Abstract Based on the outcrop profile and regional geological data,the sedimentary evolution of Carboniferous-Permian in western Wushi sag was investigated. The Carboniferous western Wushi sag is located between the southern Tianshan residual sea basin and Keping-Wensu uplift,and is quite different from that of the inner Tarim Basin. During the early stage of Early Carboniferous,as the boundary of Suogedangtawu Fault in the northern margin of Keping-Wensu uplift controlling the sedimentation,there were shallow shelf environment that was dominated by shore littoral and diamictic carbonate. During the late stage of Early Carboniferous,the first marine-flooding made Keping-Wensu uplift partially submerged,which was accompanied by a strong subsidence,forming bathyal slope environment. The flysch deposition of the proximal-distal turbidite fan typified by Kulu Formation and Suogedangtawu Formation are seen to occur within such bathyal slope environment,and continued until the early stage of Late Carboniferous. During the late stage of Late Carboniferous,another large-scale transgression occurred in this area,which,in turn,made Keping-Wensu uplift mostly submerged. The original uplift,then shifted to the open platform environments. Typical platform margin reef were well developed in the north and west edge of the study area,and northward extended to Kezibulake area,outward to the reef front slope and shallow shelf environment,which was continued until the early stage of Middle Permian. After the Middle Permian,due to the large-scale intracontinental volcano activity,large-scale regression developed in this area. At the end of the Late Permian,accompanied by the combination of Tarim Plate and Middle Tianshan Massif,the South Tianshan Ocean disappeared and formed the ancient Tianshan orogenic belt of the Hercynian period. This completely ended the marine sediments and entered the stage of continental deposition. In addition to the Carboniferous shoreline facies sandstones,the reef limestone reservoirs of the Early-Middle Permian were widely distributed,the buried depth of the reservoirs is relatively shallow and the physical properties are relatively good,giving rise to an important target for oil and gas exploration.
Fund:Financially supported by the National Science and Technology Major Project(No.2011ZX05001)
Cite this article:
Jia Jin-Hua,Zhang Li-Ping,Chen Xiu-Yan. Sedimentary evolution of the Carboniferous-Permian in western Wushi sag,Tarim Basin[J]. JOPC, 2018, 20(3): 423-434.
Jia Jin-Hua,Zhang Li-Ping,Chen Xiu-Yan. Sedimentary evolution of the Carboniferous-Permian in western Wushi sag,Tarim Basin[J]. JOPC, 2018, 20(3): 423-434.
[1] 高小芬,林晓,徐亚东,乐明亮. 2014. 南天山古生代—中生代沉积盆地演化. 地球科学: 中国地质大学学报, 39(8): 1119-1128. [Gao X F,Lin X,Xu Y D,Yue M L.2014. Evolution of sedimentary basins in South Tianshan during Paleozoic-Mesozoic. Earth Science-Journal of China University of Geosciences, 39(8): 1119-1128] [2] 郭春涛,李忠,高剑,董顺利. 2015. 塔里木盆地西北缘乌什地区石炭系沉积与碎屑锆石年代学记录及其反映的构造演化. 岩石学报, 31(9): 2679-2695. [Guo C T,Li Z,Gao J,Dong S L.2015. Depositional and detrital zircon geochronological records of Carboniferous system in Wushi,Northwest Tarim Basin: Implications for tectonic evolution. Acta Petrologica Sinica, 31(9): 2679-2695] [3] 何镜宇,孟祥化. 1987. 沉积岩和沉积相模式及建造. 北京: 地质出版社,1-435. [He J Y,Meng X H.1987. Sedimentary and Sedimentary Facies Models and Buildup. Beijing: Geological Publishing House,1-435] [4] 黄兴,朱飞,张雄华,刘晓煌,赵志刚,寇晓虎,杨宝忠. 2014. 新疆阿合奇地区晚石炭世—早二叠世<inline-graphic xlink:href="1671-1505-20-3-423/img_16.png"/>类动物群. 地质通报, 33(1): 33-41. [Huang X,Zhu F,Zhang X H,Liu X H,Zhao Z G,Kou X H,Yang B Z.2014. A study of Late Carboniferous-Early Permian Fusulinids fauna from Akqi area,Xinjiang. Geological Bulletin of China, 33(1): 33-41] [5] 贾承造,张师本,吴绍祖,黄智斌,王宝瑜,高琴琴,周守沄,王智,梁云海,赵治信,成守德,李猛,屈讯,杜品德,李永安,谭泽金,王玉珍,剡鸿炳,王德林,王齐. 2004. 塔里木盆地及周边地层(上册). 北京: 科学出版社,1-547. [Jia C Z,Zhang S B,Wu S Z,Huang Z B,Wang B Y,Gao Q Q,Zhou S Y,Wang Z,Liang Y H,Zhao Z X,Cheng S D,Li M,Qu X,Du P D,Li Y A,Tan Z J,Wang Y Z,Yan H B,Wang D L,Wang Q.2004. Stratigraphy on the Periphery of the Tarim Basin(volumeⅠ). Beijing: Science Press,1-547] [6] 贾进华,周东延,张立平,刘泽斌,周兴熙. 2004. 塔里木盆地乌什凹陷石油地质特征. 石油学报, 25(6): 12-17. [Jia J H,Zhou D Y,Zhang L P,Liu Z B,Zhou X X.2004. Petroleum geologic characteristics of Wushi sag in Tarim Basin. Acta Petrolei Sinica, 25(6): 12-17] [7] 贾润胥,翟晓先,周永昌,张大权,周棣康. 1991.塔里木盆地东北地区地质构造基本特征. 见: 贾润胥. 中国塔里木盆地北部油气地质研究(第一辑,地层沉积).武汉: 中国地质大学出版社,9-28. [Jia R X,Zhai X X,Zhou Y C,Zhang D Q,Zhou D K.1991. Basic Features of Geological Structures in Northeastern Tarim Basin. In: Jia R X(ed.). Reaearch of Petroleum Geology of Northern Tarim Basin in China. Stratigraphy and Sedimentology(1). Wuhan:China University of Geoscience Press,9-28] [8] 李继亮. 1989. 准噶尔弧后残留盆地与天山造山带大地构造关系. 沉积学报,(增刊):112-120. [Li J L.1989. The Tectonics relationship between the back arc preserved basin in Junggar and Tianshan Orogenic Belt. Acta Sedimentologica Sinica,(Supplement): 112-120] [9] 李曰俊,杨海军,赵岩,罗俊成,郑多明,刘亚雷. 2009. 南天山区域大地构造与演化. 大地构造与成矿学, 33(1): 94-104. [Li Y J,Yang H J,Zhao Y,Luo J C,Zheng D M,Liu Y L.2009. Tectonic framework and evolution of South Tianshan,NW China. Geotectonica et Metallogenia, 33(1): 94-104] [10] 李忠,高剑,郭春涛,徐建强. 2015. 塔里木块体北部泥盆—石炭纪陆缘构造演化: 盆地充填序列与物源体系约束. 地学前缘, 22(1): 35-52. [Li Z,Gao J,Guo C C,Xu J Q.2015. Devonian-Carboniferous tectonic evolution of continential margins in Northern Tarim block,Northwest China: Constrained by basin-fill sequences and provenance systems. Earth Science Frontiers, 22(1): 35-52] [11] 刘本培,王自强,张传恒,马鸿文,周洪瑞,朱鸿,龚一鸣,贾维民. 1996. 西南天山构造格局与演化. 武汉: 中国地质大学出版社,1-120. [Liu B P,Wang Z Q,Zhang C H,Ma H W,Zhou H R,Zhu H,Gong Y M,Jia W M.1996. The Tectonic Framework and Evolution in Southwest Tianshan Mountains,China. Wuhan: China University of Geosciences Press, 1-120] [12] 罗金海,车自成,周新源,李勇,李建立,张敬艺. 2007. 塔里木盆地西北缘二叠系礁灰岩的时空分布特征及其油气地质意义. 地质论评, 53(5): 600-607. [Luo J H,Che Z C,Zhou X Y,Li Y,Li J L,Zhang J Y.2007. Spatio-temporal distribution and its oil-gas significances of Permian Reef Limestone on the Northwestern Margin of the Tarim Basin. Geological Review, 53(5): 600-607] [13] 童雪飞,康志宏,周磊,刘晨晓,郭瑞琴,皇甫静静. 2016. 塔里木西北缘乌什南上石炭统索格当他乌组微量稀土元素特征及地质意义. 现代地质, 30(2): 426-435. [Tong X F,Kang Z H,Zhou L,Liu C X,Guo R Q,Huangpu J J.2016. Geological significance and characteristics of rare earth and trace elements from Upper Carboniferous Suogedangtawu Formation of the South of Wushi County in Northwestern Margin of Tarim Basin. Geoscience, 30(2): 426-435] [14] 王家生,刘本培,张传恒,周洪瑞. 1999. 南天山野云沟石炭系海底扇沉积新发现. 古地理学报, 1(3): 73-82. [Wang J S,Liu B P,Zhang C H,Zhou H R.1999. New discoveries of Carboniferous submarine fan sedimentation in Yeyungou of South Tianshan Mountain. Journal of Palaeogeography(Chinese Edition), 1(3): 73-82] [15] 王根长,刘朝安,熊剑飞. 1991. 新疆塔东北地区石炭、二叠纪沉积相. 见: 贾润胥. 中国塔里木盆地北部油气地质研究(第一辑,地层沉积).武汉:中国地质大学出版社,160-168. [Wang G C,Liu C A,Xiong J F.1991. Carboniferous and Permian sedimentary facies in the northeast of Xinjiang. In: Jia R X(ed.). Research of Petroleum Geology of Northern Tarim Basin in China. Stratigraphy ans Sedimentology(1).Wuhan: China University of Geosciences Press,160-168] [16] 王庆同,陈伟,马锦龙,杨宝忠,张新勇,阎琨,张维昕,柳晓丹. 2017. 新疆阿合奇县石炭系别根他乌组孢粉化石的发现及地质意义. 地质科技情报, 36(5): 1-6. [Wang Q T,Chen W,Ma J L,Yang Z B,Zhang X Y,Yan K,Zhang W X,Liu X D.2017. Discovery of sporopollen fossils of Carboniferous Biegentawu Formation in Aheqi,Xinjiang,and its paleoclimate significance. Geological Science and Technology Information, 36(5): 1-6] [17] 王松,李双应,杨栋栋,王道轩,李忠. 2011. 南天山大山口下石炭统野云沟组碳酸盐岩岩石学特征及沉积相分析. 地质科学, 46(2): 404-414. [Wang S,Li S Y,Yang D D,Wang D X,Li Z.2011. Characteristics of carbonate rocks and sedimentary facies analysis of the Lower Carboniferous Yeyungou Formation in Dashankou section,south Tianshan. Chinese Journal of Geology, 46(2): 404-414] [18] 王招明,夏维书,周黎霞,钟端,程华,赵培荣,梁向豪,冉体文. 2002. 塔里木盆地乌什凹陷及周边露头区油气地质 .北京: 石油工业出版社,1-225. [Wang Z M,Xia W S,Zhou L X,Zhong D,Cheng H,Zhao P R,Liang X H,Ran T W.2002. Petroleum Geology in Wushi Sag and Its Outcrop Area of the Tarim Basin. Beijing: Petroleum Industry Press,1-225] [19] 王宗秀,李春麟,Pak Nikolai,Ivleva Elena,余心起,周高誌,肖伟峰,韩淑琴,Halilov Zailabidin,Takenov Nurgazy,鄢犀利. 2017. 西天山造山带构造单元划分及古生代洋陆转换过程. 中国地质, 44(4): 623-641. [Wang Z X,Li C L,Pak Nikolai,Ivleva Elena,Yu X Q,Zhou G Z,Xiao W F,Han S Q,Halilov Zailabidin,Takenov Nurgazy,Yan X L.2017. Tectonic division and Paleozoic ocean-continent transition in Western Tianshan Orogen. Geology in China, 44(4): 623-641] [20] 吴根耀,李曰俊,刘亚雷,赵岩. 2013. 塔里木西北部乌什—柯坪—巴楚地区古生代沉积-构造演化及成盆动力学背景. 古地理学报, 15(2): 203-218. [Wu G Y,Li Y J,Liu Y L,Zhao Y.2013. Paleozoic Sedimento-tectonic evolution and basin dynamic settings in Wushi-Kalpin-Bachu area,northwest Tarim. Journal of Palaeogeography(Chinese Edition), 15(2): 203-218] [21] 吴浩若,李忠. 2013. 南天山洋古地理及构造演化: 西南天山放射虫硅质岩与地层记录的再认识. 古地理学报, 15(3): 293-304. [Wu H R,Li Z.2013. Palaeogeographic and tectonic evolution of South Tianshan Ocean: Re-examination of radiolarian cherts and stratigraphic record of southwestern Tianshan. Journal of Palaeogeography(Chinese Edition), 15(3): 293-304] [22] 杨克明,熊永旭,李晋光,先蓉有. 1992. 中国西北地区板块构造与盆地类型. 石油与天然气地质, 13(1): 47-56. [Yang K M,Xiong Y X,Li J G,Xian R Y.1992. Plate tectonic and basin types in Northwestern China. Oil & Gas Geology, 13(1): 47-56] [23] 杨树峰,陈汉林,厉子龙,励音骐,余星,李东旭,孟立丰. 2014. 塔里木早二叠世大火山岩省. 中国科学: 地球科学, 44(2): 187-199. [Yang S F,Chen H L,Li Z L,Li Y Q,Yu X,Li D X,Meng L F.2014. Early Permian Tarim large igneous province in northwest China. Science China: Earth Science, 44(2): 187-199] [24] 翟晓先,王根长,罗孝质. 1991.天山南缘石炭纪重力流沉积特征. 见：贾润胥. 中国塔里木盆地北部油气地质研究(第一辑,地层沉积). 武汉: 中国地质大学出版社,169-174. [Zhai X X,Wang G C,Luo X Z.1991. Characteristics of Carboniferous Gravity Flow Deposits in Southern Margin of Tianshan Mountains. In: Jia R X(ed.). Reaearch of Petroleum Geology of Northern Tarim Basin in China. Stratigraphy and Sedimentology(1). Wuhan: China University of Geosciences Press,169-174] [25] 张敬艺,罗金海,卿颖,曹远志,樊俊雷. 2007. 塔里木盆地西北缘石炭—二叠系浊积岩的沉积特征及其构造意义. 西北大学学报: 自然科学版, 37(5): 819-824. [Zhang J Y,Luo J H,Ting Y,Cao Y Z,Fan J L.2007. The sedimentary feature and structure significance of turbidite Carboniferous-Permian on the northwestern margin of the Tarim Basin. Journal of Northwest University(Natural Science Edition), 37(5): 819-824] [26] 张师本,倪寓南,龚福华,卢辉楠,黄智斌,林焕令,李猛,阮亦萍,杜品德,周志毅,谭泽金,赵治信,高琴琴,王智,张岩青,胡轩,赵恩宏,杨芝林, 2003. 塔里木盆地周缘地层考察指南. 北京: 石油工业出版社,1-280. [Zhang S B,Ni Y N,Gong F H,Lu H N,Huang Z B,Lin H L,Li M,Ruan Y P,Du P D,Zhou Z Y,Tan Z J,Zhao Z X,Gao Q Q,Wang Z,Zhang Y Q,Hu X,Zhao E H,Yang Z L.2003. A Guide to the Stratigraphic Investigation on the Periphery of the Tarim Basin. Beijing: Petroleum Industry Press,1-280] [27] 张新勇,刘晓煌,李保飞,张雄华,刘龙龙,牛树银,寇晓虎,杨宝忠. 2014. 新疆塔里木盆地哈拉奇地区晚石炭世—早二叠世哈拉奇组的建立. 地质通报, 33(1): 9-18. [Zhang X Y,Liu X H,Li B F,Zhang X H,Liu L L,Niu S Y,Kou X H,Yang B Z.2014. The establishment of the Late Carboniferous-Early Permian Karaqi Formation in Karaqi area on the northwestern margin of Tarim basin,Xinjiang. Geological Bulletin of China, 33(1): 9-18] [28] 张新勇,张雄华,赵志刚,戚静洁,钱春东,杨宝忠. 2017. 新疆阿合奇地区石炭系巴什索贡组珊瑚化石及其地质意义. 地质科技情报, 36(1): 14-19. [Zhang X Y,Zhang X H,Zhao Z G,Qin J J,Qian C D,Yang B Z.2017. Carboniferous Bashisuogong Formation coral fossils and their geological significances in Akqi Area,Xinjiang. Geological Science and Technology Information, 36(1): 14-19]
