直微裂缝发育，方解石半充填；f.J1井，单偏光铸体薄片，3 158.8 m, 中—细晶白云岩中裂缝发育，白云石半充填；g.XY1井，单偏光铸体薄片，3 179.9 m，含泥屑粉晶白云岩中微裂缝发育，沥青质半充填—未充填，裂缝间贯通性良好；h.XY2井，成像测井，2 986.5~2 989.2 m，可识别出高角度构造裂缝与溶蚀孔洞。
Figure 9. Characteristics of different types of reservoirs in Majiagou Formation, Xunyi-Yijun area, Ordos Basin
[1]
MANN P. Global catalogue, classification and tectonic origins of restraining- and releasing bends on active and ancient strike-slip fault systems[M]//CUNNINGHAM W D, MANN P. Tectonics of strike-slip restraining and releasing bends. McLean: Geological Society of London, 2007: 13-142.
[2]
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
[3]
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. doi: 10.3787/j.issn.1000-0976.2021.08.008JIA 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. doi: 10.3787/j.issn.1000-0976.2021.08.008
[4]
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. doi: 10.3969/j.issn.1672-7703.2021.04.005WANG 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. doi: 10.3969/j.issn.1672-7703.2021.04.005
[5]
马德波, 邬光辉, 朱永峰, 等. 塔里木盆地深层走滑断层分段特征及对油气富集的控制: 以塔北地区哈拉哈塘油田奥陶系走滑断层为例[J]. 地学前缘, 2019, 26(1): 225-237. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201901022.htmMA Debo, WU Guanghui, ZHU Yongfeng, et al. Segmentation characteristics of deep strike slip faults in the Tarim Basin and its control on hydrocarbon enrichment: taking the Ordovician strike slip fault in the Halahatang Oilfield in the Tabei area as an example[J]. Earth Science Frontiers, 2019, 26(1): 225-237. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201901022.htm
[6]
汪洋, 张哨楠, 刘永立. 塔里木盆地塔河油田走滑断裂活动对油气成藏的控制作用: 以托甫39断裂带为例[J]. 石油实验地质, 2022, 44(3): 394-401. doi: 10.11781/sysydz202203394WANG Yang, ZHANG Shaonan, LIU Yongli. Controls of strike-slip fault activities on hydrocarbon accumulation in Tahe Oilfield, Tarim Basin: a case study of TP 39 fault zone[J]. Petroleum Geology & Experiment, 2022, 44(3): 394-401. doi: 10.11781/sysydz202203394
[7]
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. doi: 10.3787/j.issn.1000-0976.2021.08.009JIAO 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. doi: 10.3787/j.issn.1000-0976.2021.08.009
[8]
管树巍, 梁瀚, 姜华, 等. 四川盆地中部主干走滑断裂带及伴生构造特征与演化[J]. 地学前缘, 2022, 29(6): 252-264. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY202206017.htmGUAN Shuwei, LIANG Han, JIANG Hua, et al. Characteristics and evolution of the main strike-slip fault belts of the central Sichuan Basin, southwestern China, and associated structures[J]. Earth Science Frontiers, 2022, 29(6): 252-264. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY202206017.htm
[9]
李海英, 韩俊, 陈平, 等. 塔里木盆地顺北4号走滑断裂带变形特征及有利区评价[J]. 新疆石油地质, 2023, 44(2): 127-135. https://www.cnki.com.cn/Article/CJFDTOTAL-XJSD202302001.htmLI Haiying, HAN Jun, C HEN Ping, et al. Deformation and favorable area evaluation of Shunbei No. 4 strike-slip fault zone in Tarim Basin[J]. Xinjiang Petroleum Geology, 2023, 44(2): 127-135. https://www.cnki.com.cn/Article/CJFDTOTAL-XJSD202302001.htm
[10]
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. https://www.cnki.com.cn/Article/CJFDTOTAL-XJSD202304010.htmLIU 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 Petroloeum Geology, 2023, 44(4): 456-464. https://www.cnki.com.cn/Article/CJFDTOTAL-XJSD202304010.htm
[11]
宋刚, 李海英, 叶宁, 等. 塔里木盆地顺托果勒低隆起顺北4号走滑断裂带成岩流体类型及活动特征[J]. 石油实验地质, 2022, 44(4): 603-612. doi: 10.11781/sysydz202204603SONG Gang, LI Haiying, YE Ning, et al. Types and features of diagenetic fluids in Shunbei No. 4 strike-slip fault zone in Shun-tuoguole Low Uplift, Tarim Basin[J]. Petroleum Geology & Experiment, 2022, 44(4): 603-612. doi: 10.11781/sysydz202204603
[12]
徐兴雨, 王伟锋, 陈谋. 鄂尔多斯盆地断裂特征及其石油地质意义[J]. 中国矿业大学学报, 2019, 48(4): 830-841. https://www.cnki.com.cn/Article/CJFDTOTAL-ZGKD201904016.htmXU Xingyu, WANG Weifeng, CHEN Mou. Characteristics of faults and their significance in hydrocarbon accumulation in Ordos Basin[J]. Journal of China University of Mining & Technology, 2019, 48(4): 830-841. https://www.cnki.com.cn/Article/CJFDTOTAL-ZGKD201904016.htm
[13]
魏国齐, 朱秋影, 杨威, 等. 鄂尔多斯盆地寒武纪断裂特征及其对沉积储集层的控制[J]. 石油勘探与开发, 2019, 46(5): 836-847. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK201905005.htmWEI Guoqi, ZHU Qiuying, YANG Wei, et al. Cambrian faults and their control on the sedimentation and reservoirs in the Ordos Basin, NW China[J]. Petroleum Exploration and Development, 2019, 46(5): 836-847. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK201905005.htm
[14]
齐荣. 鄂尔多斯盆地杭锦旗东部断裂特征及对天然气成藏的影响[J]. 特种油气藏, 2019, 26(4): 58-63. doi: 10.3969/j.issn.1006-6535.2019.04.010QI Rong. Fault characterization and its influences on gas accumulation in the eastern Haggin Banner of Ordos Basin[J]. Special Oil & Gas Reservoirs, 2019, 26(4): 58-63. doi: 10.3969/j.issn.1006-6535.2019.04.010
[15]
李潍莲, 纪文明, 刘震, 等. 鄂尔多斯盆地北部泊尔江海子断裂对上古生界天然气成藏的控制[J]. 现代地质, 2015, 29(3): 584-590. doi: 10.3969/j.issn.1000-8527.2015.03.010LI Weilian, JI Wenming, LIU Zhen, et al. Control of Boerjianghaizi fault on gas accumulation of Upper Paleozoic in northern Ordos Basin[J]. Geoscience, 2015, 29(3): 584-590. doi: 10.3969/j.issn.1000-8527.2015.03.010
[16]
胥旺, 邓虎成, 雷涛, 等. 鄂尔多斯盆地东北部大牛地气田马家沟组不同性质断裂对表生岩溶的控制作用[J]. 天然气地球科学, 2023, 34(3): 431-444. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202303005.htmXU Wang, DENG Hucheng, LEI Tao, et al. Control of different faults on supergene karst in the Majiagou Formation of Daniudi Gas Field, northeastern Ordos Basin[J]. Natural Gas Geoscience, 2023, 34(3): 431-444. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202303005.htm
[17]
杨丽华, 刘池洋, 代双和, 等. 鄂尔多斯盆地古峰庄地区断裂特征及油气地质意义[J]. 地球科学进展, 2021, 36(10): 1039-1051. doi: 10.11867/j.issn.1001-8166.2021.075YANG Lihua, LIU Chiyang, DAI Shuanghe, et al. Fault characteristics and petroleum geological significance in the Gufengzhuang area, Ordos Basin[J]. Advances in Earth Science, 2021, 36(10): 1039-1051. doi: 10.11867/j.issn.1001-8166.2021.075
[18]
刘永涛, 刘池洋, 赵俊峰, 等. 鄂尔多斯盆地西缘中部微小断层的成因机制与控藏特征[J]. 地质科学, 2018, 53(3): 922-940.LIU Yongtao, LIU Chiyang, ZHAO Junfeng, et al. Forming mechanism of small-scale faults and their control for the reservoir formation in the middle of western margin of the Ordos Basin[J]. Chinese Journal of Geology, 2018, 53(3): 922-940.
[19]
潘杰, 刘忠群, 蒲仁海, 等. 鄂尔多斯盆地镇原-泾川地区断层特征及控油意义[J]. 石油地球物理勘探, 2021, 52(2): 360-370. https://www.cnki.com.cn/Article/CJFDTOTAL-SYDQ201702021.htmPAN Jie, LIU Zhongqun, PU Renhai, et al. Fault characteristics and oil-controlling effects in Zhenyuan-Jingchuan district, southwestern Ordos Basin[J]. Oil Geophysical Prospecting, 2017, 52(2): 360-370. https://www.cnki.com.cn/Article/CJFDTOTAL-SYDQ201702021.htm
[20]
何发岐, 齐荣, 袁春艳, 等. 鄂尔多斯盆地南部地区断裂构造与油气成藏关系再认识: 以彬长地区为例[J/OL]. 地球科学, 2022: 1-18(2022-08-23). http://kns.cnki.net/kcms/detail/42.1874.P.20220822.1642.008.html .HE Faqi, QI Rong, YUAN Chunyan, et al. Further understanding of the relationship between fault characteristic and hydrocarbon accumulation in Binchang area, Ordos Basin[J/OL]. Earth Science, 2022: 1-18(2022-08-23). http://kns.cnki.net/kcms/detail/42.1874.P.20220822.1642.008.html .
[21]
王猛. 鄂尔多斯盆地镇原-泾川地区中生界断裂发育特征[J]. 断块油气田, 2019, 26(2): 142-146. https://www.cnki.com.cn/Article/CJFDTOTAL-DKYT201902003.htmWANG Meng. Mesozoic fracture development characteristics of Zhenyuan-Jingchuan area, Ordos Basin[J]. Fault-Block Oil and Gas Field, 2019, 26(2): 142-146. https://www.cnki.com.cn/Article/CJFDTOTAL-DKYT201902003.htm
[22]
何发岐, 梁承春, 陆骋, 等. 鄂尔多斯盆地南缘过渡带致密-低渗油藏断缝体的识别与描述[J]. 石油与天然气地质, 2020, 41(4): 710-718. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT202004006.htmHE Faqi, LIANG Chengchun, LU Cheng, et al. Identification and description of fault-fracture bodies in tight and low permeability reservoirs in transitional zone at the south margin of Ordos Basin[J]. Oil & Gas Geology, 2020, 41(4): 710-718. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT202004006.htm
[23]
肖正录, 路俊刚, 李勇, 等. 鄂尔多斯盆地延长组裂缝特征及其控藏作用[J]. 新疆石油地质, 2023, 44(5): 535-542. https://www.cnki.com.cn/Article/CJFDTOTAL-XJSD202305016.htmXIAO Zhenglu, LU Jungang, LI Yong, et al. Characteristics of fractures and their controls on Yanchang Formation reservoir in Ordos Basin[J]. Xinjiang Petroleum Geology, 2023, 44(5): 535-542. https://www.cnki.com.cn/Article/CJFDTOTAL-XJSD202305016.htm
[24]
李妍蓉, 李靖, 苏文杰, 等. 鄂尔多斯盆地伊陕斜坡太原组碳酸盐岩气藏富集规律[J]. 新疆石油地质, 2023, 44(5): 509-516. https://www.cnki.com.cn/Article/CJFDTOTAL-XJSD202305001.htmLI Yanrong, LI Jing, SU Wenjie, et al. Natural gas enrichment in carbonate gas reservoirs of Taiyuan Formation in Yishaan slope, Ordos Basin[J]. Xinjiang Petroleum Geology, 2023, 44(5): 509-516. https://www.cnki.com.cn/Article/CJFDTOTAL-XJSD202305001.htm
[25]
邓铭哲, 蔡芃睿, 陆建林, 等. 走滑断裂演化程度的表征参数研究[J]. 石油实验地质, 2023, 45(5): 1007-1015. doi: 10.11781/sysydz2023051007DENG Mingzhe, CAI Pengrui, LU Jianlin, et al. Characterization parameters of the evolution degree of strike-slip faults[J]. Petroleum Geology & Experiment, 2023, 45(5): 1007-1015. doi: 10.11781/sysydz2023051007
[26]
康玉柱, 王宗秀, 周新桂, 等. 鄂尔多斯盆地构造体系控油作用研究[M]. 北京: 地质出版社, 2014.KANG Yuzhu, WANG Zongxiu, ZHOU Xingui, et al. Study on oil control of tectonic system in Ordos Basin[M]. Beijing: Geology Press, 2014.
[27]
何自新. 鄂尔多斯盆地演化与油气[M]. 北京: 石油工业出版社, 2003.HE Zixin. Evolution and petroleum in Ordos Basin[M]. Beijing: Petroleum Industry Press, 2003.
[28]
何登发, 包洪平, 开百泽, 等. 鄂尔多斯盆地及其邻区关键构造变革期次及其特征[J]. 石油学报, 2021, 42(10): 1255-1269. doi: 10.7623/syxb202110001HE Dengfa, BAO Hongping, KAI Baize, et al. Critical tectonic modification periods and its geologic features of Ordos Basin and adjacent area[J]. Acta Petrolei Sinica, 2021, 42(10): 1255-1269. doi: 10.7623/syxb202110001
[29]
赵振宇, 郭彦如, 王艳, 等. 鄂尔多斯盆地构造演化及古地理特征研究进展[J]. 特种油气藏, 2012, 19(5): 15-20. doi: 10.3969/j.issn.1006-6535.2012.05.004ZHAO Zhenyu, GUO Yanru, WANG Yan, et al. Study progress in tectonic evolution and paleogeography of Ordos Basin[J]. Special Oil & Gas Reservoirs, 2012, 19(5): 15-20. doi: 10.3969/j.issn.1006-6535.2012.05.004
[30]
卢子兴, 董国栋, 裴文超, 等. 致密碳酸盐岩储层微观结构特征及发育影响因素: 以鄂尔多斯盆地东部马五1+2亚段为例[J]. 断块油气田, 2023, 30(3): 372-380, 388. https://www.cnki.com.cn/Article/CJFDTOTAL-DKYT202303003.htmLU Zixing, DONG Guodong, PEI Wenchao, et al. Microstructure characteristics and development influencing factors of tight carbonate reservoirs: a case study of the Ma 51+2 sub-member in eastern Ordos Basin[J]. Fault-Block Oil and Gas Field, 2023, 30(3): 372-380, 388. https://www.cnki.com.cn/Article/CJFDTOTAL-DKYT202303003.htm
[31]
邓尚, 李慧莉, 韩俊, 等. 塔里木盆地顺北5号走滑断裂中段活动特征及其地质意义[J]. 石油与天然气地质, 2019, 40(5): 990-998. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201905004.htmDENG Shang, LI Huili, HAN Jun, et al. Characteristics of the central segment of Shunbei 5 strike-slip fault zone in Tarim Basin and its geological significance[J]. Oil & Gas Geology, 2019, 40(5): 990-998. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT201905004.htm
[32]
黄雷, 刘池洋, 何发岐, 等. 克拉通盆地内断裂走滑变形特征[J]. 西北大学学报(自然科学版), 2022, 52(6): 930-942. https://www.cnki.com.cn/Article/CJFDTOTAL-XBDZ202206003.htmHUANG Lei, LIU Chiyang, HE Faqi, et al. strike-slip deformation characteristics of fault in craton basin[J]. Journal of Northwest University (Natural Science Edition), 2022, 52(6): 930-942. https://www.cnki.com.cn/Article/CJFDTOTAL-XBDZ202206003.htm
[33]
王建强, 刘池洋, 闫建萍, 等. 鄂尔多斯盆地南部渭北隆起发育时限及其演化[J]. 兰州大学学报(自然科学版), 2010, 46(4): 22-29. https://www.cnki.com.cn/Article/CJFDTOTAL-LDZK201004006.htmWANG Jianqiang, LIU Chiyang, YAN Jianping, et al. Development time and evolution characteristics of Weibei Uplift in the south of Ordos Basin[J]. Journal of Lanzhou University (Natural Sciences), 2010, 46(4): 22-29. https://www.cnki.com.cn/Article/CJFDTOTAL-LDZK201004006.htm
[34]
况安鹏, 余一欣, 朱秀香, 等. 塔里木盆地顺北地区11号走滑断裂带变形及其活动特征[J]. 现代地质, 2021, 35(6): 1809-1817. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ202106026.htmKUANG Anpeng, YU Yixin, ZHU Xiuxiang, et al. Deformation and activity characteristics of the No. 11 strike-slip fault zone in the Shunbei area, Tarim Basin[J]. Geoscience, 2021, 35(6): 1809-1817. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ202106026.htm
[35]
邓尚, 刘雨晴, 刘军, 等. 克拉通盆地内部走滑断裂发育、演化特征及其石油地质意义: 以塔里木盆地顺北地区为例[J]. 大地构造与成矿学, 2021, 45(6): 1111-1126. https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK202106003.htmDENG Shang, LIU Yuqing, LIU Jun, et al. Structural styles and evolution models of intracratonic strike-slip faults and the implications for reservoir exploration and appraisal: a case study of the Shunbei area, Tarim Basin[J]. Geotectonica et Metallogenia, 2021, 45(6): 1111-1126. https://www.cnki.com.cn/Article/CJFDTOTAL-DGYK202106003.htm
[36]
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
[37]
DOOLEY T P, SCHREURS G. Analogue modelling of intraplate strike-slip tectonics: a review and new experimental results[J]. Tectonophysics, 2012, 574-575: 1-71. doi: 10.1016/j.tecto.2012.05.030
[38]
周永胜, 李建国, 王绳祖. 用物理模拟实验研究走滑断裂和拉分盆地[J]. 地质力学学报, 2003, 9(1): 1-13. doi: 10.3969/j.issn.1006-6616.2003.01.001ZHOU Yongsheng, LI Jianguo, WANG Shengzu, et al. Physical experiments on strike-slip fault and pull-apart basin[J]. Journal of Geomechanics, 2003, 9(1): 1-13. doi: 10.3969/j.issn.1006-6616.2003.01.001
[39]
宋鸿林, 张长厚, 王根厚. 构造地质学[M]. 北京: 地质出版社, 2013.SONG Honglin, ZHANG Changhou, WANG Genhou. Structural geology[M]. Beijing: Geology Press, 2013.
[40]
QIU Huabiao, DENG Shang, 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(6): 2087-2113. doi: 10.1029/2018TC005229
[41]
李国会, 李世银, 李会元, 等. 塔里木盆地中部走滑断裂系统分布格局及其成因[J]. 天然气工业, 2021, 41(3): 30-37. doi: 10.3787/j.issn.1000-0976.2021.03.004LI Guohui, LI Shiyin, LI Huiyuan, et al. Distribution pattern and formation mechanism of the strike-slip fault system in the central Tarim Basin[J]. Natural Gas Industry, 2021, 41(3): 30-37. doi: 10.3787/j.issn.1000-0976.2021.03.004
[42]
张仲培, 徐勤琪, 刘士林, 等. 塔里木盆地巴麦地区东段北东向走滑断裂体系特征及油气地质意义[J]. 石油实验地质, 2023, 45(4): 761-769. doi: 10.11781/sysydz202304761ZHANG Zhongpei, XU Qinqi, LIU Shilin, et al. Characteristics of NE strike-slip fault system in the eastern section of Bachu-Maigaiti area, Tarim Basin and its oil-gas geological significance[J]. Petroleum Geology & Experiment, 2023, 45(4): 761-769. doi: 10.11781/sysydz202304761
[43]
刘雨晴, 邓尚, 张继标, 等. 塔里木盆地顺北及邻区走滑断裂体系差异发育特征及成因机制探讨[J]. 地学前缘, 2023, 30(6): 95-109. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY202306008.htmLIU Yuqing, DENG Shang, ZHANG Jibiao, et al. Characteristics and formation mechanism of the strike-slip fault networks in the Shunbei area and the surroundings, Tarim Basin[J]. Earth Science Frontiers, 2023, 30(6): 95-109. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY202306008.htm
[44]
李明, 闫磊, 韩绍阳. 鄂尔多斯盆地基底构造特征[J]. 吉林大学学报(地球科学版), 2012, 42(S3): 38-43. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ2012S3006.htmLI Ming, YAN Lei, HAN Shaoyang. The basement tectonic characteristics in Ordos Basin[J]. Journal of Jilin University (Earth Science Edition), 2012, 42(S3): 38-43. https://www.cnki.com.cn/Article/CJFDTOTAL-CCDZ2012S3006.htm
[45]
田刚, 杨明慧, 宋立军, 等. 鄂尔多斯盆地基底结构特征及演化过程新认识[J]. 地球学报, 2024, 49(1): 123-139. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX202401008.htmTIAN Gang, YANG Minghui, SONG Lijun, et al. New understanding of basement structural characteristics and its evolution process in Ordos Basin[J]. Earth Science, 2024, 49(1): 123-139. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX202401008.htm
[46]
冯志强, 李萌, 郭元岭, 等. 中国典型大型走滑断裂及相关盆地成因研究[J]. 地学前缘, 2022, 29(6): 206-223. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY202206014.htmFENG Zhiqiang, LI Meng, GUO Yuanling, et al. Genetic analysis of typical strike-slip faults and related basins in China[J]. Earth Science Frontiers, 2022, 29(6): 206-223. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY202206014.htm
[47]
车自成, 罗金海, 刘良. 中国及邻区区域大地构造学[M]. 北京: 科学出版社, 2016.CHE Zicheng, LUO Jinhai, LIU Liang. Regional tectonics of China and adjacent regions[M]. Beijing: Science Press, 2016.
[48]
万天丰. 中国大地构造学[M]. 北京: 地质出版社, 2011.WAN Tianfeng. Geotectonics of China[M]. Beijing: Geology Press, 2011.
[49]
王洪亮, 徐学义, 陈隽璐, 等. 北秦岭西段岩湾加里东期碰撞型侵入体形成时代及地球化学特征[J]. 地质学报, 2009, 83(3): 353-364. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200903005.htmWANG Hongliang, XU Xueyi, CHEN Juanlu, et al. Dating and geochemical characteristics of the Yanwan Paleozoic collisional intrusion in the west segment of northern Qinling Mts[J]. Acta Geologica Sinica, 2009, 83(3): 353-364. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE200903005.htm
[50]
王涛, 王晓霞, 田伟, 等. 北秦岭古生代花岗岩组合、岩浆时空演变及其对造山作用的启示[J]. 中国科学(D辑: 地球科学), 2009, 39(7): 949-971. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200907008.htmWANG Tao, WANG Xiaoxia, TIAN Wei, et al. North Qinling Paleozoic granite associations and their variation in space and time: implications for orogenic processes in the orogens of central China[J]. Science in China (Series D: Earth Sciences), 2009, 52(9): 1359-1384. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200907008.htm
[51]
DONG Yunpeng, ZHANG Guowei, NEUBAUER F, et al. Tectonic evolution of the Qinling orogen, China: review and synthesis[J]. Journal of Asian Earth Sciences, 2011, 41(3): 213-237. doi: 10.1016/j.jseaes.2011.03.002
[52]
何发岐, 王付斌, 郭利果, 等. 鄂尔多斯盆地古生代原型盆地演化与构造沉积格局变迁[J]. 石油实验地质, 2022, 44(3): 373-384. doi: 10.11781/sysydz202203373HE Faqi, WANG Fubin, GUO Liguo, et al. Evolution of prototype basin and change of tectonic-sedimentary pattern in Paleozoic, Ordos Basin[J]. Petroleum Geology & Experiment, 2022, 44(3): 373-384. doi: 10.11781/sysydz202203373
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