Changes in sedimentary environments and provenances of the Carboniferous-Lower Permian strata in Ashelekuoerlesi area, West Junggar

SUN Hao; XU Yan; HAN Baofu; LIAO Wen; LI Ang; CHEN Chaoqiang; JIANG Shihao

2020 Vol. 39, No. 7

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SUN Hao, XU Yan, HAN Baofu, LIAO Wen, LI Ang, CHEN Chaoqiang, JIANG Shihao. Changes in sedimentary environments and provenances of the Carboniferous-Lower Permian strata in Ashelekuoerlesi area, West Junggar[J]. Geological Bulletin of China, 2020, 39(7): 963-982.

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SUN Hao, XU Yan, HAN Baofu, LIAO Wen, LI Ang, CHEN Chaoqiang, JIANG Shihao. Changes in sedimentary environments and provenances of the Carboniferous-Lower Permian strata in Ashelekuoerlesi area, West Junggar[J]. Geological Bulletin of China, 2020, 39(7): 963-982.

Changes in sedimentary environments and provenances of the Carboniferous-Lower Permian strata in Ashelekuoerlesi area, West Junggar

Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education/School of Earth and Space Science, Peking University, Beijing 100871, China

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Corresponding author: HAN Baofu, bfhan@pku.edu.cn

Received Date: 08 March 2020

Revised Date: 09 April 2020

Publish Date: 15 July 2020

Abstract

Abstract

In the Ashelekuoerlesi area, West Junggar, the Lower Carboniferous Jiangbasitao Formation unconformably overlies the Heishantou Formation and underlies the Lower Permian Haerjiawu Formation.The youngest detrital zircon clusters from three sandstone samples yielded U-Pb ages of 328 Ma (Serpukhovian Stage) for the top of the Heishantou Formation, 318 Ma (Bashkirian stage) for the bottom of the Jiangbasitao Formation and 297 Ma (Asselian stage) for the bottom of the Haerjiawu Formation, respectively.Therefore, the Jiangbasitao Formation is Late Carboniferous in age, rather than Early Carboniferous, and is equivalent to the Upper Carboniferous Molaoba Formation in the West Junggar area.The Heishantou Formation is a set of fossil-bearing marine deposits.The Molaoba Formation is a retrograding filling sequence from fan delta facies to shallow marine facies, but there is no preservation of the progressive filling sequence above, which may have resulted from the denudation after the tectonic uplift of the Junggar residual ocean basin in the Late Carboniferous.The Haerjiawu Formation is continental alluvial fan facies.The provenances of the Carboniferous and Lower Permian strata were confined to a neighboring area, and the youngest detrital zircons were derived from the contemporaneous volcanic rocks.
- West Junggar /
- Molaoba Formation /
- depositional environment /
- provenance analysis /
- residual ocean basin /
- detrital zircon

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References

[1]	Han B F, Guo Z J, Zhang Z C, et al.Age, geochemistry, and tectonic implications of a late Paleozoic stitching pluton in the North Tian Shan suture zone, western China[J].Geological Society of America Bulletin, 2010, 122(3/4):627-640. Google Scholar
[2]	Chen J F, Han B F, Zhang L, et al.Middle Paleozoic initial amalgamation and crustal growth in the West Junggar (NW China):Constraints from geochronology, geochemistry and Sr-Nd-Hf-Os isotopes of calc-alkaline and alkaline intrusions in the Xiemisitai-Saier Mountains[J].Journal of Asian Earth Sciences, 2015, 113:90-109. Google Scholar
[3]	Coleman R G.Continental growth of northwest China[J].Tectonics, 1989, 8(3):621-635. doi: 10.1029/TC008i003p00621 CrossRef Google Scholar
[4]	Xu Z, Han B F, Ren R, et al.Ultramafic-mafic mélange, island arc and post-collisional intrusions in the Mayile Mountain, West Junggar, China:Implications for Paleozoic intra-oceanic subduction-accretion process[J].Lithos, 2012, 132/133:141-161. Google Scholar
[5]	Ren R, Han B F, Xu Z, et al.When did the subduction first initiate in the southern Paleo-Asian Ocean:New constraints from a Cambrian intra-oceanic arc system in West Junggar, NW China[J].Earth and Planetary Science Letters, 2014, 388:222-236. Google Scholar
[6]	Liu B, Han B F, Chen J F, et al.Closure time of the Junggar-Balkhash Ocean:Constraints from Late Paleozoic volcano-sedimentary sequences in the Barleik Mountains, West Junggar, NW China[J].Tectonics, 2017, 36(12):2823-2845. doi: 10.1002/2017TC004606 CrossRef Google Scholar
[7]	朱宝清, 冯益民.新疆西准噶尔板块构造及演化[J].新疆地质, 1994, 12(2):91-105. Google Scholar
[8]	高睿, 肖龙, 王国灿, 等.西准噶尔晚古生代岩浆活动和构造背景[J].岩石学报, 2013, 29(10):3413-3434. Google Scholar
[9]	徐学义, 李荣社, 陈隽璐, 等.新疆北部古生代构造演化的几点认识[J].岩石学报, 2014, 30(6):1521-1534. Google Scholar
[10]	郭丽爽, 刘玉琳, 王政华, 等.西准噶尔包古图地区地层火山岩锆石LA-ICP-MS U-Pb年代学研究[J].岩石学报, 2010, 26(2):471-477. Google Scholar
[11]	Chen S, Guo Z, Pe-Piper G, et al.Late Paleozoic peperites in West Junggar, China, and how they constrain regional tectonic and palaeoenvironmental setting[J].Gondwana Research, 2013, 23(2):666-681. Google Scholar
[12]	纵瑞文, 龚一鸣, 王国灿.西准噶尔南部石炭纪地层层序及古地理演化[J].地学前缘, 2014, 21(2):216-233. Google Scholar
[13]	Feng Y, Coleman R G, Tilton G, et al.Tectonic evolution of the West Junggar Region, Xinjiang, China[J].Tectonics, 1989, 8(4):729-752. Google Scholar
[14]	Chen J F, Han BF, Ji J Q, et al.Zircon U-Pb age and tectonic implications of Paleozoic plutons in northern West Junggar, North Xinjiang, China[J].Lithos, 2010, 115:136-152. Google Scholar
[15]	Windley B F, Alexeiev D, Xiao W J, et al.Tectonic models for accretion of the Central Asian Orogenic Belt[J].Journal of the Geological Society of London, 2007, 164(12):31-47. Google Scholar
[16]	Shen P, Shen Y C, Li X H, et al.Northwestern Junggar Basin, Xiemisitai Mountains, China:A geochemical and geochronological approach[J].Lithos, 2012, 140/141:103-118. Google Scholar
[17]	Yang G X, Li Y J, Xiao W J, et al.Petrogenesis and tectonic implications of the middle Silurian volcanic rocks in northern West Junggar, NW China[J].International Geology Review, 2014, 56(7):869-884. Google Scholar
[18]	Xiao, W J, Han, C M, Yuan C, et al.Middle Cambrian to Permian subduction-related accretionary orogenesis of northern Xinjiang, NW China:implications for the tectonic evolution of Central Asia[J].Journal of Asian Earth Sciences, 2008, 32(2/4):102-117. Google Scholar
[19]	韩宝福, 郭召杰, 何国琦."钉合岩体"与新疆北部主要缝合带的形成时限[J].岩石学报, 2010, 26(8):2233-2246. Google Scholar
[20]	徐芹芹, 季建清, 龚俊峰, 等.新疆西准噶尔晚古生代以来构造样式与变形序列研究[J].岩石学报, 2009, 25(3):636-644. Google Scholar
[21]	Kwon S T, Tilton G R, Coleman R G, et al.Isotopic studies bearing on the tectonics of the West Junggar Region, Xinjiang, China[J].Tectonics, 1989, 8(4):719-727. Google Scholar
[22]	温志刚, 赵文平, 刘团锋, 等.新疆西准噶尔巴尔鲁克蛇绿岩形成时代及大地构造意义[J].地质通报, 2016, 35(9):1401-1410. Google Scholar
[23]	徐新, 何国琦, 李华芹, 等.克拉玛依蛇绿混杂岩带的基本特征和锆石SHRIMP年龄信息[J].中国地质, 2006, 33(3):470-476. Google Scholar
[24]	辜平阳.新疆西准噶尔达尔布特蛇绿岩研究[D].长安大学硕士学位论文, 2009.http://d.wanfangdata.com.cn/thesis/Y1527411 Google Scholar
[25]	Yang G, Li Y, Santosh M, et al.Geochronology and geochemistry of basalts from the Karamay ophiolitic mélange in West Junggar (NW China):Implications for Devonian-Carboniferous intra-oceanic accretionary tectonics of the southern Altaids[J].Bulletin of the Geological Society of America, 2013, 125(3/4):401-419. Google Scholar
[26]	韩宝福, 季建清, 宋彪, 等.新疆准噶尔晚古生代陆壳垂向生长(Ⅰ)——后碰撞深成岩浆活动的时限[J].岩石学报, 2006, 22(5):1077-1086. Google Scholar
[27]	Zheng B, Han B F, Liu B, et al.Ediacaran to Paleozoic magmatism in West Junggar Orogenic Belt, NW China, and implications for evolution of Central Asian Orogenic Belt[J].Lithos, 2019, 338:111-127. Google Scholar
[28]	Liu B, Han B F, Ren R, et al.Petrogenesis and tectonic implications of the Early Carboniferous to the Late Permian Barleik plutons in the West Junggar (NW China)[J].Lithos, 2017, 272:232-248. Google Scholar
[29]	白建科, 陈隽璐, 闫臻, 等.西准噶尔南部玛依勒洋盆开启、闭合时限:来自中泥盆统与下伏地质体之间角度不整合关系的证据[J].岩石学报, 2015, 31(1):133-142. Google Scholar
[30]	詹仁斌, 戎嘉余, 程金辉, 等.华南早-中奥陶世腕足动物多样性初探[J].中国科学(D辑), 2004, 34(10):896-907. Google Scholar
[31]	张志飞, 王妍, Christian C E.海豆芽——进化中的"活化石"[J].自然杂志, 2009, 31(4):201-203. Google Scholar
[32]	冯伟明, 刘建清, 林家善, 等.川东南古蔺曼岭寒武纪-奥陶纪之交的沉积环境演变[J].地质科技情报, 2016, 35(3):71-76. Google Scholar
[33]	薛良清, Galloway W E.扇三角洲, 辫状河三角洲与三角洲体系的分类[J].地质学报, 1991, 65(2):141-153. Google Scholar
[34]	王良忱, 张金亮.沉积环境和沉积相[M].北京:石油工业出版社, 1996:179-184. Google Scholar
[35]	古永红, 王振宇, 谭秀成.国内外扇三角洲研究综述[J].新疆石油地质, 2003, 24(6):590-593. Google Scholar
[36]	李永军, 金朝, 胡克亮, 等.西天山尼勒克北于赞一带下石炭统阿克沙克组扇三角洲相沉积的发现及意义[J].地质学报, 2010, 84(10):1470-1478. Google Scholar
[37]	Ludwig K R.User's manual for Isoplot 3.00:a geochronological toolkit for Microsoft Excel[J].Berkeley Geochronological Center, Special Publication, 2003, 4:25-32. Google Scholar
[38]	Dickinson W R, Gehrels G E.Use of U-Pb ages of detrital zircons to infer maximum depositional ages of strata:a test against a Colorado Plateau Mesozoic database[J].Earth and Planetary Science Letters, 2009, 288(1/2):115-125. Google Scholar
[39]	田陟贤, 李永军, 田猛, 等.西准噶尔恰达地区哈尔加乌组火山岩锆石U-Pb年代学、地球化学及地质意义[J].吉林大学学报:地球科学版, 2016, 46(1):135-145. Google Scholar
[40]	田陟贤, 阎军, 李永军, 等.西准噶尔巴尔雷克一带石炭系黑山头组火山岩LA-ICP-MS锆石U-Pb年龄、地球化学特征及构造环境[J].地质学报, 2013, 87(3):343-352. Google Scholar
[41]	沈锐, 李永军, 李钊, 等.西准噶尔巴尔努克富Nb岛弧玄武岩LA-ICP-MS锆石U-Pb年及意义[J].新疆地质, 2015, 33(4):428-432. Google Scholar
[42]	樊婷婷, 周小虎, 柳益群, 等.新疆大黑山东部姜巴斯套组下段的凝灰岩LA-ICP-MS U-Pb年龄及其地质意义[J].沉积学报, 2011, 29(2):312-320. Google Scholar
[43]	汪帮耀, 姜常义, 李永军, 等.新疆卡拉麦里姜巴斯套组火山岩地球化学特征与构造意义[J].地球科学与环境学报, 2011, 33(3):237-245. Google Scholar
[44]	刘博.新疆西准噶尔巴尔鲁克山古生代构造演化[D].北京大学博士学位论文, 2016. Google Scholar
[45]	Yi Z, Huang B, Xiao W, et al.Paleomagnetic study of Late Paleozoic rocks in the Tacheng Basin of West Junggar (NW China):Implications for the tectonic evolution of the western Altaids[J].Gondwana Research, 2015, 27(2):862-877. Google Scholar
[46]	任荣.新疆西准噶尔南西部古生代岩浆作用与洋内俯冲增生过程[D].北京大学博士学位论文, 2013.http://d.wanfangdata.com.cn/thesis/Y2500098 Google Scholar
[47]	邸晓辰, 舍建忠, 贾建.西准噶尔阿克布拉克地区晚泥盆世朱鲁木特组火山岩地球化学、锆石U-Pb年代学特征及地质意义[J].新疆地质, 2019, 37(1):1-6. Google Scholar
[48]	Choulet F, Cluzel D, Faure M, et al.New constraints on the pre-Permian continental crust growth of Central Asia (West Junggar, China) by U-Pb and Hf isotopic data from detrital zircon[J].Terra Nova, 2012, 24(3):189-198. Google Scholar
[49]	陈超强.新疆西准噶尔巴尔鲁克蛇绿岩沉积盖层碎屑锆石U-Pb年龄及其地质意义[D].北京大学学士学位论文, 2019.http://d.wanfangdata.com.cn/thesis/Y2500098 Google Scholar
[50]	Li D, He D, Qi X, et al.How was the Carboniferous Balkhash-West Junggar remnant ocean filled and closed? Insights from the Well Tacan-1 strata in the Tacheng Basin, NW China[J].Gondwana Research, 2015, 27(1):342-362. doi: 10.1016/j.gr.2013.10.003 CrossRef Google Scholar
[51]	李永军, 沈锐, 王冉, 等.新疆西准噶尔巴尔努克早石炭世富Nb岛弧玄武岩的发现及其地质意义[J].岩石学报, 2014, 30(12):3501-3511. Google Scholar
[52]	Xu Z, Han B F, Ren R, et al.Palaeozoic multiphase magmatism at Barleik Mountain, southern West Junggar, Northwest China:implications for tectonic evolution of the West Junggar[J].International Geology Review, 2013, 55(5):633-656. Google Scholar
[53]	Kuibida M L, Dyachkov B A, Vladimirov A G, et al.Contrasting granitic magmatism of the Kalba fold belt (East Kazakhstan):Evidence for Late Paleozoic post-orogenic events[J].Journal of Asian Earth Sciences, 2019, 175:178-198. Google Scholar
①	新疆维吾尔自治区地质调查院.1: 25万托里县幅(L44C003004)区域地质调查报告.2014. Google Scholar