Four main paleouplifts evolution in Ordos Basin and their differences in significance of oil and gas reservoir control
BAO Hongping1,2, HE Dengfa3, WANG Qianping1,2, ZHANG Lei1,2, ZHANG Jianwu1,2, YAN Ting1,2, YAN Wei1,2
1 Institute of Exploration and Development,Changqing Oilfield Company,PetroChina,Xi'an 710018,China;; 2 National Engineering Laboratory for Exploration and Development of Low Permeability Oil & Gas Fields,Xi'an 710018,China;; 3 School of Energy Resources,China University of Geosciences(Beijing),Beijing 100083,China;
Abstract:The Ordos Basin contains four main paleouplift structures in geological history, i.e., the Central,Ulager,Weihe,and Wushenqi Paleouplifts. This paper systematically analyzed the four paleouplifts with respect to stratigraphic distribution and tectonic evolution,and put forward a new concept of the Weihe Paleouplift. The four paleouplifts formed in different geological ages and regional tectonic environments,and it underwent different evolutionary processes: (1)The Central Paleouplift formed in the extensional tectonic setting of the Early Paleozoic,which was reversed and transformed into a depression subsidence area during the Indosinian period;(2)The Ulager Paleouplift is a long-term inherited uplift that has existed since the formation of the basin basement;different uplift subsidence occurred in the Cretaceous and Cenozoic and differentiated into different units of the present structure;(3)The Weihe Paleouplift formed in a regional compressive tectonic environment in the Cretaceous. It is also differentiated by differential uplift subsidence in the Cenozoic into different units of present structure;(4)The Wushenqi Paleouplift was an ancient topographic highland that existed in Precambrian,with no further development in the Early Paleozoic. Therefore,it was highlighted only in the Cambrian and disappeared rapidly after the Ordovician. The differences of reservoir control in paleouplifts are mainly as follows: (1)The paleouplift formed prior to and during the Paleozoic played a positive role in controlling facies,storage and source-storage configuration,and that the paleouplift later on from uplift to depression is beneficial to the evolution and accumulation of oil and gas,and reservoir formation;(2)The later uplift since the Cretaceous is mainly destructive to oil and gas accumulation,especially for Paleozoic natural gas reservoirs.
BAO Hongping,HE Dengfa,WANG Qianping et al. Four main paleouplifts evolution in Ordos Basin and their differences in significance of oil and gas reservoir control[J]. JOPC, 2022, 24(5): 951-969.
[1] 安作相. 1998. 陕北气区的形成与中央古隆起. 中国海上油气(地质), 12(3): 150-153. [An Z X.1998. Formation of Shanbel Gas area and Central Paleouplift. China Offshore Oil and Gas(Geology), 12(3): 150-153] [2] 白海峰,包洪平,李泽敏,郝松立,武春英,井向辉. 2020. 鄂尔多斯盆地元古界长城系沉积特征及天然气成藏潜力. 地质科学, 55(3): 672-691. [Bai H F,Bao H P,Li Z M,Hao S L,Wu C Y,Jing X H.2020. Sedimentary characteristics and gas accumulation potential of Changcheng system in Ordos Basin in Proterozoic. Chinese Journal of Geology, 55(3): 672-691] [3] 包洪平,郭玮,刘刚,李磊,武春英,白海峰. 2020a. 鄂尔多斯地块南缘构造演化及其对盆地腹部的构造-沉积分异效应. 地质科学, 55(3): 703-725. [Bao H P,Guo W,Liu G,Li L,Wu C Y,Bai H F.2020a. Tectonic evolution in the southern Ordos block and its significance in the tectono-depositional differentiation in the interior of the Ordos Basin. Chinese Journal of Geology, 55(3): 703-725] [4] 包洪平,黄正良,武春英,魏柳斌,任军峰,王前平. 2020b. 鄂尔多斯盆地中东部奥陶系盐下侧向供烃成藏特征及勘探潜力. 中国石油勘探, 25(3): 134-145. [Bao H P,Huang Z L,Wu C Y,Wei L B,Ren J F,Wang Q P.2020b. The reservoir forming characteristics and exploration potential of Ordovician under salt system derived from lateral hydrocarbon supply and accumulation,in central and eastern Ordos Basin. China Petroleum Exploration, 25(3): 134-145] [5] 包洪平,邵东波,郝松立,章贵松,阮正中,刘刚,欧阳征健. 2019. 鄂尔多斯盆地基底结构及早期沉积盖层演化. 地学前缘, 26(1): 33-43. [Bao H P,Shao D B,Hao S L,Zhang G S,Ruan Z Z,Liu G,Ouyang Z J.2019. Structure of basement and evolution of early sedimentary cover of Ordos Basin. Earth Science Frontiers, 26(1): 33-43] [6] 陈陇刚,王北颖,陈丽荣,张飚,代新宇. 2003. 华山花岗岩的包体特征及指示意义. 陕西地质, 21(1): 61-66. [Chen L G,Wang B Y,Chen L R,Zhang B,Dai X Y.2003. Inclusion and its indicating features of the Huashan granite. Geology of Shaanxi, 21(1): 61-66] [7] 邓昆,张哨楠,周立发,刘燕. 2011. 鄂尔多斯盆地古生代中央古隆起形成演化与油气勘探. 大地构造与成矿学, 35(2): 190-197. [Den K,Zhang S N,Zhou L F,Liu Y.2011. Formation and evolution of Paleozoic Central Paleouplift and Oil and Gas Exploration in Ordos Basin. Geotectonica et Metallogenia, 35(2): 190-197] [8] 何登发,谢晓安. 1997. 中国克拉通盆地中央古隆起与油气勘探. 勘探家, 2(2): 11-19. [He D F,Xie X A.1997. Central Paleouplift and oil and gas exploration in China Craton Basin. Explorationist, 2(2): 11-19] [9] 何登发,包洪平,孙方源,张才利,开百泽,许艳华,成祥,翟咏荷. 2020. 鄂尔多斯盆地中央古隆起的地质结构与成因机制. 地质科学, 55(3): 627-656. [He D F,Bao H P,Sun F Y,Zhang C L,Kai B Z,Xu Y H,Cheng X,Zhai Y H.2020. Geologic structure and genetic mechanism for the central uplift in the Ordos Basin. Chinese Journal of Geology, 55(3): 627-656] [10] 何登发,李德生,童晓光,赵文智. 2008. 多期叠加盆地古隆起控油规律. 石油学报, 29(4): 475-488. [He D F,Li D S,Tong X G,Zhao W Z.2008. Oil control law of paleo-uplift in multi-stage superimposed basin. Acta Petrolei Sinica, 29(4): 475-488] [11] 黄建松,郑聪斌,张军. 2005. 鄂尔多斯盆地中央古隆起成因分析. 天然气工业, 25(4): 23-26. [Huang J S,Zheng C B,Zhang J.2005. Origin analysis of Central Paleouplift in Ordos Basin. Natural Gas Industry, 25(4): 23-26] [12] 贾进斗,何国琦,李茂松,周鼎潮,张林祥. 1997. 鄂尔多斯盆地基底结构特征及其对古生界天然气的控制. 高校地质学报, 3(2): 144-153. [Jia J D,He G Q,Li M S,Zhou D W,Zhang L X.1997. Characteristics of basement structure in Ordos Basin and its control over Paleozoic natural gas. Geological Journal of China Universities, 3(2): 144-153] [13] 解国爱,张庆龙,郭令智. 2003. 鄂尔多斯盆地西南缘古生代前陆盆地与中央古隆起成因及其与油气的关系. 石油学报, 24(2): 18-29. [Xie A G,Zhang Q L,Guo L Z.2003. Origin of Paleozoic foreland basin and Central Paleouplift in the west south margin of Ordos Basin. Acta Petrolei Sinica, 24(2): 18-29] [14] 解国爱,张庆龙,潘明宝,赵世龙,任文军,郭令智. 2005. 鄂尔多斯盆地两种不同成因古隆起的特征及其在油气勘探中的意义. 地质通报, 24(4): 373-377. [Xie A G,Zhang Q L,Pan M B,Zhao S L,Ren W J,Guo L Z.2005. Characteristics of two different genesis paleouplifts in Ordos Basin and their significance in oil and gas exploration. Geological Bulletin, 24(4): 373-377] [15] 吕艳,郑利宏,门文辉,李亚哲,徐永龙. 2014. 花岗岩地貌景观的成因及类型划分刍议: 以陕西华山地区为例. 地质与勘探, 50(1): 18-27. [Lü Y,Zheng L H,Men W H,Li Y Z,Xu Y L.2014. Genesis and classification of granite landscapes: a case study of the Huashan Mountains in Shaanxi Province. Geology and Exploration, 50(1): 18-27] [16] 任文军,张庆龙,张进,郭令智. 1999. 鄂尔多斯盆地中央古隆起板块构造成因初步研究. 大地构造与成矿学, 23(2): 191-196. [Ren W J,Zhang Q L,Zhang J,Guo L Z.1999. A preliminary study on the plate tectonic origin of the central paleo-uplift in the Ordos Basin. Geotectonica et Metallogenia, 23(2): 191-196] [17] 汤锡元,郭忠铭,陈荷立. 1992. 陕甘宁盆地西缘逆冲推覆构造及油气勘探. 西安: 西北大学出版社,1-156. [Tang X Y,Guo Z M,Chen H L.1992. Thrust Nappe Structure and Hydrocarbon Exploration in the Western Margin of Shaanxi-Gansu-Ningxia Basin. Xi'an: Northwest University Press,1-156] [18] 汤显明,惠斌耀. 1993. 鄂尔多斯盆地中央古隆起与天然气聚集. 石油与天然气地质, 14(1): 64-71. [Tang X M,Hui B Y.1993. Central Paleouplift and natural gas accumulation in Ordos Basin. Oil & Gas Geology, 14(1): 64-71] [19] 汪泽成,赵文智,胡素云,徐安娜,江青春,姜华,黄士鹏,李秋芬. 2017. 克拉通盆地构造分异对大油气田形成的控制作用: 以四川盆地震旦系—三叠系为例. 天然气工业, 37(1): 9-23. [Wang Z C,Zhao W Z,Hu S Y,Xu A N,Jiang Q C,Jiang H,Huang S P,Li Q F.2017. Control of tectonic differentiation on the formation of large oil and gas fields in craton basins: a case study of Sinian-Triassic of the Sichuan Basin. Natural Gas Industry, 37(1): 9-23] [20] 王鸿祯,史晓颖. 1998. 沉积层序及海平面旋回的分类级别: 旋回周期的成因讨论. 现代地质, 12(1): 1-16. [Wang H Z,Shi X Y.1998. Hierarchy of depositional seqences and eustatic cycles: a discussion on the mechanism of sedimentary cycles. Geoscience, 12(1): 1-16] [21] 王建强,贾楠,刘池洋,邱欣卫,赵红格,郭真. 2011. 鄂尔多斯盆地西南部下白垩统宜君组砾岩砾组分析及其意义. 沉积学报, 29(2): 226-234. [Wang J Q,Jia N,Liu C Y,Qiu X W,Zhao H G,Guo Z.2011. Fabric analysis of Yijun Gravels of Lower Cretaceous in the southwestern Ordos Basin. Acta Sedimentologica Sinica, 29(2): 226-234] [22] 魏柳斌,陈洪德,郭玮,严婷,蔡郑红,周黎霞. 2021. 鄂尔多斯盆地乌审旗—靖边古隆起对奥陶系盐下沉积与储层的控制作用. 石油与天然气地质, 42(2): 391-400,521. [Wei L B,Chen H D,Guo W,Yan T,Cai Z H,Zhou L X.2021. Wushen-Jingbian paleo-uplift and its control on the Ordvician subsalt depsition and reservioirs in Ordos Basin. Oil & Gas Geology, 42(2): 391-400,521] [23] 肖娥,胡建,张遵忠,戴宝章,王艳芬,李海勇. 2012. 东秦岭花山复式岩基中蒿坪与金山庙花岗岩体岩石地球化学、锆石 U-Pb 年代学和 Lu-Hf 同位素组成. 岩石学报, 28(12): 31-46. [Xiao E,Hu J,Zhang Z Z,Dai B Z,Wang Y F,Li H Y.2012. Petrogeochemistry,zircon U-Pb dating and Lu-Hf isotopic compositions of the Haoping and Jinshanmiao granites from the Huashan complex batholith in eastern Qinling Orogen. Acta Petrologica Sinica, 28(12): 31-46] [24] 徐春春,沈平,杨跃明,赵路子,罗冰,文龙,陈康,冉崎,钟原,彭翰霖. 2020. 四川盆地川中古隆起震旦系—下古生界天然气勘探新认识及勘探潜力. 天然气工业, 40(7): 1-9. [Xu C C,Shen P,Yang Y M,Zhao L Z,Luo B,Wen L,Chen K,Ran Q,Zhong Y,Peng H L.2020. New understandings and potential of Sinian-Lower Paleozoic natural gas exploration in the central Sichuan paleo-uplift of the Sichuan Basin. Natural Gas Industry, 40(7): 1-9] [25] 许志琴,李源,梁凤华,裴先治. 2015. “秦岭—大别—苏鲁”造山带中“古特提斯缝合带”的连接. 地质学报, 89(4): 671-680. [Xu Z Q,Li Y,Liang F H,Pei X Z.2015. A connetion between of the Paleo-Tethys suture zone in the Qinlin-Dabie-Sulu Orogenic belt. Acta Geologica Sinica, 89(4): 671-680] [26] 许志琴,杨经绥,姜枚,李海兵. 1999. 大陆俯冲作用及青藏高原周缘造山带的崛起. 地学前缘, 6(3): 139-151. [Xu Z Q,Yang J S,Jiang M,Li H B.1999. Continental subduction and uplifting of the orogenic belts at the margin of the Qinhai-Tibet Plateau. Earth Science Frontiers, 6(3): 139-151] [27] 杨华,付金华,包洪平. 2010. 鄂尔多斯地区西部和南部奥陶纪海槽边缘沉积特征与天然气成藏潜力分析. 海相油气地质, 15(2): 1-13. [Yang H,Fu J H,Bao H P.2010. Sedimentary characteristics and natural gas reservoir potential of Ordovician trough margin in western and southern Ordos Region. Marine Origin Petroleum Geology, 15(2): 1-13] [28] 杨兴科,杨永恒,季丽丹,苏春乾,郑孟林,赵亮. 2006. 鄂尔多斯盆地东部热力作用的期次和特点. 地质学报, 80(5): 705-711. [Yang X K,Yang Y H,Ji L D,Su C Q,Zheng M L,Zhao L.2006. Stages and characteristics of thermal actions in eastern part of Ordos Basin. Acta Geologica Sinica, 80(5): 705-711] [29] 张宏法,陈刚,包洪平,王润三,马占荣,彭天朗. 2011. 山西临县紫金山碱性杂岩内二长岩锆石 U-Pb 年代学及其意义. 矿物学报, 31(1): 70-79. [Zhang H F,Chen G,Bao H P,Wang R S,Ma Z R,Peng T L.2011. U-Pb Zircon geochronology of the Zijinshan Alkaline intrusive complex,Shanxi Province,and its geological significance by using LA-ICP-MS. Acta Mineralogica Sinica, 31(1): 70-79] [30] 张吉森,杨奕华,王少飞,帅世敏. 1995. 鄂尔多斯地区奥陶系沉积及其与天然气的关系. 天然气工业, 15(2): 5-10. [Zhang J S,Yang Y H,Wang S F,Shuai S M.1995. Ordovician sediments in Ordos area and their relationship with natural gas. Natural Gas Industry, 15(2): 5-10] [31] 张抗. 1989. 鄂尔多斯断块构造和资源. 陕西西安: 陕西科学技术出版社,1-394. [Zhang K.1989. Ordos Fault Block Tectonics and Resouces. Shaanxi Xi'an: Shaanxi Science and Technology Publishing House,1-394] [32] 赵俊峰,刘池洋,王晓梅,马艳萍,黄雷. 2009. 吕梁山地区中新生代隆升演化探讨. 地质论评, 55(5): 663-672. [Zhao J F,Liu C Y,Wang X M,Ma Y P,Huang L.2009. Uplifting and evolution characteristics in the Lvliang Mountain and its adjacent area during the Meso-Cenozoic. Geologica Review, 55(5): 663-672] [33] 赵重远,刘池祥. 1990. 华北克拉通沉积盆地形成与演化及其油气赋存. 陕西西安: 西北大学出版社,1-189. [Zhao C Y,Liu C Y.1990. Formation and Evolution of Sedimentary Basins in North China Craton and Their Oil and Gas Occurrence. Shaanxi Xi'an: Northwest University Press,1-189] [34] 赵重远. 1983. 鄂尔多斯西缘构造演化及板块应力机制初探. 见: 内蒙古自治区石油学会编,鄂尔多斯盆地西缘地区石油地质论文集. 呼和浩特: 内蒙古人民出版社,20-28. [Zhao C Y.1983. Tectonic Evolution and Plate Stress Mechanism in West Edge of Ordos Basin. In: Papers on Petroleum Geology in the Western Margin of Ordos. Hohhot: Inner Mongolia People's Publishing House,20-28] [35] 中国石油地质志编委会. 1992. 中国石油地质志(卷十二,长庆油田). 北京: 石油工业出版社,1-490. [The Editorial Committee on Petroleum Geology of China. 1992. Petroleum Geology of China(Volume 12,Changqing Oilfield). Beijing: Petroleum Industry Press,1-490] [36] Cooper M R.1990. Tectonic cycles in Southern Africa.Earth Science Review, 28(4): 321-364. [37] Gansser A.1964. Geology of the Himalayas. Geochimica et Cosmochimica Acta, 30(5): 553-554. [38] Mc A. Powell ,C,Conaghan P J.1975. Tectonic models of the Tibetan Plateau. Geology, 3: 727-731. [39] Mitchum R M,Wagoner Wagoner J C.1991. High frequency sequences and their stacking patterns: sequence-stratigraphic evidence of high frequency eustatic cycles.Sedimentaty Geology, 70: 131-160. [40] Molnar P,Tapponnier P.1975. Cenozoic tectonics of Asia: effects of a continental collision. Science, 189(1): 419-426. [41] Powell C M, Conaghan P J.1975. Tectonics models of the Tibetan Plateau. Geology, 3(12): 727-732.