Volume 41 Issue 3
May  2022
Turn off MathJax
Article Contents
Wang Xiangdong, Wang Ren, Shi Wanzhong, Tang Daqing, Xu Litao, Feng Qian. Tectonic characteristics and evolution of typical rift basins in eastern China: A case study in the Gudian area, Songliao Basin[J]. Bulletin of Geological Science and Technology, 2022, 41(3): 85-95. doi: 10.19509/j.cnki.dzkq.2022.0089
Citation: Wang Xiangdong, Wang Ren, Shi Wanzhong, Tang Daqing, Xu Litao, Feng Qian. Tectonic characteristics and evolution of typical rift basins in eastern China: A case study in the Gudian area, Songliao Basin[J]. Bulletin of Geological Science and Technology, 2022, 41(3): 85-95. doi: 10.19509/j.cnki.dzkq.2022.0089

Tectonic characteristics and evolution of typical rift basins in eastern China: A case study in the Gudian area, Songliao Basin

doi: 10.19509/j.cnki.dzkq.2022.0089
  • Received Date: 06 Aug 2021
  • The Gudian Rift is a favorable area for deep natural gas exploration in the southern Songliao Basin, and it also records rich information on basin evolution and Mesozoic-Cenozoic plate movements in eastern China.By using the well and high-resolution 3D seismic data, combined with regional tectonics, the geological structure and tectonic evolution of the Gudian Rift were investigated.The results show that the Gudian Rift can be vertically divided into basement, lower, middle and upper structure layers.Due to the subduction of the Pacific Plate beneath to the East Asian Plate and the changes in the regional tectonic stress field since the Late Mesozoic, the Gudian Rift experienced syn-rift, transition, post rift and tectonic inversion periods.The Gudian fault was initially formed from six fault segments in syn rift period(depositional period of the Huoshiling and Shahezi Formations) and the isolated fault segments with different strikes then grew and connected to a unified boundary fault in the late rifting stage(depositional period of the Yingcheng Formation).Afterwards, extensive and intense transtensional activities occurred during transition(depositional period of the Denglouku and Quantou Formations) and depression periods(depositional period of the Qingshankou, Yaojia and Nenjiang Formations), and strong inversion and segmental thrust activities occurred during inversion period(end of the depositional period of the Nenjiang Formation), respectively.This study provides references for the investigation of tectonic activity and evolution in the Songliao Basin and eastern China, and further guides oil and gas exploration.

     

  • loading
  • [1]
    Athmer W, Luthi S M. The effect of relay ramps on sediment routes and deposition: A review[J]. Sedimentary Geology, 2011, 242(1/4): 1-17.
    [2]
    王任, 石万忠, 张先平, 等. 中国东部北黄海盆地东部坳陷岩浆活动特征及其与区域构造的耦合关系[J]. 地球科学, 2017, 42(4): 587-600. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201704008.htm

    Wang R, Shi W Z, Zhang X P, et al. Magmatic activity characteristics and its coupling relationship with regional tectonics in the eastern Depression of North Yellow Sea Basin, Eastern China[J]. Earth Science, 2017, 42(4): 587-600(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201704008.htm
    [3]
    肖丹, 石万忠, 王嘹亮, 等. 北黄海盆地东部M隆起构造特征及演化[J]. 海洋地质与第四纪地质, 2016, 36(5): 75-84. https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ201605010.htm

    Xiao D, Shi W Z, Wang L L, et al. Tectonic characteristics and evolution of the M uplift in the east area of North Yellow Sea[J]. Marine Geology & Quaternary Geology, 2016, 36(5): 75-84(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-HYDZ201605010.htm
    [4]
    张宝权, 张少阳, 尚卫忠, 等. 松辽盆地深层区域地质特征及有利勘探方向[J]. 石油地球物理勘探, 2006, 41(增刊1): 70-74. https://www.cnki.com.cn/Article/CJFDTOTAL-SYDQ2006S1015.htm

    Zhang B Q, Zhang S Y, Shang W Z, et al. Regional geologic feature and favorable exploration direction of deep beds in Songliao Basin[J]. Oil Geophysical Prospecting, 2006, 41(S1): 70-74(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-SYDQ2006S1015.htm
    [5]
    葛荣峰, 张庆龙, 王良书, 等. 松辽盆地构造演化与中国东部构造体制转换[J]. 地质论评, 2010, 56(2): 180-195. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP201002005.htm

    Ge R F, Zhang Q L, Wang L S, et al. Tectonic evolution ofSongliao Basin and the prominent tectonic regime transition in Eastern China[J]. Geological Review, 2010, 56(2): 180-195(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP201002005.htm
    [6]
    石万忠, 孟福林, 王晓龙, 等. 松辽盆地南部孤店断陷火石岭组烃源岩评价及预测[J]. 石油学报, 2018, 39(12): 1344-1354, 1388. doi: 10.7623/syxb201812003

    Shi W Z, Meng F L, Wang X L, et al. The evaluation and prediction of source rocks in Huoshiling Formation of Gudian Fault Depression, south of Songliao Basin[J]. Acta Petrolei Sinica, 2018, 39(12): 1344-1354, 1388(in Chinese with English abstract). doi: 10.7623/syxb201812003
    [7]
    Wang P, Mattern F, Didenko N A, et al. Tectonics and cycle system of the Cretaceous Songliao Basin: An inverted active continental margin basin[J]. Earth Science Reviews, 2016, 159: 82-102. doi: 10.1016/j.earscirev.2016.05.004
    [8]
    Li C, Liu S F. Cretaceous anomalous subsidence and its response to dynamic topography in the Songliao Basin, Northeast China[J]. Journal of Asian Earth Sciences, 2015, 109: 86-99. doi: 10.1016/j.jseaes.2015.04.045
    [9]
    胡望水, 吕炳全, 张文军, 等. 松辽盆地构造演化及成盆动力学探讨[J]. 地质科学, 2005, 40(1): 16-31. doi: 10.3321/j.issn:0563-5020.2005.01.002

    Hu W S, Lü B Q, Zhang W J, et al. An approach to tectonic evolution and dynamics of the Songliao Basin[J]. Chinese Journal of Geology, 2005, 40(1): 16-31(in Chinese with English abstract). doi: 10.3321/j.issn:0563-5020.2005.01.002
    [10]
    Jiang F, Cheng R, Ruan B, et al. Formation mechanism of volcanic reservoirs within a volcanostratigraphic framework: The case of the Wangfu fault depression in the Songliao Basin, China[J]. Marine and Petroleum Geology, 2017, 84: 160-178. doi: 10.1016/j.marpetgeo.2017.03.036
    [11]
    陈为佳, 何登发, 桂宝玲, 等. 松南地区构造-地层层序与盆地演化[J]. 地质学报, 2014, 88(5): 932-942. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201405010.htm

    Chen W J, He D F, Gui B L, et al. Tectono-stratigraphic sequence and basin evolution in Southern Songliao Basin[J]. Acta Geologica Sinica, 2014, 88(5): 932-942(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE201405010.htm
    [12]
    杨立英, 李瑞磊, 张江涛, 等. 松辽盆地南部十屋断陷构造特征研究[J]. 地球物理学进展, 2005, 20(3): 775-779. doi: 10.3969/j.issn.1004-2903.2005.03.032

    Yang L Y, Li R L, Zhang J T, et al. Study of structure character with seismic data in Shiwu Fault Depression in south of Songliao Basin[J]. Progress in Geophysics, 2005, 20(3): 775-779(in Chinese with English abstract). doi: 10.3969/j.issn.1004-2903.2005.03.032
    [13]
    李易隆, 贾爱林, 何东博, 等. 松辽盆地长岭断陷早白垩世断坳转换期沉积体系特征与演化过程[J]. 天然气地球科学, 2014, 25(5): 709-720. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX201405010.htm

    Li Y L, Jia A L, He D B, et al. Early Cretaceous sedimentary systems and depositional process during the period of transition from faulted depression to sag, Changling Faulted Depression, Songliao Basin[J]. Natural Gas Geoscience, 2014, 25(5): 709-720(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX201405010.htm
    [14]
    单敬福, 葛黛薇, 乐江华, 等. 松辽盆地东南缘层序地层与沉积体系配置及演化: 以梨树断陷西北部营城组地层为例[J]. 沉积学报, 2013, 31(1): 67-76. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201301009.htm

    Shan J F, Ge D W, Le J H, et al. Framework of sequence stratigraphy, sedimentary system and Evolution of southeastern Songliao Basin: An example from Yingcheng Formation in Lishu Fault Depression[J]. Acta Sedimentologica Sinica, 2013, 31(1): 67-76(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201301009.htm
    [15]
    曹民强. 松辽盆地钱家店铀矿含铀岩系层序地层结构对铀成矿的约束[J]. 地质科技通报, 2021, 40(4): 131-142. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ202104012.htm

    Cao M Q. Constraints of the sequence stratigraphic structure of uranium-bearing series on mineralization in Qianjiadian uranium deposit, Songliao Basin[J]. Bulletin of Geological Science and Technology, 2021, 40(4): 131-142. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ202104012.htm
    [16]
    Wang R, Shi W Z, Xie X, et al. Boundary fault linkage and its effect on Upper Jurassic to Lower Cretaceous sedimentation in the Gudian half-graben, Songliao Basin, northeastern China[J]. Marine and Petroleum Geology, 2018, 98, 33-49. doi: 10.1016/j.marpetgeo.2018.08.007
    [17]
    付宪弟, 马世忠, 孙雨, 等. 松辽盆地南部孤店断层活动性分析及其控藏作用[J]. 东北石油大学学报, 2010, 34(2): 21-25. doi: 10.3969/j.issn.2095-4107.2010.02.005

    Fu X D, Ma S Z, Sun Y, et al. Analysis of the activity and its role in controlling reservoir accumulation of Gudian fault of southern Songliao Basin[J]. Journal of Northeast Petroleum University, 2010, 34(2): 21-25(in Chinese with English abstract). doi: 10.3969/j.issn.2095-4107.2010.02.005
    [18]
    程璇, 徐尚, 郝芳, 等. 松辽盆地嫩江组富有机质页岩有机孔隙成因[J]. 地质科技情报, 2019, 38(4): 62-69. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201904008.htm

    Cheng X, Xu S, Hao F, et al. Origin of organic pores in the organic rich shale of Nenjiang Formation, Songliao Basin, China[J]. Bulletin of Geological Science and Technology, 2019, 38(4): 62-69(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201904008.htm
    [19]
    Wang P, Xie X, Mattern F. The Cretaceous Songliao Basin: Volcanogenic succession, sedimentary sequence and tectonic evolution, NE China[J]. Acta Geologica Sinica, 2007, 81(6): 1002-1011. doi: 10.1111/j.1755-6724.2007.tb01022.x
    [20]
    王璞珺, 赵然磊, 蒙启安, 等. 白垩纪松辽盆地: 从火山裂谷到陆内拗陷的动力学环境[J]. 地学前缘, 2015, 22(3): 99-117. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201503011.htm

    Wang P J, Zhao R L, Meng Q A, et al. The Cretaceous Songliao Basin: Dynamic background from volcanic rift to interior sag basin[J]. Earth Science Frontiers, 2015, 22(3): 99-117(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201503011.htm
    [21]
    Song Y, Ren J, Stepashko A A, et al. Post-rift geodynamics of the Songliao Basin, NE China: Origin and significance of T11(Coniacian) unconformity[J]. Tectonophysics, 2014, 634: 1-18. doi: 10.1016/j.tecto.2014.07.023
    [22]
    Walsh J J, Nicol A, Childs C. An alternative model for the growth of faults[J]. Journal of Structural Geology, 2002, 24(11): 1669-1675. doi: 10.1016/S0191-8141(01)00165-1
    [23]
    Soliva R, Benedicto A, Schultz R A, et al. Displacement and interaction of normal fault segments branched at depth: Implications for fault growth and potential earthquake rupture size[J]. Journal of Structural Geology, 2008, 30(10): 1288-1299. doi: 10.1016/j.jsg.2008.07.005
    [24]
    Fossen H, Rotevatn A. Fault linkage and relay structures in extensional settings: A review[J]. Earth-Science Reviews, 2016, 154: 14-28. doi: 10.1016/j.earscirev.2015.11.014
    [25]
    Yang M, Li L, Zhou J, et al. Segmentation and inversion of the Hangjinqi fault zone, the northern Ordos basin(North China)[J]. Journal of Asian Earth Sciences, 2013, 70/71(1): 64-78.
    [26]
    Xu Q, Shi W, Xie X, et al. Inversion and propagation of the late Paleozoic Porjianghaizi fault(North Ordos Basin, China): Controls on sedimentation and gas accumulations[J]. Marine and Petroleum Geology, 2018, 91: 706-722. doi: 10.1016/j.marpetgeo.2018.02.003
    [27]
    刘凯, 石万忠, 王任, 等. 鄂尔多斯盆地杭锦旗地区盒1段致密砂岩孔隙结构分形特征及其与储层物性的关系[J]. 地质科技通报, 2021, 40(1): 57-68. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ202101006.htm

    Liu K, Shi W Z, Wang R, et al. Pore structure fractal characteristics and its relationship with reservoir properties of the first Member of Lower Shihezi Formation tight sandstone in Hangjinqi area, Ordos Basin[J]. Bulletin of Geological Science and Technology, 2021, 40(1): 57-68 (in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ202101006.htm
    [28]
    张军龙, 蒙启安, 张长厚, 等. 松辽盆地徐家围子断陷边界断裂生长过程的定量分析[J]. 地学前缘, 2009, 16(4): 87-96. doi: 10.3321/j.issn:1005-2321.2009.04.009

    Zhang J L, Meng Q A, Zhang C H, et al. A quantitative study on the growth of boundary faults of the Xujiaweizi Faulting Depression in the Songliao Basin[J]. Earth Science Frontiers, 2009, 16(4): 87-96(in Chinese with English abstract). doi: 10.3321/j.issn:1005-2321.2009.04.009
    [29]
    Su J, Zhu W, Wei J, et al. Fault growth and linkage: Implications for tectonosedimentary evolution in the Chezhen Basin of Bohai Bay, eastern China[J]. AAPG Bulletin, 2011, 95(1): 1-26. doi: 10.1306/06301009207
    [30]
    王玺, 陈清华, 朱文斌, 等. 苏北盆地高邮凹陷边界断裂带构造特征及成因[J]. 大地构造与成矿学, 2013, 37(1): 20-28. doi: 10.3969/j.issn.1001-1552.2013.01.003

    Wang X, Chen Q H, Zhu W B, et al. Structural characteristics and origin of boundary fault belts of the Gaoyou Sag in the Subei Basin[J]. Geotectonica et Metallogenia, 2013, 37(1): 20-28(in Chinese with English abstract). doi: 10.3969/j.issn.1001-1552.2013.01.003
    [31]
    Morley C K. Evolution of large normal faults: Evidence from seismic reflection data[J]. AAPG Bulletin, 2002, 86(6): 961-978.
    [32]
    李君, 黄志龙, 李凌君, 等. 对松辽盆地南部东南隆起区抬升过程的新认识[J]. 新疆石油地质, 2008, 29(6): 690-692. https://www.cnki.com.cn/Article/CJFDTOTAL-XJSD200806007.htm

    Li J, Huang Z L, Li L J, et al. New understanding of uplifting process of Southeast Uplift area in Southern Songliao Basin[J]. Xinjiang Petroleum Geology, 2008, 29(6): 690-692(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-XJSD200806007.htm
    [33]
    陈娟, 张庆龙, 王良书, 等. 松辽盆地长岭断陷盆地断陷期构造转换及油气地质意义[J]. 地质学报, 2008, 82(8): 1027-1035. doi: 10.3321/j.issn:0001-5717.2008.08.002

    Chen J, Zhang Q L, Wang L S, et al. Tectonic transformation of Changling fault depression in the southern Songliao Basin and its significance of hydrocarbon accumulation[J]. Acta Geologica Sinica, 2008, 82(8): 1027-1035(in Chinese with English abstract). doi: 10.3321/j.issn:0001-5717.2008.08.002
    [34]
    Feng Z, Jia C, Xie X, et al. Tectono stratigraphic units and stratigraphic sequences of the nonmarine Songliao Basin, northeast China[J]. Basin Research, 2010, 22(1): 79-95. doi: 10.1111/j.1365-2117.2009.00445.x
    [35]
    Davis G A, Wang C, Zheng Y D, et al. The enigmatic Yinshan fold and thrust belt of northern China: New views on its intraplate contractional styles[J]. Geology, 1998, 26: 43-46.
    [36]
    Li S, Yang S, Wu C. Late Mesozoic rifting in Northeast China and Northeast Asia fault basin system[J]. Scientia Sinica, 1988, 31(2): 246-256.
    [37]
    Sun W, Ding X, Hu Y, et al. The golden transformation of the Cretaceous plate subduction in the west Pacific[J]. Earth and Planetary Science Letter, 2007, 262, 533-542. doi: 10.1016/j.epsl.2007.08.021
    [38]
    王亮, 赵红岩, 邱春光, 等. 东非裂谷Turkana坳陷新生代构造演化及动力学[J]. 地质科技通报, 2021, 40(5): 151-161. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ202105017.htm

    Wang L, Zhao H Y, Qiu C G, et al. Cenozoic tectonic evolution and dynamics of Turkana Depression, East African Rift[J]. Bulletin of Geological Science and Technology, 2021, 40(5): 151-161(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ202105017.htm
    [39]
    赵军, 唐贤君, 蒋一鸣, 等. 东海盆地西湖凹陷西北缘中始新世构造变革厘定及成因探讨[J]. 地质科技通报, 2020, 39(3): 58-67. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ202003010.htm

    Zhao J, Tang X J, Jiang Y M, et al. Confirmation and genesis of the Middle Eocene tectonic transformation in northwestern margin of Xihu Depression, East China Sea Basin[J]. Bulletin of Geological Science and Technology, 2020, 39(3): 58-67(in Chinese with English abstract). https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ202003010.htm
    [40]
    Didenko A N, Khanchuk A I, Tikhomirova A I, et al. Eastern segment of the kiselevka-manoma terrane(northern Sikhote alin): Paleomagnetism and geodynamic implications[J]. Russian Journal of Pacific Geology, 2014, 8: 18-37. doi: 10.1134/S1819714014010023
    [41]
    Liu S, Gurnis M, Ma P, et al. Reconstruction of northeast Asian deformation integrated with western Pacific plate subduction since 200 Ma[J]. Earth Science Reviews, 2017, 175: 114-142. doi: 10.1016/j.earscirev.2017.10.012
    [42]
    Wakita K. Geology and tectonics of Japanese islands: A review-the key to understanding the geology of Asia[J]. Journal of Asian Earth Science, 2013, 72: 75-87. doi: 10.1016/j.jseaes.2012.04.014
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索

    Article Metrics

    Article Views(67) PDF Downloads(28) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return