Tectonic analysis of the eastern boundary of Ordos Basin: a case study of northern region of Shilou area
SHI Jing1, HE Dengfa1, BAO Hongping2, WEI Liubin2
1 School of Energy Resources,China University of Geosciences(Beijing),Beijing 100083, China; 2 Exploration and Development Research Institute of Changqing Oil Field Branch, PetroChina, Xi'an 710018, China
Abstract:The boundary belt of the eastern margin of Ordos Basin is believed to be composed of the Jinxi flexural fold belt and Lishi fault,but this boundary is a residual boundary and not the original sedimentary boundary. Taking the northern region of Shillou as an example,a regional geological profile was constructed at the basin-mountain scale in the eastern part of the Ordos Basin. The 2D-Move software was used for inversion and forward simulation of tectonic evolution,and quantitative analysis of structural deformation was conducted. Based on theseresults,the eastern boundary of the Ordos Basin was redefined. (1)In the late Caledonian period,the northern part of the Shiliouarea was affected by deep basement fault activity,and salt detachment folds were formed in the Ordovician gypsum salt rock layers,followed by the deposition of the Carboniferous,Permian,Triassic,Jurassic and Cretaceous systems. During the Yanshanian,the strata were subjected to E-W compressive stress,causing the overall strata to tilt. In the Cenozoic Lvliang uplift,they accelerated and underwent differential weathering and erosion,forming the present tectonic pattern. (2)The present length of the regional geological profile is 263.76 km,with an altitude of up to 2000 m. The shortening of strata from the late Caledonian to the Cretaceous sedimentary period is 3.14 km,with a shortening rate of 1.18%. The elevation of the formation uplift is 3.82 km. (3)Based on the characteristics of stratigraphy,structure,and evolution,the eastern boundary of the Ordos Basin during the Yanshan Movement is redefined,and it is believed that the eastern boundary should extend easternward to the east side of Lvliang Uplift. This paper can provide a reference and new ideas for studying the eastern margin of the Ordos Basin,structural deformation,and coalbed methane exploration and development in the western Shanxi flexural fold belt.
SHI Jing,HE Dengfa,BAO Hongping et al. Tectonic analysis of the eastern boundary of Ordos Basin: a case study of northern region of Shilou area[J]. JOPC, 2024, 26(1): 150-164.
[1] 蔡益栋,高国森,刘大锰,邱峰. 2022. 鄂尔多斯盆地东缘临兴中区煤系气富集地质条件及成藏模式. 天然气工业, 42(11): 25-36. [Cai Y D,Gao G S,Liu D M,Qiu F.2022. Geological conditions for coal measure gas enrichment and accumulation models in Linxingzhong Block along the eastern margin of the Ordos Basin. Natural Gas Industry, 42(11): 25-36] [2] 陈晨,王克. 2022. 鄂尔多斯盆地东缘煤层气储层物性特征规律研究. 中外能源, 27(4): 15-21. [Chen C,Wang K.2022. Study on physical characteristics of coalbed methane reservoirs in eastern margin of Ordos Basin. Sino-Global Energy, 27(4): 15-21] [3] 陈世悦. 1998. 论秦岭碰撞造山作用对华北石炭二叠纪海侵过程的控制. 岩相古地理, 18(2): 48-54. [Chen S Y.1998. The controls of the collisional orogenesis in the Qinling Mountains on the Carboniferous-Permian transgressional processes in North China. Sedimentary Facies and Palaeogeography, 18(2): 48-54] [4] 程守田,黄焱球,付雪洪. 1997. 早中侏罗世大鄂尔多斯古地理重建与内陆拗陷的发育演化. 沉积学报, 15(4): 43-49. [Cheng S T,Huang Y Q,Fu X H.1997. Paleogeography reconstruction of the Early-Middle Jurassic Large Ordos Basin and development and evolution of continental downwarping. Acta Sedimentologica Sinica, 15(4): 43-49] [5] 董树文,张岳桥,龙长兴,杨振宇,季强,王涛,胡建民,陈宣华. 2007. 中国侏罗纪构造变革与燕山运动新诠释. 地质学报, 81(11): 1449-1461. [Dong S W,Zhang Y Q,Long C X,Yang Z Y,Ji Q,Wang T,Hu J M,Chen X H.2007. Jurassic tectonic revolution in China and new interpretation of the Yanshan movement. Acta Geologica Sinica, 81(11): 1449-1461] [6] 郭艳琴,李文厚,郭彬程,张倩,陈强,王若谷,刘溪,马瑶,李智超,张梦婷,李百强. 2019. 鄂尔多斯盆地沉积体系与古地理演化. 古地理学报, 21(2): 293-320. [Guo Y Q,Li W H,Guo B C,Zhang Q,Chen Q,Wang R G,Liu X,Ma Y,Li Z C,Zhang M T,Li B Q.2019. Sedimentary systems and palaeogeography evolution of Ordos Basin. Journal of Palaeogeography(Chinese Edition), 21(2): 293-320] [7] 胡波,翟明国,彭澎,刘富,第五春荣,王浩铮,张海东. 2013. 华北克拉通古元古代末—新元古代地质事件: 来自北京西山地区寒武系和侏罗系碎屑锆石LA-ICP-MS U-Pb年代学的证据. 岩石学报, 29(7): 2508-2536. [Hu B,Zhai M G,Peng P,Liu F,Diwu C R,Wang H Z,Zhang H D.2013. Late Paleoproterozoic to Neoproterozoic geological events of the North China Craton: evidence from LA-ICP-MS U-Pb geochronology of detrital zircons from the Cambrian and Jurassic sedimentary rocks in Western Hills of Beijing. Acta Petrologica Sinica, 29(7): 2508-2536] [8] 李文厚,庞军刚,曹红霞,肖丽,王若谷. 2009. 鄂尔多斯盆地晚三叠世延长期沉积体系及岩相古地理演化. 西北大学学报(自然科学版), 39(3): 501-506. [Li W H,Pang J G,Cao H X,Xiao L,Wang R G.2009. Depositional system and paleogeographic evolution of the late Triassic Yanchang Stage in Ordos Basin. Journal of Northwest University(Natural Science Edition), 39(3): 501-506] [9] 李文厚,张倩,李克永,陈强,郭艳琴,马瑶,冯娟萍,张道锋. 2021. 鄂尔多斯盆地及周缘地区晚古生代沉积演化. 古地理学报, 23(1): 39-52. [Li W H,Zhang Q,Li K Y,Chen Q,Guo Y Q,Ma Y,Feng J P,Zhang D F.2021. Sedimentary evolution of the late Paleozoic in Ordos Basin and its adjacent areas. Journal of Palaeogeography(Chinese Edition), 23(1): 39-52] [10] 廖昌珍,张岳桥,温长顺. 2007. 鄂尔多斯盆地东缘边界带构造样式及其区域构造意义. 地质学报, 81(4): 466-475. [Liao C Z,Zhang Y Q,Wen C S.2007. Structural styles of the eastern boundary zone of the Ordos Basin and its regional tectonic significance. Acta Geologica Sinica, 81(4): 466-475] [11] 刘绍龙. 1986. 华北地区大型三叠纪原始沉积盆地的存在. 地质学报, 60(2): 128-138. [Liu S L.1986. The existence of a large-scale Triassic sedimentary basin in North China. Acta Geologica Sinica, 60(2): 128-138] [12] 彭思钟,刘德勋,张磊夫,邱振,王以城,封从军,孙萌思. 2022. 鄂尔多斯盆地东缘大宁—吉县地区山西组页岩岩相与沉积相特征. 沉积学报, 40(1): 47-59. [Peng S Z,Liu D X,Zhang L F,Qiu Z,Wang Y C,Feng C J,Sun M S.2022. Shale lithofacies and sedimentary facies of the Permian Shanxi Formation,Daning-Jixian area,eastern margin of Ordos Basin. Acta Sedimentologica Sinica, 40(1): 47-59] [13] 山西省地质矿产局. 1989. 山西省区域地质志. 北京: 地质出版社,1-789. [Shanxi Bureau of Geology and Mineral Resources. 1989. Regional Geology of Shanxi Province. Beijing: Geological Publishing House,1-789] [14] 尚景武. 2020. 鄂尔多斯盆地构造演化历程. 产业与科技论坛, 19(7): 46-47. [Shang J W.2020. Tectonic evolution of Ordos Basin. Industrial & Science Tribune, 19(7): 46-47] [15] 孙越,蒋裕强,熊先钺,李星涛,李树新,邱振,孙雄伟. 2022. 鄂尔多斯盆地东缘大宁—吉县地区山西组亚段海陆过渡相页岩岩相与沉积环境变化. 煤田地质与勘探, 50(9): 104-114. [Sun Y,Jiang Y Q,Xiong X Y,Li X T,Li S X,Qiu Z,Sun X W.2022. Lithofacies and sedimentary environment evolution of the Shan23 Sub-member transitional shale of the Shanxi Formation in the Daning-Jixian area,eastern Ordos Basin. Coal Geology & Exploration, 50(9): 104-114] [16] 王成旺,徐凤银,甄怀宾,陈高杰,甯波,曹铮,陈岑. 2022. 鄂尔多斯盆地东缘本溪组8#煤层方解石脉体成因. 特种油气藏, 29(4): 62-68. [Wang C W,Xu F Y,Zhen H B,Chen G J,Ning B,Cao Z,Chen C.2022. Genesis of calcite veins in 8# coal bed of Benxi Formation on eastern margin of Ordos Basin. Special Oil & Gas Reservoirs, 29(4): 62-68] [17] 王猛,呼婧,冯钊,韩建伟,贾方方,余亮,邓明,刘亚辉. 2019. 鄂尔多斯盆地早古生代构造演化特征分析. 辽宁化工, 48(6): 577-579. [Wang M,Hu J,Feng Z,Han J W,Jia F F,Yu L,Deng M,Liu Y H.2019. Analysis on structural evolution characteristics of Early Paleozoic Ordos Basin. Liaoning Chemical Industry, 48(6): 577-579] [18] 王双明. 2011. 鄂尔多斯盆地构造演化和构造控煤作用. 地质通报, 30(4): 544-552. [Wang S M.2011. Ordos Basin tectonic evolution and structural control of coal. Geological Bulletin of China, 30(4): 544-552] [19] 王锡勇,张庆龙,王良书,葛荣峰,陈娟. 2010. 鄂尔多斯盆地东缘中—新生代构造特征及构造应力场分析. 地质通报, 29(8): 1168-1176. [Wang X Y,Zhang Q L,Wang L S,Ge R F,Chen J.2010. Structural features and tectonic stress fields of the Mesozoic and Cenozoic in the eastern margin of the Ordos Basin,China. Geological Bulletin of China, 29(8): 1168-1176] [20] 王雪莲,王长陆,陈振林,田继军. 2005. 鄂尔多斯盆地奥陶系风化壳岩溶储层研究. 特种油气藏, 12(3): 32-35. [Wang X L,Wang C L,Chen Z L,Tian J J.2005. Study of Ordovician weathering crust karst reservoirs in Ordos Basin. Special Oil and Gas Reservoirs, 12(3): 32-35] [21] 王以城,张磊夫,邱振,彭思钟,封从军,孙萌思. 2022. 鄂尔多斯盆地东缘二叠系山n23亚段海陆过渡相页岩岩相类型与储层发育特征. 天然气地球科学, 33(3): 418-430. [Wang Y C,Zhang L F,Qiu Z,Peng S Z,Feng C J,Sun M S.2022. Lithofacies types and reservoir characteristics of transitional shales of the Permian Shan23 sub-member,eastern Ordos Basin. Natural Gas Geoscience, 33(3): 418-430] [22] 武洪涛,孙妹娴. 2019. 鄂尔多斯盆地构造演化浅述. 科技资讯, 17(7): 78-79,81. [Wu H T,Sun M X.2019. A brief description of the tectonic evolution of the Ordos Basin. Science & Technology Information, 17(7): 78-79,81] [23] 肖玲玲,牛路伟,王国栋. 2021. 吕梁界河口群变质岩石的构造指示: 来自地球化学和同位素年代学的证据. 岩石学报, 37(4): 1015-1043. [Xiao L L,Niu L W,Wang G D.2021. Geochemistry,geochronology and its geological implication of metamorphic rocks of the Jiehekou Group in the Lüliang Complex. Acta Petrologica Sinica, 37(4): 1015-1043] [24] 徐立富,邓纪梅,杜佳,李勇,吴鹏,吴翔,胡维强,赵霏,郑薇,江智勋. 2021. 鄂尔多斯盆地东缘临兴地区海陆过渡相页岩岩相类型和储层差异. 煤炭学报,46(S2): 862-876. [Xu L F,Deng J M,Du J,Li Y,Wu P,Wu X,Hu W Q,Zhao F,Zheng W,Jiang Z X.2021. Lithofacies types and reservoir differences of marine continental transitional shale in Linxing area,eastern margin of Ordos Basin. Journal of China Coal Society,46(S2): 862-876] [25] 杨华,刘新社,闫小雄. 2015. 鄂尔多斯盆地晚古生代以来构造-沉积演化与致密砂岩气成藏. 地学前缘, 22(3): 174-183. [Yang H,Liu X S,Yan X X.2015. The relationship between tectonic-sedimentary evolution and tight sandstone gas reservoir since the late Paleozoic in Ordos Basin. Earth Science Frontiers, 22(3): 174-183] [26] 杨俊杰. 2002. 鄂尔多斯盆地构造演化与油气分布规律. 北京: 石油工业出版社,1-228. [Yang J J.2002. Tectonic Evolution and Oil-gas Reservoirs Distribution in Ordos Basin. Beijing: Petroleum Industry Press,1-228] [27] 杨秀春,徐凤银,王虹雅,李曙光,林文姬,王伟,郝帅. 2022. 鄂尔多斯盆地东缘煤层气勘探开发历程与启示. 煤田地质与勘探, 50(3): 30-41. [Yang X C,Xu F Y,Wang H Y,Li S G,Lin W J,Wang W,Hao S.2022. Exploration and development process of coalbed methane in eastern margin of Ordos Basin and its enlightenment. Coal Geology & Exploration, 50(3): 30-41] [28] 叶连俊,沙庆安,赵东旭,潘正莆,王尧,田兴有,陈景山. 1983. 华北地台沉积建造. 北京: 科学出版社,1-140. [Ye L J,Sha Q A,Zhao D X,Pan Z P,Wang Y,Tian X Y,Chen J S.1983. North China Platform Sedimentary Construction. Beijing: Science Press,1-140] [29] 翟明国. 2021. 鄂尔多斯地块是破解华北早期大陆形成演化和构造体制谜团的钥匙. 科学通报, 66(26): 3441-3461. [Zhai M G.2021. Ordos Block(Basin)is a key to understand early continental evolution and tectonic regime of the North China Craton. Chinese Science Bulletin, 66(26): 3441-3461] [30] 张福礼. 2002. 鄂尔多斯盆地早古生代复合的古构造体系与天然气. 地质力学学报, 8(3): 193-200. [Zhang F L.2002. Compound ancient tectonic system and natural gas of early Paleozoic in Ordos Basin. Journal of Geomechanics, 8(3): 193-200] [31] 张岳桥,施炜,廖昌珍,胡博. 2006. 鄂尔多斯盆地周边断裂运动学分析与晚中生代构造应力体制转换. 地质学报, 80(5): 639-647. [Zhang Y Q,Shi W,Liao C Z,Hu B.2006. Fault kinematic analysis and change in Late Mesozoic tectonic stress regimes in the peripheral zones of the Ordos Basin,North China. Acta Geologica Sinica, 80(5): 639-647] [32] 赵国春. 2009. 华北克拉通基底主要构造单元变质作用演化及其若干问题讨论. 岩石学报, 25(8): 1772-1792. [Zhao G C.2009. Metamorphic evolution of major tectonic units in the basement of the North China Craton key issues and discussion. Acta Petrologica Sinica, 25(8): 1772-1792] [33] 赵国春,孙敏,S A Wilde.2002. 华北克拉通基底构造单元特征及早元古代拼合. 中国科学(D辑), 32(7): 538-550. [Zhao G C,Sun M,Wilde S A.Tectonic unit characteristics and Early Proterozoic flattening in the basement of the North China Craton. Science in China(Series D), 32(7): 538-550] [34] 赵红格,刘池洋,翁望飞,桂小军,岳乐平,王建强,梁美艳. 2007. 新近纪鄂尔多斯盆地东西部的构造反转及其意义. 石油学报, 28(6): 6-11. [Zhao H G,Liu C Y,Weng W F,Gui X J,Yue L P,Wang J Q,Liang M Y.2007. Structural reverse and its significance to oil and gas in the east and west parts of Ordos Basin in the Neogene. Acta Petrolei Sinica, 28(6): 6-11] [35] 赵俊峰,刘池洋,Nigel Mountney,芦建军,曹冀龙,杨瑶,薛锐. 2015. 吕梁山隆升时限与演化过程研究. 中国科学: 地球科学, 45(10): 1427-1438. [Zhao J F,Liu C Y,Mountney N,Lu J J,Cao J L,Yang Y,Xue R.2015. Timing of uplift and evolution of the Lüliang Mountains,North China Craton. Scientia Sinica Terrae, 45(10): 1427-1438] [36] 赵瑞幅,郭敬辉,彭澎,刘富. 2011. 恒山地区古元古代2.1 Ga地壳重熔事件: 钾质花岗岩锆石U-Pb定年及Hf-Nd同位素研究. 岩石学报, 27(6): 1607-1623. [Zhao R F,Guo J H,Peng P,Liu F.2011.2.1 Ga crustal remelting event in Hengshan Complex: evidence from zircon U-Pb dating and Hf-Nd isotopic study on potassic granites. Acta Petrologica Sinica, 27(6): 1607-1623] [37] 赵振宇,郭彦如,王艳,林冬娟. 2012. 鄂尔多斯盆地构造演化及古地理特征研究进展. 特种油气藏, 19(5): 15-20, 151. [Zhao Z Y,Guo Y R,Wang Y,Lin D J.2012. Study progress in tectonic evolution and paleogeography of Ordos Basin. Special Oil and Gas Reservoirs, 19(5): 15-20, 151] [38] 朱定伟,丁文龙,游声刚,邓礼华,卞文杰. 2013. 鄂尔多斯盆地东南部古构造恢复及地质意义. 特种油气藏, 20(1): 48-51, 153. [Zhu D W,Ding W L,You S G,Deng L H,Bian W J.2013. Paleostructure restoration and its geological significance of southeast of Ordos Basin. Special Oil and Gas Reservoirs, 20(1): 48-51, 153] [39] Kröner A,Wilde S A,Li J H,Wang K Y.2005. Age and evolution of a Late Archean to Paleoproterozoic upper to lower crustal section in the Wutaishan/Hengshan/Fuping terrain of northern China. Journal of Asian Earth Sciences, 24(5): 577-595. [40] Liu S X,Wu C F,Li T,Wang H C.2018. Multiple geochemical proxies controlling the organic matter accumulation of the marine-continental transitional shale: a case study of the Upper Permian Longtan Formation,western Guizhou,China. Journal of Natural Gas Science and Engineering, 56: 152-165. [41] Luo W,Hou M C,Liu X C,Huang S G,Chao H,Zhang R,Deng X.2018. Geological and geochemical characteristics of marine-continental transitional shale from the Upper Permian Longtan Formation,northwestern Guizhou,China. Marine and Petroleum Geology, 89(1): 58-67.