Development stage of Jurassic Che−Mo Paleouplift in the Junggar Basin and its constraints on sedimentary system

KONG Jiahao; ZHANG Guanlong; XU Shumei; WANG Jinduo; ZENG Zhiping; WANG Qianjun; REN Xincheng; WU Xiangfeng; SHU Pengcheng; MA Huilei; CUI Huiqi

doi:10.12029/gc20220322001

2025 Vol. 52, No. 2

Article Contents

Article navigation > Geology in China > 2025 > 52(2): 631-649

Next Article Previous Article

KONG Jiahao, ZHANG Guanlong, XU Shumei, WANG Jinduo, ZENG Zhiping, WANG Qianjun, REN Xincheng, WU Xiangfeng, SHU Pengcheng, MA Huilei, CUI Huiqi. 2025. Development stage of Jurassic Che−Mo Paleouplift in the Junggar Basin and its constraints on sedimentary system[J]. Geology in China, 52(2): 631-649. doi: 10.12029/gc20220322001

Citation:

KONG Jiahao, ZHANG Guanlong, XU Shumei, WANG Jinduo, ZENG Zhiping, WANG Qianjun, REN Xincheng, WU Xiangfeng, SHU Pengcheng, MA Huilei, CUI Huiqi. 2025. Development stage of Jurassic Che−Mo Paleouplift in the Junggar Basin and its constraints on sedimentary system[J]. Geology in China, 52(2): 631-649. doi: 10.12029/gc20220322001

Development stage of Jurassic Che−Mo Paleouplift in the Junggar Basin and its constraints on sedimentary system

1.
Shengli Oilfield Branch Lusheng Petroleum Development Co., Ltd, Dongying 257000, Shandong, China
2.
The Exploration and Development Research Institute, Shengli Oilfield Sinopec, Dongying 257000, Shandong, China
3.
College of Marine Geosciences, Ocean University of China, Qingdao 266100, Shandong, China
4.
Key Lab of Submarine Geosciences and Prospecting Techniques, Ministry of Education, Qingdao 266100, Shandong, China
5.
Frontiers Science Center for Deep Ocean Multispheres and Earth System, Qingdao 266100, Shandong, China

Fund Project: Supported by Science and Technology Research Project of Sinopec Shengli Oilfield Company (No.302000018-21-zc0613-0075, No.2019QZKK0902).

More Information

Author Bio: KONG Jiahao, male, born in 1997, master, engaged in sedimentology, sequence stratigraphy and basin analysis; E-mail: 1154786051@qq.com
Corresponding author: XU Shumei, female, born in 1970, doctor, professor, engaged in the research and teaching of sedimentology and basin analysis; E-mail: xsm@ouc.edu.cn.

Received Date: 22 March 2022

Revised Date: 31 May 2022

Publish Date: 25 March 2025

Abstract

Abstract

This paper is the result of oil and gas exploration engineering.
Objective
Che−Mo synsedimentary paleouplift in Junggar basin is an important geomorphic unit that affects the structural style and reservoir distribution characteristics of Jurassic. The study of its development process is helpful to understand the basin mountain coupling relationship and the accumulation law of oil and gas reservoirs in Junggar basin.
Methods
Based on the logging data and seismic data of 41 wells in the abdomen of the basin, this paper makes a detailed analysis and isochronous comparison of Jurassic sand body and stratigraphic structure, and focuses on the synergistic evolution between the phased development of Che−Mo paleouplift and the orogenic belt around Junggar basin, especially Bogda mountain, and its influence on the basin boundary and sedimentary pattern.
Results
The evolution of Che−Mo paleouplift can be divided into three stages: initial development stage, rapid uplift stage and post uplift denudation stage. The initial development stage of Early Jurassic Che−Mo paleouplift has no or little influence on the distribution and structural style of Badaowan Formation and Sangonghe Formation. The study area is supplied by Zhayier mountain in the northwest and Kelameili mountain in the northeast, mainly forming braided river delta sedimentary system; The Middle Jurassic was the rapid uplift stage of Che−Mo paleouplift. In addition to the source supply of Zhayier mountain in the northwest and Kelameili mountain in the northeast, Bogda mountain also rose out of the water at the same time and began to supply the source, resulting in significant changes in basin boundary, stratigraphic distribution and structural style, resulting in large−area overlap of the first and second members of Xishanyao Formation, loss or denudation of the third members of Xishanyao Formation, The sedimentary system combination of Braided River Delta and beach bar is formed; The uplift of Che−Mo paleouplift in late Middle Jurassic and late Jurassic resulted in the denudation loss of Toutunhe Formation and Qigu Formation, forming a regional unconformity with Cretaceous.
Conclusions
The formation and evolution of Che−Mo paleouplift in Jurassic not only affected the sedimentary landform of the basin, but also significantly changed the basin boundary and provenance pattern, and led to significant changes in sedimentary system, stratigraphic structure style and distribution law.
- Jurassic /
- sedimentary system /
- Che−Mo paleouplift /
- tectonic evolution /
- oil and gas exploration engineering /
- Junggar Basin

FullText(HTML)

References

[1]	Eberth J, Pascovici G, Thomas H G, Warr N, Weißhaar D, Miniball C. 2001. From euroball to gamma−ray tracking arrays − new developments in ge detector technologies [C]//Nuclear Structure Physics − Celebrating the Career of Peter von Brentano − The International Symposium. Gottingen, Germany. Google Scholar
[2]	Fang Shihu, Guo Zhaojie, Jia Chengzao, Zhang Zhicheng, Wang Xulong, Wang Meina. 2006. Meso−cenozoic heavy minerals’assemblages in the southern Junggar Basin and its im plications for basin−orogen pattern[J]. Chinese Journal of Geology, 41(4): 648−662 (in Chinese with English abstract). Google Scholar
[3]	Fang Y, Wu C D, Guo Z J, Kejun H, Lin D, Wang L, Li L. 2015. Provenance of the southern Junggar Basin in the Jurassic: Evidence from detrital zircon geochronology and depositional environments[J]. Sedimentary Geology, 315: 47−63. doi: 10.1016/j.sedgeo.2014.10.014 CrossRef Google Scholar
[4]	Guo Zhaojie, Zhang Zhicheng, Wu Chaodong, Fang Shihu, Zhang Rui. 2006. Mesozoic Cenozoic Tianshan uplift process and its comparative study with Junggar and Altai Mountains[J]. Acta Geologica Sinica, 80(1): 1−15 (in Chinese with English abstract). doi: 10.1111/j.1755-6724.2006.tb00788.x CrossRef Google Scholar
[5]	He Dengfa, Chen Xinfa, Kuang Jun, Zhou Lu, Tang Yong, Liu Deguang. 2008. Formation, evolution and genetic mechanism of Chepaizi Mosuo Bay paleouplift in Junggar Basin[J]. Earth Science Frontiers, 15(4): 42−55 (in Chinese with English abstract). doi: 10.1016/S1872-5791(08)60038-X CrossRef Google Scholar
[6]	He Guoqi, Lu Shuning, Li Maosong. 1995. Significance of large fault systems in paleo−plate studies: A case study of Central Asia[J]. Geological Journal of Universities, 1(1): 1−10 (in Chinese with English abstract). Google Scholar
[7]	Ji Youliang, Zhou Yong, Kuang Jun, Wan Lu, Zhang Rui, Lu Chunhong. 2010. Formation and evolution of Che Mo ancient uplift in Junggar Basin and its control over sedimentary facies[J]. Science China Earth Science, 40(10): 1342−1355 (in Chinese). Google Scholar
[8]	Kuang Jun, Hou Lianhua, Zhang Yueqian, Shi Xinpiao, Wang Jinghong. 2009. Shallow reservoir forming factors and exploration direction of Chemogu uplift in Junggar Basin [J]. Xinjiang Petroleum Geology, 30(4): 445–449 (in Chinese with English abstract). Google Scholar
[9]	Kuang Lichun, Lei Dewen, Tang Yong. 2013. Jurassic Cretaceous Sedimentary Characteristics and Lithostratigraphic Reservoirs in Junggar Basin [M]. Beijing: Petroleum Industry Press, 1–156 (in Chinese with English abstract). Google Scholar
[10]	Li Zhong, Peng Shoutao. 2013. Mesozoic Cenozoic detrital zircon U−Pb chronology, provenance system analysis and intracontinental basin mountain evolution at the north and south foothills of Tianshan[J]. Acta Petrologica Sinica, 29(3): 739−755 (in Chinese with English abstract). Google Scholar
[11]	Liu Chuanpeng. 2013. Microscopic characteristics and effective reservoir control factors of the second member of Sangonghe Formation in Moxizhuang area, Junggar Basin[J]. Geology in China, 40(5): 1515−1522 (in Chinese with English abstract). Google Scholar
[12]	Liu Zhaorong. 2008. There is no Mesozoic paleouplift in the central Junggar Basin[J]. Xinjiang Petroleum Geology, 29(2): 256−259 (in Chinese with English abstract). Google Scholar
[13]	Lu Cheng. 2016. Study on Secondary Logging Interpretation of Old Wells in Blocks 1 and 3 in the Central Junggar Basin [D]. Xinjiang: Xinjiang University, 1−86 (in Chinese with English abstract). Google Scholar
[14]	Ma Baojun, Qi Jiafu, Yu Fusheng, Zhang Kexin. 2008, Structural characteristics and physical simulation of Che Mo ancient uplift in Junggar Basin[J]. Geotectonica et Metallogenia, 32(1): 36–41(in Chinese with English abstract). Google Scholar
[15]	Peng B, Jin Z J, Wang H, Jia X. 2018. Sedimentology and sequence stratigraphy of a retrogradational fan−delta system within Lower Triassic in the Mabei area, Junggar Basin (northwestern China)[J]. Russian Geology and Geophysics, 59: 606−619. doi: 10.1016/j.rgg.2018.05.002 CrossRef Google Scholar
[16]	Shang Xiaofei, Hou Jiagen, Cheng Yuanzhong, An Zhenyue, Yao Ruixiang, Li Yan. 2014. Discussion on the genetic mechanism of thick lake beach bar sand body and its geological significance—Taking the second member of Shahejie Formation in Banqiao sag of Huanghua depression as an example[J]. Acta Geologica Sinica, 88(9): 1705−1718 (in Chinese with English abstract). Google Scholar
[17]	Song Yan, Chen Shi, Zhang yilou, Liang Xinxin, Liang Yuanyuan, Hou Wen. 2020. Calibration of basin mountain differentiation time limit in the Middle and Late Jurassic in Bogda area, southeast margin of Junggar Basin[J]. Science Technology and Engineering, 20(3): 924−934 (in Chinese with English abstract). Google Scholar
[18]	Wang Jufeng, Deng Hongwen, Cai Xiyuan. 2005. Sedimentary system of Sangonghe Formation of Lower Jurassic in the hinterland of Junggar Basin[J]. Xinjiang Petroleum Geology, 26(2): 137−141 (in Chinese with English abstract). Google Scholar
[19]	Wang Xuying, Jiang Zaixing. 2020. Sedimentary system characteristics and model of Paleogene Fusan member in Subei Basin[J]. Geoscience, 34(6): 1132−1143 (in Chinese with English abstract). Google Scholar
[20]	Wei Hongxing. 2007. Structural Characteristics and Formation and Evolution of the Southern Margin of Bogda Mountain [D]. Shaanxi: Northwest University, 1–75 (in Chinese with English abstract). Google Scholar
[21]	Xu Shumei, Li Meng, Wang Jinduo, Ren Xincheng, Zeng Zhiping, Wu Xiangfeng, Xu Pengcheng, Feng Huaiwei. 2020. Cycle style and sand body superposition law of Lower Jurassic Sangonghe Formation in the abdomen of Junggar Basin[J]. Journal of Palaeogeography, 22(2): 221−234 (in Chinese with English abstract). Google Scholar
[22]	Xu Xueyi, Wang Hongliang, Chen Junlu. 2016. Geology of Tianshan and Its Adjacent Areas in China [M]. Beijing: Geological Publishing House, 1–175 (in Chinese with English abstract). Google Scholar
[23]	Peng Xiling. 2007. Query on chemo ancient uplift in Junggar Basin[J]. China Petroleum Exploration, (6): 63−71 (in Chinese with English abstract). Google Scholar
[24]	Yang Y T, Song C C, He S. 2015. Jurassic tectonostratigraphic evolution of the Junggar basin, NW China: A record of Mesozoic intraplate deformation in Central Asia[J]. Tectonics, 34(1): 86−115. doi: 10.1002/2014TC003640 CrossRef Google Scholar
[25]	Yue Yong, Jiang Shu, Tian Jingchun, Lin Xin. 2024. Late Cretaceous to Early Paleocene sedimentary environment evolution: Geochemical evidences of Well PBX1 in the southwestern Tarim Basin[J]. Geology in China, 51(2): 592−605 (in Chinese with English abstract). Google Scholar
[26]	Yu Fusheng, Amuguleng, Yang Guangda, Ma Baojun. 2008. Structural evolution characteristics and genetic simulation of Che Mo ancient uplift in Junggar Basin[J]. Acta Geoscientica Sinica, 29(1): 39−44 (in Chinese with English abstract). Google Scholar
[27]	Zhang Fushun, Yu Yingfan, Zhu Yunhui, Xia Mouzhong. 2007. Formation and evolution of Che Mo ancient uplift and oil and gas distribution[J]. Oil and Gas Geology of Western China, 3(1): 13−20 (in Chinese with English abstract). Google Scholar
[28]	Zhang Zhihuan, Qin liming, Li Wei, Wang Chunjiang, Qiu Nansheng, Meng Xianlong, Zhang Zhenying, Yuan Dongshan. 2009. Oil source and hydrocarbon source focus transfer of oil−bearing structures on the north and south sides of Chemogu uplift in the abdomen of Junggar Basin[J]. Geology in China, 36(4): 826−836 (in Chinese with English abstract). Google Scholar
[29]	Zhao Shujuan, Li Sanzhong, Liu Xin, Lou Da, Suo Yanhui , Dai Liming, Sun Wenjun, Li Tao, Wang Xuebin, Yang Chao. 2014. The structure of the eastern margin of Junggar Basin: The intracontinental process of the transition between Altay and North Tianshan orogenic belt[J]. Science China Earth Science, 44(10): 2130–2141 (in Chinese). Google Scholar
[30]	Zhao Wenzhi, Jin Jiuqiang. 2000. Formation and Evolution of Jurassic Prototype Basins in Northwest China [M]. Beijing: Geological Publishing House (in Chinese with English abstract). Google Scholar
[31]	Zhu Wen, Wang Ren, Lu Xinchuan, Shi Wanzhong, Ren Mengyi, Liu Kai. 2021. Yanshanian tectonic activity and sedimentary response in the northwest hinterland of Junggar Basin[J]. Earth Science, 46(5): 1692−1709 (in Chinese with English abstract). Google Scholar
[32]	Zhu X M, Li S L, Wu D, Zhu S F, Dong Y L, Zhao D N, Wang X L, Zhang Q. 2017. Sedimentary characteristics of shallow−water braided delta of the Jurassic, Junggar basin, Western China[J]. Journal of Petroleum Science and Engineering, 149: 591−602. doi: 10.1016/j.petrol.2016.10.054 CrossRef Google Scholar
[33]	Zhu Yunhui, Meng Xianlong. 2005. Formation and evolution of Chemo ancient uplift in Junggar Basin and its influence on oil and gas accumulation in the abdomen[J]. West China Petroleum Geosciences, 1(1): 55−57 (in Chinese with English abstract). Google Scholar
[34]	Zheng Youwei, Wang Yadong, Guo Jianming, Liu Xingwang, Zhao Guangliang, Su Long, Zheng Jianjing. 2016. Evolution characteristics of Jurassic heavy minerals in the southeast margin of Junggar Basin and its response to the uplift of Bogda mountain[J]. Acta Sedimentation Sinica, 34(6): 1147−1154 (in Chinese with English abstract). Google Scholar
[35]	Zhao Hongliang. 2006. Evolution and reservoir control law of Che Mo paleouplift in Junggar Basin[J]. Xinjiang Petroleum Geology, 27(2): 160−162 (in Chinese). Google Scholar
[36]	Zhou T Q, Wu C D, Yuan B, Shi Z K, Wang J L, Zhu W, Zhou Y X, Jiang X, Zhao J Y, Wang J, Ma J. 2019. New insights into multiple provenances evolution of the Jurassic from heavy minerals characteristics in Southern Junggar Basin, NW China[J]. Petroleum Exploration and Development, 46(1): 67−81. Google Scholar
[37]	方世虎, 郭召杰, 贾承造, 张志诚, 王绪龙, 王美娜. 2006. 准噶尔盆地南缘中−新生界沉积物重矿物分析与盆山格局演化[J]. 地质科学, 41(4): 648−662. doi: 10.3321/j.issn:0563-5020.2006.04.008 CrossRef Google Scholar
[38]	郭召杰, 张志诚, 吴朝东, 方世虎, 张锐. 2006. 中、新生代天山隆升过程及其与准噶尔、阿尔泰山比较研究[J]. 地质学报, 80(1): 1−15. doi: 10.3321/j.issn:0001-5717.2006.01.001 CrossRef Google Scholar
[39]	何登发, 陈新发, 况军, 周路, 唐勇, 刘德光. 2008. 准噶尔盆地车排子–莫索湾古隆起的形成演化与成因机制[J]. 地学前缘, 15(4): 42−55. doi: 10.3321/j.issn:1005-2321.2008.04.006 CrossRef Google Scholar
[40]	何国琦, 陆书宁, 李茂松. 1995. 大型断裂系统在古板块研究中的意义—以中亚地区为例[J]. 高校地质学报, 1(1): 1–10. Google Scholar
[41]	纪友亮, 周勇, 况军, 万璐, 张锐, 卢春红. 2010. 准噶尔盆地车–莫古隆起形成演化及对沉积相的控制作用[J]. 中国科学: 地球科学, 40(10): 1342−1355. Google Scholar
[42]	况军, 侯连华, 张越迁, 石新朴, 王京红. 2009. 准噶尔盆地车莫古隆起浅层成藏因素及勘探方向[J]. 新疆石油地质, 30(4): 445−449. Google Scholar
[43]	匡立春, 雷德文, 唐勇. 2013. 准噶尔盆地侏罗–白垩系沉积特征和岩性地层油气藏[M]. 北京: 石油工业出版社, 1–156. Google Scholar
[44]	李忠, 彭守涛. 2013. 天山南北麓中–新生界碎屑锆石U–Pb年代学记录、物源体系分析与陆内盆山演化[J]. 岩石学报, 29(3): 739−755. Google Scholar
[45]	刘传鹏. 2013. 准噶尔盆地莫西庄地区三工河组二段储层微观特征及有效储层控制因素[J]. 中国地质, 40(5): 1515−1522. doi: 10.3969/j.issn.1000-3657.2013.05.016 CrossRef Google Scholar
[46]	刘朝荣. 2008. 准噶尔盆地中部不存在中生代古隆起[J]. 新疆石油地质, 29(2): 256−259. Google Scholar
[47]	路成. 2016. 准噶尔盆地中部1、3区块老井测井二次解释研究[D]. 乌鲁木齐: 新疆大学, 1−86. Google Scholar
[48]	马宝军, 漆家福, 于福生, 张克鑫. 2008. 准噶尔盆地车–莫古隆起构造特征及物理模拟[J]. 大地构造与成矿学, 32(1): 36−41. Google Scholar
[49]	商晓飞, 侯加根, 程远忠, 安振月, 姚瑞香, 李燕. 2014. 厚层湖泊滩坝砂体成因机制探讨及地质意义—以黄骅坳陷板桥凹陷沙河街组二段为例[J]. 地质学报, 88(9): 1705−1718. Google Scholar
[50]	宋燕, 陈石, 张艺楼, 梁鑫鑫, 梁媛媛, 侯文. 2020. 关于准噶尔盆地东南缘博格达地区中晚侏罗世盆山分异时限的标定[J]. 科学技术与工程, 20(3): 924−934. Google Scholar
[51]	王居峰, 邓宏文, 蔡希源. 2005. 准噶尔盆地腹部下侏罗统三工河组沉积体系[J]. 新疆石油地质, 26(2): 137−141. Google Scholar
[52]	王旭影, 姜在兴. 2020. 苏北盆地古近系阜三段沉积体系特征与模式[J]. 现代地质, 34(6): 1132−1143. Google Scholar
[53]	魏红兴. 2007. 博格达山南缘构造特征及其形成演化[D]. 西安: 西北大学, 1–75. Google Scholar
[54]	许淑梅, 李萌, 王金铎, 任新成, 曾治平, 武向峰, 舒鹏程, 冯怀伟. 2020. 准噶尔盆地腹部下侏罗统三工河组旋回样式及砂体叠置规律[J]. 古地理学报, 22(2): 221−234. Google Scholar
[55]	徐学义, 王洪亮, 陈隽璐. 2016. 中国天山及邻区地质[M]. 北京: 地质出版社, 1–175. Google Scholar
[56]	彭希龄. 2007. 准噶尔盆地车莫古隆起质疑[J]. 中国石油勘探, (6): 63–71. Google Scholar
[57]	岳勇, 蒋恕, 田景春, 林新. 2024. 塔里木盆地西南部晚白垩世—早古新世沉积环境演化: 来自皮山PBX1井的地化证据[J]. 中国地质, 51(2): 592−605. Google Scholar
[58]	于福生, 阿木古冷, 杨光达, 马保军. 2008. 准噶尔盆地车–莫古隆起的构造演化特征及其成因模拟[J]. 地球学报, 29(1): 39−44. Google Scholar
[59]	张福顺, 余滢帆, 朱允辉, 夏忠谋. 2007. 车—莫古隆起形成演化与油气分布[J]. 中国西部油气地质, 3(1): 13−20. Google Scholar
[60]	张枝焕, 秦黎明, 李伟, 王春江, 邱楠生, 孟闲龙, 张振英, 袁东山. 2009. 准噶尔盆地腹部车莫古隆起南北两侧含油构造油源及烃源灶转移[J]. 中国地质, 36(4): 826−836. Google Scholar
[61]	赵淑娟, 李三忠, 刘鑫, 楼达, 索艳慧, 戴黎明, 孙文军, 李涛, 王学斌, 杨朝. 2014. 准噶尔盆地东缘构造: 阿尔泰与北天山造山带交接转换的陆内过程[J]. 中国科学: 地球科学, 44(10): 2130–2141. Google Scholar
[62]	赵文智, 靳久强. 2000. 中国西北地区侏罗纪原型盆地形成与演化[M]. 北京: 地质出版社. Google Scholar
[63]	朱文, 王任, 鲁新川, 石万忠, 任梦怡, 刘凯. 2021. 准噶尔盆地西北腹部燕山期构造活动与沉积响应[J]. 地球科学, 46(5): 1692−1709. Google Scholar
[64]	朱允辉, 孟闲龙. 2005. 准噶尔盆地车莫古隆起的形成演化及其对腹部油气成藏的影响[J]. 中国西部油气地质, 1(1): 55−57,108. Google Scholar
[65]	郑有伟, 王亚东, 郭建明, 刘兴旺, 赵光亮, 苏龙, 郑建京. 2016. 准噶尔盆地东南缘侏罗系重矿物演化特征及对博格达山隆升的响应[J]. 沉积学报, 34(6): 1147−1154. Google Scholar
[66]	赵宏亮. 2006. 准噶尔盆地车莫古隆起演化及其控藏规律[J]. 新疆石油地质, 27(2): 160−162. Google Scholar