Detrital zircon U-Pb age of the Kanas Group from the Friendship Peak region in northern Xinjiang and its implications for the tectonic evolution of the Altay Orogenic Belt

WANG Xing; LIN Xinwang; ZHANG Yafeng; ZHAO Duanchang; ZHAO Jianglin; WU Tong; LIU Kun

doi:10.12097/j.issn.1671-2552.2022.09.007

2022 Vol. 41, No. 9

Article Contents

Article navigation > Geological Bulletin of China > 2022 > 41(9): 1574-1588

Next Article Previous Article

WANG Xing, LIN Xinwang, ZHANG Yafeng, ZHAO Duanchang, ZHAO Jianglin, WU Tong, LIU Kun. Detrital zircon U-Pb age of the Kanas Group from the Friendship Peak region in northern Xinjiang and its implications for the tectonic evolution of the Altay Orogenic Belt[J]. Geological Bulletin of China, 2022, 41(9): 1574-1588. doi: 10.12097/j.issn.1671-2552.2022.09.007

Citation:

WANG Xing, LIN Xinwang, ZHANG Yafeng, ZHAO Duanchang, ZHAO Jianglin, WU Tong, LIU Kun. Detrital zircon U-Pb age of the Kanas Group from the Friendship Peak region in northern Xinjiang and its implications for the tectonic evolution of the Altay Orogenic Belt[J]. Geological Bulletin of China, 2022, 41(9): 1574-1588. doi: 10.12097/j.issn.1671-2552.2022.09.007

Detrital zircon U-Pb age of the Kanas Group from the Friendship Peak region in northern Xinjiang and its implications for the tectonic evolution of the Altay Orogenic Belt

1.
Shaanxi Mineral Resources and Geological Survey, Xi'an 710068, Shaanxi, China
2.
Shaanxi Institute of Geological Survey, Xi'an 710054, Shaanxi, China

Received Date: 12 December 2019

Revised Date: 10 November 2020

Publish Date: 15 September 2022

Abstract

Abstract

A large amount of geological information about the evolution, sedimentation and metamorphism of paleo-continental margin is retained in fragment sedimentary rocks from the Kanas Group, which is developed in the Friendship Peak region in the western section of the Altay Mountains, northern Xinjiang.The detrital zircon samples were collected in two rock formations for the study of isotopic dating.The results showed that the distribution characteristics of zircon U-Pb age in the two sets of clastic rocks were similar.The youngest magmatic zircon ages were 546±4 Ma and 545±4 Ma, respectively, which represents the lower limit of the sedimentary age.The relatively older zircon ages can be divided into three categories:3063±16 Ma, 2548±18 Ma and 2541±18 Ma in Archean Eon, 2223~1463 Ma in Paleo-Meso Proterozoic Era, 985~781 Ma in Neoproterozoic Era, which implies that the existence of Precambrian crystalline basement in the sediment source region.The relatively newer zircon age was 421~429 Ma, which is similar to the time of the strong magmatic activities in Altai region..It may be related to the stratum suffering from later hydrothermal deterioration events.The geological structure evolution in northern Xinjiang can be divided into five stages:the formation stage of the Archean continental nucleus, the formation and evolution stage of the Columbia supercontinent, the assembly and breakup stage of the Rodinia supercontinent, the deposition stage of Sinian-Cambrian flysch, the stage of severe magmatic activity in Caledonian.
- detrital zircon U-Pb age /
- Kanas Group /
- tectonic evolution /
- Altay Orogenic Belt /
- geological survey engineering /
- Northern Xinjiang

FullText(HTML)

References

[1]	丁建刚, 杨成栋, 杨富全, 等.新疆阿尔泰别也萨麻斯稀有金属矿床含矿伟晶岩与花岗岩围岩成因关系[J]. 地球科学与环境学报, 2022, 42(1):71-85. Google Scholar
[2]	蔺新望, 王星, 陈光庭, 等. 新疆北部阿尔泰山东段泥盆纪岩浆活动及侵位方式的探讨[J]. 现代地质, 2020, 34(3): 514-531. Google Scholar
[3]	蔺新望, 王星, 赵江林, 等. 新疆富蕴县北部金格岩体斜长花岗岩LA-ICP-MS锆石U-Pb同位素年龄及其地质意义[J]. 地质通报, 2019, 38(11): 1813-1824. doi: 10.12097/j.issn.1671-2552.2019.11.005 CrossRef Google Scholar
[4]	蔺新望, 张亚峰, 陈国超, 等. 阿尔泰造山带南缘岩浆混合作用: 阿克布拉克岩体岩石学、地球化学和年代学证据[J]. 地球科学, https://kns.cnki.net/kcms/detail/42.1874.P.20211214.1625.006.html. Google Scholar
[5]	仲正, 仝来喜, 刘兆, 等. 中国阿尔泰造山带的变形-变质历史研究: 以富蕴县乌恰沟地区为例[J]. 大地构造与成矿学, 2021, 45(4): 651-666. Google Scholar
[6]	谭晓淼, 高锐, 王海燕, 等. 中亚造山带东段深地震反射剖面大炮揭露下地壳与Moho结构: 数据处理与初步解释[J]. 吉林大学学报(地球科学版), 2021, 51(3): 898-908. Google Scholar
[7]	王登红, 陈毓川, 江彪, 等. 中国三叠纪大陆成矿体系[J]. 地学前缘, 2020, 27(2): 45-59. doi: 10.13745/j.esf.sf.2020.3.11 CrossRef Google Scholar
[8]	Wang T, Hong D W, Jahn B M, et al. Timing, Petrogenesis, and Setting of Paleozoic Synorogenic intrusions from the Altai Mountains, Northwest China: implications for the tectonic evolution of an accretionary Orogen[J]. Journal of Geology, 2006, 114: 735-751. doi: 10.1086/507617 CrossRef Google Scholar
[9]	王涛, 童英, 李舢, 等. 阿尔泰造山带花岗岩时空演变、构造环境及地壳生长意义——以中国阿尔泰为例[J]. 岩石矿物学杂志, 2010, 29(6): 595-618. doi: 10.3969/j.issn.1000-6524.2010.06.002 CrossRef Google Scholar
[10]	王星, 蔺新望, 赵端昌, 等. 阿尔泰北部喀纳斯群碎屑岩锆石U-Pb同位素年龄及其意义[J]. 西北地质, 2016, 49(3): 13-27. doi: 10.3969/j.issn.1009-6248.2016.03.002 CrossRef Google Scholar
[11]	王星, 蔺新望, 张亚峰, 等. 新疆北部阿尔泰山西段乞格拉塔乌岩体LA-ICP-MS锆石U-Pb同位素年龄及其地质意义[J]. 地质论评, 2019, 65(2): 370-385. Google Scholar
[12]	谢樊, 王海燕, 侯贺晟, 等. 中亚造山带东段浅表构造速度结构: 深地震反射剖面初至波层析成像的揭露[J]. 吉林大学学报(地球科学版), 2021, 51(2): 584-596. Google Scholar
[13]	徐扛, 舒坦, 孔令竹, 等. 中国阿尔泰造山带南缘晚古生代花岗岩脉年代学特征及构造意义[J]. 大地构造与成矿学, 2021, 45(3): 444-462. Google Scholar
[14]	徐芹芹, 季建清, 孙东霞, 等. 新疆阿尔泰青河—富蕴地区晚新生代隆升-剥露过程——来自磷灰石裂变径迹的证据[J]. 地质通报, 2015, 34(5): 834-844. doi: 10.3969/j.issn.1671-2552.2015.05.004 CrossRef Google Scholar
[15]	杨富全, 张志欣, 刘国仁, 等. 新疆中亚造山带三叠纪矿床地质特征、时空分布及找矿方向[J]. 矿床地质, 2020, 39(2): 197-214. Google Scholar
[16]	杨富全, 张忠利, 王蕊, 等. 新疆阿尔泰稀有金属矿地质特征及成矿作用[J]. 大地构造与成矿学, 2018, 42(6): 1010-1026. Google Scholar
[17]	杨硕, 刘阁, 靳刘圆, 等. 新疆东准噶尔地区老君庙岩群时代厘定、原岩恢复及对基底的指示意义[J]. 地质通报, 2020, 39(1): 7-17. Google Scholar
[18]	章享云, 王根厚, 赵军, 等. 阿尔泰乌希里克地区满克依顶萨依岩体地球化学特征、形成时代及其构造环境[J]. 地质通报, 2016, 35(8): 1376-1387. doi: 10.3969/j.issn.1671-2552.2016.08.017 CrossRef Google Scholar
[19]	张亚峰, 蔺新望, 赵玉梅, 等. 新疆北部青河县阿斯喀尔特铍矿区花岗质岩石年代学及地球化学特征[J]. 矿床地质, 2017, 36(3): 643-658. Google Scholar
[20]	张振龙, 杨富全, 李强, 等. 新疆阿尔泰阿舍勒铜锌矿床矿物学特征及其地质意义[J]. 矿床地质, 2020, 39(5): 905-925. Google Scholar
[21]	Windley B F, Krner A, Guo J H, et al. Neoproterozoic to paleozoic geology of the Altai orogen, NW China: new zircon age data and tectonic evolution[J]. The Journal of Geology, 2002, 110: 719-737. Google Scholar
[22]	Xiao W J, Windley B F, Badarch G, et al. Palaeozoic accretionary and convergent tectonics of the southern Altaids: implications for the growth of Central Asia[J]. Journal of the Geological Society, 2004, 161: 339-342. Google Scholar
[23]	何国琦, 韩宝福, 岳永君, 等. 中国阿尔泰造山带的构造分区和地壳演化[C]//新疆地质科学(第2辑), 北京: 地质出版社, 1990: 14-25. Google Scholar
[24]	胡霭琴, 韦刚健. 关于准噶尔盆地基底时代问题的讨论——据同位素年代学研究结果[J]. 新疆地质, 2003, 21(4): 398-406. Google Scholar
[25]	胡霭琴, 张国新, 李启新, 等. 新疆北部地质演化及其与成矿的关系[J]. 新疆地质, 1994, 12(1): 32-39. Google Scholar
[26]	胡霭琴, 张国新, 李启新, 等. 新疆北部主要地质事件同位素年[J]. 地球化学, 1995, 24(1): 20-31. Google Scholar
[27]	胡霭琴, 张国新, 张前锋, 等. 阿尔泰造山带变质岩系时代问题的讨论[J]. 地质科学, 2002, 37(2): 129-142. Google Scholar
[28]	李会军, 何国琦, 吴泰然, 等. 阿尔泰－蒙古微大陆的确定及其意义[J]. 岩石学报, 2006, 22(5): 1369-1379. Google Scholar
[29]	李锦轶, 肖序常. 对新疆地壳结构与构造演化几个问题的简要评述[J]. 地质科学, 1999, 34(4): 405-419. Google Scholar
[30]	李锦轶, 何国琦, 徐新, 等. 新疆北部及邻区地壳构造格架及其形成过程的初步探讨[J]. 地质学报, 2006, 80(1): 148-168. Google Scholar
[31]	李天德, B.H. 波里扬斯基. 中国和哈萨克斯坦阿尔泰大地构造及地壳演化[J]. 新疆地质, 2001, 19(1): 27-32. Google Scholar
[32]	宋国学, 秦克章, 刘铁兵, 等. 阿尔泰南缘阿舍勒盆地泥盆纪火山岩中古老锆石的U-Pb年龄、Hf同位素和稀土元素特征及其地质意义[J]. 岩石学报, 2010, 26(10): 2946-2958. Google Scholar
[33]	肖序常, 汤耀庆, 冯益民, 等. 新疆北部及其邻区大地构造[M]. 北京: 地质出版社, 1992: 1-171. Google Scholar
[34]	于根旺, 王伟, 赵越, 等. 阿尔泰递增变质带中夹层石英的LA-ICP-MS碎屑锆石U-Pb年龄: 对沉积时限及物源的限定[J]. 中国地质, 2016, 43(2): 500-510. Google Scholar
[35]	刘源, 杨家喜, 胡健民, 等. 阿尔泰构造带喀纳斯群时代的厘定及其意义[J]. 岩石学报, 2013, 29(3): 887-898. Google Scholar
[36]	王广耀, 张玉婷. 新疆阿尔泰震旦系的发现及其意义[J]. 中国区域地质, 1993, 7: 117-119. Google Scholar
[37]	龙晓平, 袁超, 孙敏, 等. 北疆阿尔泰南缘泥盆系浅变质碎屑沉积岩地球化学特征及其形成环境[J]. 岩石学报, 2008, 24(4): 718-732. Google Scholar
[38]	袁超, 孙敏, 龙晓平, 等. 阿尔泰哈巴河群的沉积时代及其构造背景[J]. 岩石学报, 2007, 23(7): 1635-1644. Google Scholar
[39]	Li J Y, Xiao W J, Wang K Z, et al. Neoproterozoec-Paleozoic tectonostratigraphy, magmatic activities and tectonic evolution of eastern Xinjian, N W China[C]//Mao J W, Goldfarb S, Wang X, et al. Tectonic Evolution and Metallogeny of the Chinese Altay and Tinanshan. IACOD Cuidebook Series, 2003, 10: 31-74. Google Scholar
[40]	Anderson T. Correction of common Pb in U-Pb analyses that do not report ²⁰⁴Pb[J]. Chemcal Geology, 2002, 192(1/2): 59-79. Google Scholar
[41]	Ludwig K R. Users Manual for Isoplot/Ex rex. 2.49, A Geochronological Toolkit for Microsoft Excel[M]. Berkeley Geochronology Center Special Publication, No. 1a, 2001: 1-51. Google Scholar
[42]	李艳广, 汪双双, 刘民武, 等. 斜锆石LA ICP MS U Pb定年方法及应用[J]. 地质学报, 2015, 89(12): 2400-2418. Google Scholar
[43]	李长民. 锆石成因矿物学与锆石微区定年综述[J]. 地质调查与研究, 2009, 33(3): 161-174. Google Scholar
[44]	吴元保, 郑永飞. 锆石成因矿物学研究及其对U-Pb年龄解释的制约[J]. 科学通报, 2004, 49(16): 1589-1604. Google Scholar
[45]	Cawood P A, Nemehin. A.A. Provenance record of a rift basin: U-Pb ages of detrital zircons from the Perth Basin, western Australia[J]. Sedimentray Geology, 2000, 134(3/4): 209-234. Google Scholar
[46]	Sireombe K N. Tracing provenance through the isotope ages of littoral and sedimentary detrital zircon, Eastern Australia[J]. Sedimentray Geology, 1999, 124(1/4): 47-67. Google Scholar
[47]	王少轶, 许虹, 杨晓平, 等. 大兴安岭北部中侏罗统漠河组砂岩LA-ICP-MS碎屑锆石U-Pb年龄: 对漠河盆地源区的制约[J]. 中国地质, 2015, 45(2): 1293-1302. Google Scholar
[48]	赵同阳, 朱志新, 韩琼, 等. 新疆阿尔泰山西段喀纳斯群碎屑锆石LA-ICP-MS U-Pb测年及地质意义[J]. 新疆地质, 2016, 34(1): 25-29. Google Scholar
[49]	方同辉, 王京彬, 张进红, 等. 新疆阿尔泰元古代基性岩浆侵入事件[J]. 中国地质, 2002, 29(1): 48-54. Google Scholar
[50]	牛贺才, 于学元, 许继峰, 等. 中国新疆阿尔泰晚古生代火山作用及成矿[M]. 北京: 地质出版社, 2006: 1-82. Google Scholar
①	陕西省地质调查院. 新疆阿尔泰1: 5万M45E018012等五幅区域地质矿产调查项目成果报告及附图. 2017. Google Scholar