鄂尔多斯盆地四大古隆起演化及其油气控藏意义的差异<sup>&#x0002A;</sup>

doi:10.7605/gdlxb.2022.05.068

古地理学报 ›› 2022, Vol. 24 ›› Issue (5): 951-969. doi: 10.7605/gdlxb.2022.05.068

所属专题：近年来的相关构造古地理学文章；

• 热烈庆贺西北大学建校120周年 • 上一篇下一篇

鄂尔多斯盆地四大古隆起演化及其油气控藏意义的差异^*

包洪平^1,2, 何登发³, 王前平^1,2, 张雷^1,2, 张建伍^1,2, 严婷^1,2, 闫伟^1,2

1 中国石油长庆油田分公司勘探开发研究院,陕西西安 710018;
2 低渗透油气田勘探开发国家工程实验室,陕西西安 710018;
3 中国地质大学(北京)能源学院,北京 100083

收稿日期:2022-06-17 修回日期:2022-06-29 出版日期:2022-10-01 发布日期:2022-10-10
作者简介:包洪平,男,1967年生,1989年毕业于西北大学地质学系,教授级高级工程师,主要从事油气成藏地质研究。E-mail: bhp_cq@petroChina.com.cn。
*庆贺西北大学建校120周年!
基金资助:
中国石油长庆油田分公司重大科技专项(编号: ZDZX2021)资助

Four main paleouplifts evolution in Ordos Basin and their differences in significance of oil and gas reservoir control

BAO Hongping^1,2, HE Dengfa³, WANG Qianping^1,2, ZHANG Lei^1,2, ZHANG Jianwu^1,2, YAN Ting^1,2, YAN Wei^1,2

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;

Received:2022-06-17 Revised:2022-06-29 Online:2022-10-01 Published:2022-10-10
About author:BAO Hongping,born in 1967,professorial engineer,graduated from the Geology Dempartment, Northwest University in 1989. He is mainly engaged in oil and gas geological exploration. E-mail: bhp_cq@petroChina.com.cn.
Supported by:
Financially supported by the Major Science and Technology Special Project from PetroChina Changqing Oilfield Company(No.ZDZX2021)

摘要/Abstract

摘要： 鄂尔多斯盆地在地质历史上曾存在中央古隆起、乌兰格尔古隆起、渭河古隆起及乌审旗古隆起4个主要的隆起构造。作者通过沉积地层分布及构造演化过程剖析等方法,系统分析了4大古隆起构造演化的差异性及其对油气成藏控制作用的差异,并首次提出“渭河古隆起”的概念。研究表明,4大古隆起分别形成于不同的地质时代和区域构造环境,并经历了不同的演化过程: 中央古隆起形成于早古生代拉伸构造环境,在印支期发生构造反转而转化为坳陷沉降区; 乌兰格尔古隆起则是自盆地基底形成以来就已存在的长期继承性隆起,但在白垩纪及新生代发生差异隆升—沉降而分化为现今构造的不同单元; 渭河古隆起形成于白垩纪的区域挤压构造环境,也是在新生代发生差异隆升—沉降而分化为今构造的不同单元; 乌审旗古隆起是前寒武纪即已存在的古地形高地,早古生代并无进一步的发展,因而仅是在寒武纪海侵沉积时突显、奥陶纪开始沉积后即快速消隐。古隆起的控藏差异主要表现为: (1)古生代及之前形成的古隆起对盆地油气成藏多具有控相、控储及控制源—储配置等积极作用,且后期“由隆转坳”的古隆起对油气的成藏演化极为有利; (2)白垩纪以来的较晚期隆起对油气成藏总体以破坏性作用为主,尤以对古生界天然气藏的影响最为显著。

关键词: 鄂尔多斯盆地, 古隆起, 差异演化, 古隆起控藏, 渭河古隆起

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.

Key words: Ordos Basin, paleouplift, differential evolution, paleouplift controlling reservoir, Weihe Paleouplift

中图分类号:

P531TE121.2

包洪平, 何登发, 王前平, 张雷, 张建伍, 严婷, 闫伟. 鄂尔多斯盆地四大古隆起演化及其油气控藏意义的差异^*[J]. 古地理学报, 2022, 24(5): 951-969.

BAO Hongping, HE Dengfa, WANG Qianping, ZHANG Lei, ZHANG Jianwu, YAN Ting, YAN Wei. 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.

http://www.gdlxb.cn/CN/Y2022/V24/I5/951

参考文献

[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.

选择文件类型/文献管理软件名称

选择包含的内容

鄂尔多斯盆地四大古隆起演化及其油气控藏意义的差异^*

Four main paleouplifts evolution in Ordos Basin and their differences in significance of oil and gas reservoir control

RichHTML

PDF

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

[1]	张晓阳, 窦云飞, 孔维江, 李康, 吕大炜, 陈金凤, 贾海波, 沈晓丽. 鄂尔多斯盆地东缘临兴地区本溪组铝土岩系沉积发育地质过程及储集层物性特征^*[J]. 古地理学报, 2025, 27(2): 286-306.
[2]	李阳. 鄂尔多斯盆地南缘旬探1井奥陶系天文旋回信号提取及三级层序的判识^*[J]. 古地理学报, 2025, 27(1): 209-224.
[3]	刘恒宇, 刘明洁, 郝志磊, 任茵, 吴恩郁, 许晗, 钟寿康, 谭秀成, 曾伟, 连承波, 戴鸿鸣. 古老深层致密砂岩储集层孔隙形成与保存机制:以鄂尔多斯盆地长城系为例^*[J]. 古地理学报, 2024, 26(6): 1435-1451.
[4]	刘明成, 吴胜和, 万晓龙, 李桢, 樊建民, 陈朝晖, 王梓沣, 刘海旭. 鄂尔多斯盆地庆城油田延长组页岩层系层序地层与沉积相特征^*[J]. 古地理学报, 2024, 26(4): 779-795.
[5]	魏柳斌, 王宗延, 李漪, 庞志超, 王前平, 包洪平, 杨琦琦, 王振, 苏中堂, 张立军. 豹皮(斑)状碳酸盐岩分类与成因初探: 以鄂尔多斯盆地马家沟组四段为例^*[J]. 古地理学报, 2024, 26(4): 880-894.
[6]	吴宇婷, 甯濛, 夏攀, 乔占峰, 于洲, 文华国. 白云岩-蒸发岩共生体系白云石化过程研究:以鄂尔多斯盆地马家沟组为例^*[J]. 古地理学报, 2024, 26(4): 895-910.
[7]	黄有根, 许杰, 郑小鹏, 刘燕, 钟寿康, 李琳, 张道锋, 谭秀成. 鄂尔多斯盆地中东部下二叠统太原组灰岩沉积特征与沉积模式^*[J]. 古地理学报, 2024, 26(4): 911-925.
[8]	李华, 何幼斌, 姚凤南, 何一鸣, 姜纯伟, 张显坤, 吴吉泽, 徐艳霞, 梁建设. 鄂尔多斯盆地西北缘奥陶系克里摩里组等深流沉积^*[J]. 古地理学报, 2024, 26(4): 962-971.
[9]	齐荣, 李国蓉, 张军涛, 王付斌, 李宇翔, 杨飞, 刘璐, 何赛, 田家奇, 李肖肖. 鄂尔多斯盆地富县地区马家沟组热液改造特征与研究意义^*[J]. 古地理学报, 2024, 26(3): 632-643.
[10]	丁晓琪, 田胤瑜, 雷涛, 张威, 李晓慧, 高景云. 吕梁古隆起对鄂尔多斯盆地马家沟组沉积的控制作用: 基于陕西府谷剖面^*[J]. 古地理学报, 2024, 26(3): 671-682.
[11]	李元昊, 史立川, 雷秀洁, 淡卫东. 鄂尔多斯盆地上三叠统延长组负载构造类型及特征^*[J]. 古地理学报, 2024, 26(2): 269-278.
[12]	刘国庆, 苏中堂, 郝志磊, 魏柳斌, 任军锋, 廖慧鸿, 吴浩文. 鄂尔多斯盆地马家沟组碳酸盐岩-膏盐岩共生体系沉积微相与沉积模式^*[J]. 古地理学报, 2024, 26(2): 279-295.
[13]	熊加贝, 何登发, 成祥, 罗瑀峰. 鄂尔多斯盆地南缘奥陶系顶部碳酸盐岩风化壳特征及其成因机制^*[J]. 古地理学报, 2024, 26(1): 100-118.
[14]	毛丹凤, 何登发, 包洪平, 魏柳斌, 成祥, 苟钧壹, 石婧, 许艳华. 鄂尔多斯盆地怀远运动期不整合类型及其分布特征^*[J]. 古地理学报, 2024, 26(1): 119-131.
[15]	石婧, 何登发, 包洪平, 魏柳斌. 鄂尔多斯盆地东部边界的构造学分析:以石楼北地区为例^*[J]. 古地理学报, 2024, 26(1): 150-164.

模态框（Modal）标题

选择文件类型/文献管理软件名称

选择包含的内容

鄂尔多斯盆地四大古隆起演化及其油气控藏意义的差异*

Four main paleouplifts evolution in Ordos Basin and their differences in significance of oil and gas reservoir control

RichHTML

PDF

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

编辑推荐

Metrics

本文评价

鄂尔多斯盆地四大古隆起演化及其油气控藏意义的差异^*