Sedimentary characteristics of the lower Permian in Ordos Basin and its adjacent areas
Guo Yan-Qin1, Zhao Ling-Sheng1, Guo Bin-Cheng2, Fei Shi-Xiang3, Li Wen-Hou4, Zhang Qian4, Yuan Zhen1, Ma Yao1, He Zi-Qiong1, Li Bai-Qiang5
1 School of Earth Sciences and Engineering,Xi'an Shiyou University,Shaanxi Key Laboratory of Petroleum Accumulation Geology,Xi'an 710065,China; 2 Research Institute of Petroleum Exploration and Development,PetroChina,Beijing 100083,China; 3 Research Institute of Petroleum Exploration and Development,PetroChina Changqing Oilfield Company,Xi'an 710018,China; 4 Department of Geology/State Key Laboratory of Continental Dynamics, Northwest University,Xi'an 710069,China; 5 School of Resources and Environmental Engineering,Hefei University of Technology,Hefei 230009,China
Abstract：Based on the extensive field profile observation and detailed description of drilling cores in the basin,rock type and texture,sedimentary structure,paleontological fossils and logging curve response characteristics are analyzed to reveal the sedimentary characteristics of the lower Permian Taiyuan and Shanxi Formations in Ordos Basin and its adjacent areas. The result shows that the main sedimentary environments of the Taiyuan Formation are shelf,coast,alluvial fan and delta,in which the coastal sedimentary facies includes barrier island,lagoon and tidal flat. The delta facies can be divided into delta plain,delta front and prodelta. Alluvial fan,river,meandering river delta,lacustrine and coast are the main sedimentary facies in the Shanxi Formation. Fluvial facies includes braided and meandering river deposits,and the later can be divided into meandering river delta plain,meandering river delta front and prodelta deposits. The lacustrine is dominated by shallow lake deposits and the coast is dominated by lagoon deposits. During the Taiyuan sedimentary period,the marine sediments are dominant and distribute in a wide area to the south of Yinchuan and Yulin. The sedimentary environment has transitioned from shallow sea shelf in the eastern and western area,to lagoon and tidal flat in the central area,with barrier island developed in the middle. Alluvial fan and fan delta deposits are developed in the northwestern margin of the basin,and delta deposits are dominant in the vast areas of the north. The delta facies has changed from delta plain to delta front from north to south. During the sedimentary period of Shanxi Formation,sea water receded from the southeast part of the basin and evolved into marine continental transitional facies. Generally,the sedimentary environment has changed from alluvial fan(Wuda-Hangjinqi-Ordos area of the northern basin of basin),to braided and meandering river(Wuda-Hangjinqi-Ordos extend southward to Jingbian area),to delta plain(Jingbian to Yan'an), delta front(extend southward to Tongxin-Jingbian area), and to shallow lake(Pengyang-Jingyang area in the south of the basin). To the south of Pengyang-Jingyang area,the shallow lake deposited were replaced by delta deposits due to the sediment flux from the southern basin margin. The southern part of the Ordos Basin,Wuxiang-Yima area,was lagoon environment.
Guo Yan-Qin,Zhao Ling-Sheng,Guo Bin-Cheng et al. Sedimentary characteristics of the lower Permian in Ordos Basin and its adjacent areas[J]. JOPC, 2021, 23(1): 65-80.
[1] 陈洪德,李洁,张成弓,程立雪,程礼军. 2011. 鄂尔多斯盆地山西组沉积环境讨论及其地质启示. 岩石学报, 27(8): 2213-2229. [Chen H D,Li J,Zhang C G,Cheng L X,Cheng L J.2011. Discussion of sedimentary environment and its geological enlightenment of Shanxi Formation in Ordos Basin. Acta Petrologica Sinica, 27(8): 2213-2229] [2] 陈全红,李可永,张道锋,金栓联,郭艳琴,庞军刚,袁珍. 2010. 鄂尔多斯盆地本溪组—太原组扇三角洲沉积与油气聚集的关系. 中国地质, 37(2): 421-429. [Chen Q H,Li K Y,Zhang D F,Jin S L,Guo Y Q,Pang J G,Yuan Z.2010. The relationship between fan delta and hydrocarbon accumulation in Benxi-Taiyuan Formation,Ordos Basin. Geology in China, 37(2): 421-429] [3] 陈世悦,刘焕杰. 1997. 华北地台东部石炭—二叠纪岩相古地理特征. 中国区域地质, 16(4): 379-386. [Chen S Y,Liu H J.1997. Carboniferous-Permian lithofacies and paleogeography in the eastern partofthe North China Platform. Regional Geology of China, 16(4): 379-386] [4] 陈昭佑,王光强. 2010. 鄂尔多斯盆地大牛地气田山西组砂体组合类型及成因模式. 石油与天然气地质, 31(5): 632-639. [Chen Z Y,Wang G Q.2010. Assemblage types and genetic models of the Shanxi sandbodies in Daniudi gas field,Ordos Basin. Oil and Gas Geology, 31(5): 632-639] [5] 付金华,魏新善,任军峰. 2008. 伊陕斜坡上古生界大面积岩性气藏分布与成因. 石油勘探与开发, 35(6): 664-667,691. [Fu J H,Wei X S,Ren J F.2008. Distribution and genesis of large-scale upper Paleozoic lithologic gas reservoirs on Yi-Shaan Slope. Petroleum Exploration and Development, 35(6): 664-667,691] [6] 付锁堂,田景春,陈洪德,侯中健,张锦泉,刘文均,杨华,付金华,范正平,石晓英. 2003. 鄂尔多斯盆地晚古生代三角洲沉积体系平面展布特征. 成都理工大学学报(自然科学版), 30(3): 236-241. [Fu S T,Tian J C,Chen H D,Hou Z J,Zhang J Q,Liu W J,Yang H,Fu J H,Fan Z P,Shi X Y.2003. The delta depositional system distribution of late Paleozoic era in Ordos Basin. Journal of Chengdu University of Technology(Science & Technology Edition), 30(3): 236-241] [7] 郭书元,张广权,陈舒薇. 2009. 陆表海碎屑岩—碳酸盐岩混积层系沉积相研究: 以鄂尔多斯东北部大牛地气田为例. 古地理学报, 11(6): 611-627. [Guo S Y,Zhang G Q,Chen S W.2009. Study on sedimentary facies of mixed clastic-carbonate sediments strata system in epicontinental sea: a case of Daniudi gas field in northeastern Ordos. Journal of Palaeogeography(Chinese Edition), 11(6): 611-627] [8] 郭伟,刘洪林,薛华庆,兰朝利,汤小琪. 2015. 鄂尔多斯盆地北部山西组页岩沉积相及其对页岩储层的控制作用. 地质学报, 89(5): 931-941. [Guo W,Liu H L,Xue H Q,Lan Z L,Tang X Q.2015. Depositional facies of Permian Shanxi Formation gas shale in the northern Ordos Basin and its impact on shale reservoir. Acta Geologica Sinica, 89(5): 931-941] [9] 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] [10] 郭艳琴,王美霞,郭彬程,蔡志成,惠磊,何子琼,马瑶,李文厚,李百强. 2020. 鄂尔多斯盆地西缘北部上古生界沉积体系特征及古地理演化. 西北大学学报(自然科学版), 50(1): 93-104. [Guo Y Q,Wang M X,Guo B C,Cai Z C,Hui L,He Z Q,Ma Y,Li W H,Li B Q.2020. Sedimentary system characteristics and paleographic evolution of upper Paleozoic of northern west margin,Ordos Basin. Journal of Northwest University(Natural Science Edition), 50(1): 93-104] [11] 郭英海,刘焕杰,权彪,汪泽成,钱凯. 1998. 鄂尔多斯地区晚古生代沉积体系及古地理演化. 沉积学报,(3): 44-51. [Guo Y H,Liu H J,Quan B,Wang Z C,Qian K.1998. Late Paleozoic sedimentary system and paleogeographic evolution of Ordos Area. Acta Sedimentologica Sinica,(3): 44-51] [12] 郝蜀民,李良,尤欢增. 2007. 大牛地气田石炭—二叠系海陆过渡沉积体系与近源成藏模式. 中国地质, 34(4): 606-611. [Hao S M,Li L,You H Z.2007. Permo-carboniferous paralic depositional systems in the Daniudi gas field and its near-source box-type gas accumulation forming model. Geology in China, 34(4): 606-611] [13] 郝蜀民,惠宽洋,李良. 2006. 鄂尔多斯盆地大牛地大型低渗气田成藏特征及其勘探开发技术. 石油与天然气地质, 27(6): 762-768. [Hao S M,Hui K Y,Li L.2006. Reservoiring features of Daniudi low-permeability gas field in Ordos Basin and its exploration and development technologies. Oil & Gas Geology, 27(6): 762-768] [14] 侯中帅,陈世悦,王越,李天宝,赫庆庆,崔绮梦. 2018. 鄂尔多斯盆地东缘保德地区上古生界层序地层与沉积相特征. 古地理学报, 20(2): 232-243. [Hou Z S,Chen S Y,Wang Y,Li T B,He Q Q,Cui Q M.2018. Characteristics of sequence stratigraphy and sedimentary facies of the upper Paleozoic in Baode area,eastern margin of Ordos Basin. Journal of Palaeogeography(Chinese Edition), 20(2): 232-243] [15] 胡朝元,钱凯,王秀芹,施振生,张光武,许惠忠. 2010. 鄂尔多斯盆地上古生界多藏大气田形成的关键因素及气藏性质的嬗变. 石油学报, 31(6): 879-884. [Hu Z Y,Qian K,Wang X Q,Shi Z S,Zhang G W,Xu H Z.2010. Critical factors for the formation of an Upper Paleozoic giant gas field with multiple gas reservoirs in Ordos Basin and the transmutation of gas reservoir properties. Acta Petrolei Sinica, 31(6): 879-884] [16] 李剑,魏国齐,谢增业,刘锐娥,郝爱胜. 2013. 中国致密砂岩大气田成藏机理与主控因素: 以鄂尔多斯盆地和四川盆地为例. 石油学报,34(增刊1): 14-28. [Li J,Wei G Q,Xie Z Y,Liu R E,Hao A S.2013. Accumulation mechanism and main controlling factors of large tight sandstone gas fields in China: cases study on Ordos Basin and Sichuan Basin. Acta Petrolei Sinica,34(Supplement 1): 14-28] [17] 李树霞,向芳,张瑶,王誉婉,王金元. 2017. 鄂尔多斯盆地南缘晚古生代沉积物源及其对秦岭造山带北部演化的指示. 成都理工大学学报(自然科学版), 44(5): 589-601. [Li S X,Xiang F,Zhang Y,Wang Y W,Wang J Y.2017. Provenance analysis of the late Paleozoic sediments in south margin of the Ordos Basin and its indication to evolution of the north of Qinling Orogenic Belt in China. Journal of Chengdu University of Technology(Science & Technology Edition), 44(5): 589-601] [18] 李熙喆,张满郎,谢武仁. 2009. 鄂尔多斯盆地上古生界岩性气藏形成的主控因素与分布规律. 石油学报, 30(2): 168-175. [Li X Z,Zhang M L,Xie W R.2009. Controlling factors for lithologic gas reservoir and regularity of gas distribution in the upper Paleozoic of Ordos Basin. Acta Petrolei Sinica, 30(2): 168-175] [19] 梁积伟,郭艳琴,李玮,黄源林,肖丽,王若谷. 2007. 靖边气田山西组下段储层沉积微相特征. 西北大学学报(自然科学版), 37(5): 808-814. [Liang J W,Guo Y Q,Li W,Huang Y L,Xiao L,Wang R G.2007. Reservoir microfacies characteristics of lower member of Shanxi Formation in northwest part of Ordos Basin. Journal of Northwest University(Natural Science Edition), 37(5): 808-814] [20] 刘畅. 2019. 鄂尔多斯盆地临兴地区上古生界层序地层格架及沉积模式. 非常规油气, 6(1): 23-33. [Liu C.2019. Sequence stratigraphy framework and sedimentary model of upper Paleozoic in Linxing area,Ordos Basin. Unconventional Oil & Gas, 6(1): 23-33] [21] 刘锐娥,肖红平,范立勇,张春林,郝爱胜,缪卫东. 2013. 鄂尔多斯盆地二叠系“洪水成因型”辫状河三角洲沉积模式. 石油学报,34(增刊 1): 120-127. [Liu R E,Xiao H P,Fan L Y,Zhang C L,Hao A S,Liao W D.2013. A depositional mode of flood-induced braided river delta in Permian of Ordos Basin. Acta Petrolei Sinica,34(Supplement 1): 120-127] [22] 罗东明,陈舒薇,张广权. 2011. 大牛地气田上古生界沉积相与天然气富集规律的再认识. 石油与天然气地质, 32(3): 368-374. [Luo D M,Chen S W,Zhang G Q.2011. New understandings of the upper Paleozoic sedimentary facies and gas accumulation patterns in Daniudi gas field. Oil & Gas Geology, 32(3): 368-374] [23] 马瑶,李文厚,王若谷,庞军刚,吴越. 2015. 鄂尔多斯盆地子洲地区上古生界沉积相及演化特征. 地质科学, 50(1): 286-302. [Ma Y,Li W H,Wang R G,Pang J G, Wu Y.2015. Sedimentary facies and its evolution of the upper Paleozoic in Zizhou area of Ordos Basin. Chinese Journal of Geology(Scientia Geologica Sinica), 50(1): 286-302] [24] 闵琪,付金华,席胜利,刘新社,王涛,姬红,李燕. 2000. 鄂尔多斯盆地上古生界天然气运移聚集特征. 石油勘探与开发, 27(4): 26-29. [Min Q,Fu J H,Xi S L,Liu X S,Wang T,Ji H,Li Y.2000. Characteristics of natural gas migration and accumulation in the upper Paleozoic of Ordos Basin. Petroleum Exploration and Development, 27(4): 26-29] [25] 庞军刚,李文厚,杨友运,郭艳琴. 2007. 鄂尔多斯盆地子洲地区上古生界沉积体系特征. 天然气工业, 27(12): 58-61. [Pang J G,Li W H,Yang Y Y,Guo Y Q.2007. Features of upper Paleozoic depositional system in Zizhou region,Ordos Basin. Natural Gas Industry, 27(12): 58-61] [26] 邵龙义,董大啸,李明培,王海生,王东东,鲁静,郑明全,程爱国. 2014. 华北石炭—二叠纪层序—古地理及聚煤规律. 煤炭学报, 39(8): 1725-1734. [Shao L Y,Dong D X,Li M P,Wang H S,Wang D D,Lu J,Zheng M Q,Cheng A G.2014. Sequence-paleogeography and coal accumulation of the Carboniferous Permian in the North China Basin. Journal of China Coal Society, 39(8): 1725-1734] [27] 沈玉林,郭英海,李壮福. 2006. 鄂尔多斯盆地苏里格庙地区二叠系山西组及下石盒子组盒八段沉积相. 古地理学报, 8(1): 53-62. [Shen Y L,Guo Y H,Li Z F.2006. Sedimentary facies of the Shanxi Formation and Member 8 of Xiashihezi Formation of Permian in Suligemiao area,Ordos Basin. Journal of Palaeogeography(Chinese Edition), 8(1): 53-62] [28] 谭晨曦,李文厚,张慧军,郑勇. 2011. 鄂尔多斯盆地大牛地气田山西组沉积相研究. 西北大学学报(自然科学版), 41(1): 107-112. [Tan C X,Li W H,Zhang H J,Zheng Y.2011. Study of the sedimentary facies of Shanxi formation in Daniudi Gasfield of Ordos Basin. Journal of Northwest University(Natural Science Edition), 41(1): 107-112] [29] 王付斌,李良,陈亚平. 2007. 大牛地气田太原组沉积模式. 天然气工业, 27(12): 49-51. [Wang F B,Li L,Chen Y P.2007. Depositional model of Taiyuan Formation in Daniudi gas field,Ordos Basin. Natural Gas Industry, 27(12): 49-51] [30] 王国亭,姜在兴,陈昭佑. 2010. 大牛地气田太原组储集砂体沉积相研究. 新疆石油天然气, 6(1): 9-13. [Wang G T,Jiang Z X,Chen Z Y.2010. Study on sedimentary facies of Taiyuan Group reservoir sandstone in Danudi gas field. Xinjiang Oil & Gas, 6(1): 9-13] [31] 王越,陈世悦,梁绘媛,王剑,李天宝. 2016. 鄂尔多斯盆地保德地区上古生界沉积相与沉积演化特征. 沉积学报, 34(4): 775-784. [Wang Y,Chen S Y,Liang H Y,Wang J,Li T B.2016. Sedimentary facies and their evolution in the upper Paleozoic of Baode Area,Ordos Basin. Acta Sedimentologica Sinica, 34(4): 775-784] [32] 席胜利,李文厚,刘新社,郭英海. 2009. 鄂尔多斯盆地神木地区下二叠统太原组浅水三角洲沉积特征. 古地理学报, 11(2):187-194. [Xi S L,Li W H,Liu X S,Guo Y H.2009. Sedimentary characteristics of shallow water delta of the lower Permian Taiyuan Formation in Shenmu area, Ordos Basin. Journal of Palaeogeography(Chinese Edition), 11(2):187-194] [33] 杨辰雨,田景春,张翔,林小兵,刘绪钢,曹桐生,邢浩婷. 2015. 基于砂体构型精细刻画潮坪砂坝优质砂体: 以大牛地气田D17井区太原组2段为例. 石油与天然气地质, 36(2): 248-254. [Yang C Y,Tian J C,Zhang X,Lin X B,Liu X G,Cao T S,Xing H T.2015. Configuration-based fine description of high-quality sand bodies in tidal-flat bar: taking the tight sandstone reservoir in the 2nd member of the Taiyuan Formation in D-17 Wellblock in Daniudi gasfield as an example. Oil & Gas Geology, 36(2): 248-254] [34] 叶黎明,齐天俊,彭海燕. 2008. 鄂尔多斯盆地东部山西组海相沉积环境分析. 沉积学报, 26(2): 202-210. [Ye L M,Qi T J,Peng H Y.2008. Depositional environment analysis of Shanxi Formation in eastern Ordos Basin. Acta Sedimentologica Sinica, 26(2): 202-210] [35] 于兴河,王香增,王念喜,单新,周进松,韩小琴,李亚龙,杜永慧,赵晨帆. 2017. 鄂尔多斯盆地东南部上古生界层序地层格架及含气砂体沉积演化特征. 古地理学报, 19(6): 935-954. [Yu X H,Wang X Z,Wang N X,Shan X,Zhou J S,Han X Q,Li Y L,Du Y H,Zhao C F.2017. Sequence stratigraphic framework and sedimentary evolution characteristics of gas-bearing sandbody in the upper Paleozoic in southeastern Ordos Basin. Journal of Palaeogeography(Chinese Edition), 19(6): 935-954] [36] 张广权,陈舒薇,郭书元. 2011. 鄂尔多斯地区东北部大牛地气田山西组沉积相. 石油与天然气地质, 32(3): 388-397. [Zhang G Q,Chen S W,Guo S Y.2011. Sedimentary facies of the Shanxi Formation in Daniudi gas field,northeastern Ordos area. Oil & Gas Geology, 32(3): 388-397] [37] 赵靖舟,付金华,姚泾利,刘新社,王宏娥,曹青,王晓梅,马艳萍,凡元芳. 2012. 鄂尔多斯盆地准连续型致密砂岩大气田成藏模式. 石油学报,33(增刊1): 37-52. [Zhao J Z,Fu J H,Yao J L,Liu X S,Wang H E,Cao Q,Wang X M,Ma Y P,Fan Y F.2012. Quasi-continuous accumulation model of large tight sandstone gas field in Ordos Basin. Acta Petrolei Sinica,33(Supplement 1): 37-52] [38] 郑文波,胡向阳,陈舒薇,刘建党,贾超. 2015. 鄂尔多斯盆地大牛地气田上古生界沉积演化特征. 沉积学报, 33(2): 306-313. [Zheng W B,Hu X Y,Chen S W,Liu J D,Jia C.2015. Characteristics of sedimentary evolution in the upper Paleozoic,Daniudi gasfield,Ordos Basin. Acta Sedimentologica Sinica, 33(2): 306-313] [39] 朱宗良,李文厚,李克永,陈全红,郭艳琴,袁珍. 2010. 杭锦旗地区上古生界层序及沉积体系发育特征. 西北大学学报(自然科学版), 40(6): 1050-1054. [Zhu Z L,Li W H,Li K Y,Chen Q H,Guo Y Q,Yuan Z.2010. The characteristic of sequence stratigraphy and sedimentary systems of Taiyuan-Xiashihezi formation in Hangjinqi area. Journal of Northwest University(Natural Science Edition), 40(6): 1050-1054] [40] Du W,Jiang Z X,Zhang Y,Xu J.2013. Sequence stratigraphy and sedimentary facies in the Lower Member of the Permian Shanxi Formation,Northeastern Ordos Basin,China. Journal of Earth Science, 24(1): 75-88. [41] Jiang Z X,Xu J,Wang G T.2012. The discovery and significance of a sedimentary hiatus with in the Carboniferous Taiyuan Formation,northeastern Ordos Basin,China. AAPG Bulletin, 96(7): 1173-1195. [42] Liu J L,Liu K Y,Huang X.2016. Effect of sedimentary heterogeneities on hydrocarbon accumulations in the Permian Shanxi Formation,Ordos Basin,China: insight from an integrated stratigraphic forward and petroleum system modelling. Marine and Petroleum Geology, 76(9): 412-431. [43] Wang C Y,Wang Z C,Wang J L,Bao Y,Hu X M.2008. Reconstruction of paleo river systems and distribution of sedimentary facies of Shanxi and lower Shihezi formations in southern Ordos basin. Journal of China University of Mining & Technology, 18(2): 241-244. [44] Xue C Q,Zhong J H,Hou M X,Li F T,Peng C F.2019. Sedimentary facies distribution and the characteristics of transitional shale in the upper Palaeozoic in northeast Ordos basin,China. Arabian Journal of Geosciences,DOI: https://doi.org/10.1007/s12517-019-4669-5. [45] Yang Y T,Li W,Ma L.2005. Tectonic and stratigraphic controls of hydrocarbon systems in the Ordos Basin: a multicycle cratonic basin in central China. AAPG Bulletin, 89(2): 255-269.
