新疆东天山卡拉塔格二叠纪火山岩成因及构造意义

doi:10.13278/j.cnki.jjuese.20200131

吉林大学学报(地球科学版) ›› 2021, Vol. 51 ›› Issue (4): 1119-1138.doi: 10.13278/j.cnki.jjuese.20200131

新疆东天山卡拉塔格二叠纪火山岩成因及构造意义

张雪¹, 翁凯², 赵晓健², 杜守礼³, 尚颖⁴

1. 长安大学地球科学与资源学院, 西安 710054;
2. 自然资源部岩浆作用成矿与找矿重点实验室/中国地质调查局西安地质调查中心, 西安 710054;
3. 中国石油长庆油田分公司勘探开发研究院, 西安 710018;
4. 中国地质科学院国家地质实验测试中心, 北京 100037

收稿日期:2020-06-01 出版日期:2021-07-26 发布日期:2021-08-02
通讯作者: 翁凯(1985-),男,副研究员,博士,主要从事矿物学、岩石学、矿床学方面的研究,E-mail:kaikaino1@qq.com E-mail:kaikaino1@qq.com
作者简介:张雪(1986-),女,工程师,博士,主要从事矿产普查与勘探方面的研究,E-mail:Xueer@chd.edu.cn
基金资助:
中央高校基本科研业务费资助项目（300102270110）；陕西省自然科学基金项目（2021JQ-329，2020JQ-440）；国家自然科学基金项目（41602236）

Permian Volcanic Rocks in Kalatage Area, Eastern Tianshan, Xinjiang: Petrogenesis and Tectonic Implications

Zhang Xue¹, Weng Kai², Zhao Xiaojian², Du Shouli³, Shang Ying⁴

1. School of Earth Science and Resources, Chang'an University, Xi'an 710054, China;
2. Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, MNR/Xi'an Center of Geological Survey, China Geological Survey, Xi'an 710054, China;
3. Research Institute of Exploration and Development, Changqing Oilfield Company, PetroChina, Xi'an 710018, China;
4. National Research Center for Geoanalysis, Chinese Academy of Geological Sciences, Beijing 100037, China

Received:2020-06-01 Online:2021-07-26 Published:2021-08-02
Supported by:
Supported by the Projects of Fundamental Research Funds of the Central Universities for Chang'an University (300102270110), the Natural Science Foundations of Shannxi Province,China (2021JQ-329,2020JQ-440) and the National Natural Science Foundation of China (41602236)

摘要/Abstract

摘要： 新疆东天山中北部的卡拉塔格地区广泛出露一套二叠纪陆相火山熔岩，本次对其采集的玄武岩和英安岩进行岩相学、锆石U-Pb定年、Lu-Hf同位素和岩石地球化学分析。年代学研究获得2个英安岩样品LA-ICP-MS锆石U-Pb加权平均年龄为（267.5±1.5）Ma和（296.7±1.7）Ma，代表了英安岩的结晶年龄为早二叠世。岩石地球化学数据显示：玄武岩为碱性系列，具有高Al₂O₃质量分数和Na₂O/K₂O值，低TFeO、Cr质量分数和Mg^#值的特征；微量元素Yb标准化的Ta、La和Nb值指示该区玄武质岩浆起源于富集型地幔；低La/Ba值，（Th/Nb）_N>1，Nb/La<1，表明岩浆在上升过程中受到了地壳岩石圈物质的混染；样品w（Zr）>100×10^-6，Zr/Y>5，显示大陆板内玄武岩特征。英安岩为钙碱性系列，富硅铝，Rb、Ba、Th、U、Zr等元素质量分数较高，Ti、Nb、Ta、Sr、P等元素质量分数较低，明显不同于玄武岩元素分布特征，却与地壳元素分布相似；ε_Hf（t）值（5.4~14.7）为正，表明英安岩源区为新生地壳；w（Rb）-w（Y+Nb）构造环境判别图解表明其形成于大陆伸展环境。结合前人的研究成果，认为卡拉塔格早二叠世火山岩形成于板内伸展环境，为天山石炭纪—二叠纪大火成岩省裂谷火山作用的组成部分，限定了该区古亚洲洋闭合于早二叠世之前。

关键词: 东天山, 二叠纪, 火山岩, 锆石U-Pb测年, 地球化学, 岩石成因

Abstract: The Kalatage area is located in the north central part of the Eastern Tianshan, where the Permian continental volcanic rocks are widely distributed. Their petrography, geochemistry, zircon U-Pb geochronology,and Lu-Hf isotope analysis for basalt and dacite are presented in this paper. The LA-ICP-MS zircon U-Pb dating of (267.5±1.5) Ma and (296.7±1.7) Ma from two dacite samples represents the crystallization age of dacite in the Early Permian. The geochemical data show that the basalt is of alkaline series with high Al₂O₃,Na₂O/K₂O, low TFeO, Mg^#, and Cr. The Ta, La, and Nb contents standardized by Yb indicate its basaltic magmatic origin from the enriched mantle source. The low La/Ba, (Th/Nb)_N>1 and Nb/La<1 suggest that the magma was mixed with lithospheric material during its ascent. The samples have w(Zr)>100×10^-6 and Zr/Y>5, indicating the characteristics of continental intraplate basalt. The dacite is of calc-alkaline type with enrichment of silicon and aluminum, high contents of Rb, Ba, Th, U, Zr, etc, and low content of Ti, Nb, Ta, Sr, P, etc. These features are obviously different from those of the basalt but similar to the crust. The dacite has positive ε_Hf(t) value (5.4-14.7), indicating that the source region is the new crust. The w(Y+Nb)-w(Rb) discrimination diagrams of tectonic setting show that the dacite was formed in the continental extensional setting. Combined with the previous research results, we believe that the Kalatage Early Permian volcanic rocks formed in the continental extensional setting, and they are part of the Carboniferous-Permian rift-related volcanism in Tianshan, which restricted the closure of Paleo-Asian Ocean in this area before the Early Permian.

Key words: Eastern Tianshan, Permian, volcanic rocks, zircon U-Pb dating, geochemistry, petrogenesis

中图分类号:

P581

张雪, 翁凯, 赵晓健, 杜守礼, 尚颖. 新疆东天山卡拉塔格二叠纪火山岩成因及构造意义[J]. 吉林大学学报(地球科学版), 2021, 51(4): 1119-1138.

Zhang Xue, Weng Kai, Zhao Xiaojian, Du Shouli, Shang Ying. Permian Volcanic Rocks in Kalatage Area, Eastern Tianshan, Xinjiang: Petrogenesis and Tectonic Implications[J]. Journal of Jilin University(Earth Science Edition), 2021, 51(4): 1119-1138.

参考文献

[1] Seng r A M C, Natal'in B A, Burtman V S. Evolution of the Altaid Tectonic Collage and Paleozoic Crustal Growth in Eurasia[J]. Nature, 1993, 364:299-307.
[2] 肖文交,宋东方,Windley B F, 等.中亚增生造山过程与成矿作用研究进展[J]. 中国科学:地球科学,2019, 49(10):1512-1545. Xiao Wenjiao,Song Dongfang,Windley B F,et al. Research Progresses of the Accretionary Processes and Metallogenesis of the Central Asian Orogenic Belt[J]. Science China:Earth Sciences, 2019, 49(10):1512-1545.
[3] Jahn B M,Windley B,Natal'in B, et al.Phanerozoic Continental Growth in Central Asia[J].Journal of Asian Earth Sciences, 2004, 23:599-603.
[4] 车自成,刘洪福,刘良,等.中天山造山带的形成与演化[M].北京:地质出版社,1994:1-135. Che Zicheng,Liu Hongfu,Liu Liang, et al. The Formation and Evolution of the Tianshan Orogenic Belt[M]. Beijing:Geological Publishing House, 1994:1-135.
[5] 夏林圻,夏祖春,徐学义,等. 天山石炭纪大火成岩省与地幔柱[J]. 地质通报,2004, 23(9/10):903-910. Xia Linqi,Xia Zhuchun,Xu Xueyi, et al.Carboniferous Tianshan Igneous Megaprovince and Mantle Plume[J]. Geological Bulletin of China, 2004, 23(9/10):903-910.
[6] 夏林圻,李向民,夏祖春,等. 天山石炭-二叠纪大火成岩省裂谷火山作用与地幔柱[J]. 西北地质,2006, 39(1):1-49. Xia Linqi,Li Xiangmin,Xia Zuchun,et al. Carboniferous-Permian Rift-Related Volcanism and Mantle Plume in the Tianshan, Northwestern China[J]. Northwestern Geology, 2006, 39(1):1-49.
[7] 徐学义,马中平,夏祖春,等. 天山石炭-二叠纪后碰撞花岗岩的Nd、Sr、Pb同位素源区示踪[J].西北地质,2005, 38(2):1-18. Xu Xueyi,Ma Zhongping,Xia Zuchun, et al. Discussion of the Sources and Characteristics on Sr, Nd, Pb Isotopes of the Carboniferous to Permian Post-Collision Granites from Tianshan[J].Northwestern Geology,2005, 38(2):1-18.
[8] Xiao Wenjiao,Zhang Liancheng,Qin Kezhang,et al. Paleozoic Accretionary and Collisional Tectonics of the Eastern Tianshan (China):Implications for the Continental Growth of Central Asia[J].American Journal of Science, 2004, 304:370-395.
[9] Xiao Wenjiao,Han Chunming,Yuan Chao, et al.Middle Cambrian to Permian Subduction-Related Accretionary Orogenesis of North Xinjiang, NW China:Implications for the Tectonic Evolution of Central Asia[J].Journal of Asian Earth Sciences, 2008, 32:102-117.
[10] 李曰俊,孙龙德,吴浩若,等. 南天山西端乌帕塔尔坎群发现石炭-二叠纪放射虫化石[J]. 地质科学,2005, 40(2):220-226. Li Yuejun,Sun Longde,Wu Haoruo,et al. Permo-Carboniferous Radiolaria from the Wupatarkan Group, West Terminal of Chinese South Tianshan[J]. Chinese Journal of Geology, 2005, 40(2):220-226.
[11] 李玮,陈隽璐,董云鹏,等. 早古生代古亚洲洋俯冲记录:来自东天山卡拉塔格高镁安山岩的年代学、地球化学证据[J]. 岩石学报,2016, 32(2):505-521. Li Wei,Chen Junlu, Dong Yunpeng, et al. Early Paleozoic Subduction of the Paleo-Asian Ocean:Zircon U-Pb Geochronological and Geochemical Evidence from the Kalatag High-Mg Andesites, East Tianshan[J].Acta Petrologica Sinica, 2016, 32(2):505-521.
[12] 李华芹,谢才富,常海亮,等.新疆北部有色贵金属矿床成矿作用年代学[M]. 北京:地质出版社,1998:1-264. Li Huaqin,Xie Caifu,Chang Hailiang,et al. Geochronology of Mineralization of Nonferrous Precious Metal Deposits in Northern Xinjiang[M].Beijing:Geological Publishing House, 1998:1-264.
[13] Mao Jingwen,Pirajno F,Zhang Zuoheng, et al. A Review of the Cu-Ni Sulphide Deposits in the Chinese Tianshan and Altay Orogens (Xinjiang Autonomous Region, NW China):Principal Characteristics and Ore-Forming Processes[J].Journal of Asian Earth Sciences,2008, 32(2/3/4):184-203.
[14] Yuan Chao,Sun Min,Wilde S, et al.Post-Collisional Plutons in the Balikun Area,East Chinese Tianshan:Evolving Magmatism in Response to Extension and Slab Break-Off[J].Lithos, 2010, 119(3/4):269-288.
[15] 顾连兴,胡受奚,于春水,等. 博格达陆内碰撞造山带挤压-拉张构造转折期的侵入活动[J].岩石学报,2001, 17(2):187-198. Gu Lianxing, Hu Shouxi, Yu Chunshui, et al.Intrusive Activities During Compression-Extension Tectonic Conversion in the Bogda Intrascontinental Orogen[J]. Acta Petrologica Sinica, 2001, 17(2):187-198.
[16] 秦克章,孙枢,陈海泓,等.新疆北部金属矿床时空分布格局-古生代多岛海型碰撞造山带的标志[C]//陈海泓,侯泉林,肖文交.中国碰撞造山带研究.北京:海洋出版社,1999:183-196. Qin Kezhang,Sun Shu,Chen Haihong, et al. Temporal and Spatial Distribution Pattern of Metal Deposits in Northern Xinjiang:A Sign of Paleozoic Multi Island Sea Collision Orogenic Belt[C]//Chen Haihong, Hou Quanlin, Xiao Wenjiao. A Study of Collisional Orogenic Belts in China.Beijing:Oceanic Publishing House,1999:183-196.
[17] 涂光炽. 初议中亚成矿域[J]. 地质科学,1999, 34(4):397-404. Tu Guangzhi.A Preliminary Discussion on the Metallogenic Domain of Central Asia[J].Scientia Geologica Sinica, 1999, 34(4):397-404.
[18] 朱永峰,何国琦,安芳. 中亚成矿域核心地区地质演化与成矿规律[J]. 地质通报,2007, 26(9):1167-1177. Zhu Yongfeng,He Guoqi, An Fang. Geological Evolution and Metallogeny in the Core Part of the Central Asian Metallogenic Domain[J].Geological Bulletin of China, 2007, 26(9):1167-1177.
[19] 王京彬,王玉往,何志军. 东天山大地构造演化的成矿示踪[J]. 中国地质,2006, 33(3):461-469. Wang Jingbin,Wang Yuwang,He Zhijun. Ore Deposits as a Guide to the Tectonic Evolution in the East Tianshan Mountains, NW China[J].Chinese Geoglogy, 2006, 33(3):461-469.
[20] Qin Kezhang,Su Benxun,Sakyi P A, et al. SIMS Zircon U-Pb Geochronology and Sr-Nd Isotopes of Ni-Cu-Bearing Mafic-Ultramafic Intrusions in Eastern Tianshan and Beishan in Correlation with Flood Basalts in Tarim Basin (NW China):Constraints on a ca.280 Ma Mantle Plume[J].American Journal of Science, 2011, 311(3):237-260.
[21] 龙灵利,王京彬,王玉往,等. 东天山卡拉塔格矿集区赋矿火山岩地层时代探讨:SHRIMP锆石U-Pb年龄证据[J].矿产勘查,2016, 7(1):30-37. Long Lingli, Wang Jingbin, Wang Yuwang, et al. Discussion on the Age of Ore-Host Volcanic Strata in the Kalatage Ore Concentration Area, Eastern Tianshan:Evidence from SHRIMP Zircon U-Pb Dating[J]. Mineral Exploration, 2016, 7(1):30-37.
[22] 毛启贵,方同辉,王京彬,等. 东天山卡拉塔格早古生代红海块状硫化物矿床精确定年及其地质意义[J]. 岩石学报,2010, 26(10):3017-3026. Mao Qigui,Fang Tonghui,Wang Jingbin,et al. Geochronology Studies of the Early Paleozoic Honghai Massive Sulfide Deposits and Its Geological Significance in Kalatage Area, Eastern Tianshan Mountain[J]. Acta Petrologica Sinica, 2010, 26(10):3017-3026.
[23] 王福同,冯京,胡建卫,等.新疆土屋大型斑岩铜矿床特征及发现意义[J]. 中国地质,2001, 28(1):36-39. Wang Futong,Feng Jing,Hu Jianwei, et al. Characteristics and Discovery Significance of Tuwu Large Porphyry Copper Deposit in Xinjiang[J].Chinese Geoglogy,2001, 28(1):36-39.
[24] 高珍权,方维萱,胡瑞忠,等. 新疆东天山卡拉塔格斑岩型铜(金)矿成矿地质背景与找矿评价[J].地质学报,2006, 80(1):90-100. Gao Zhenquan,Fang Weixuan,Hu Ruizhong,et al.The Metallogenic Environment of Kalatage Prophyry Copper (Gold) Deposit and Its Prospecting Perspective, Xinjiang, China[J]. Acta Geologica Sinica, 2006, 80(1):90-100.
[25] 毛启贵,王京彬,方同辉,等. 新疆东天山卡拉塔格地区中泥盆世玉带斑岩铜(金)矿发现的地质找矿意义[J]. 地质与勘探,2017, 53(1):1-11. Mao Qigui,Wang Jingbin, Fang Tonghui, et al. Discovery of the Middle Devonian Yudai Porphyric Cu (Au) Deposit in the Kalatage Area of Eastern Tianshan Mountain, Xinjiang and Its Geological Prospecting Significance[J]. Geology and Exploration, 2017, 53(1):1-11.
[26] 秦克章,方同辉,王书来,等. 吐哈盆地南缘古生代"天窗"卡拉塔格铜金矿化区的发现及其成矿潜力[J]. 中国地质,2001, 28(3):16-23. Qin Kezhang,Fang Tonghui,Wang Shulai,et al. Discovery and Metallogenic Potential of Paleozoic "Skylight" Kalatage Copper Gold Mineralization Area in the Southern Margin of Turpan Hami Basin[J]. Chinese Geoglogy, 2001, 28(3):16-23.
[27] 姜晓,郭勇明,杨良哲,等. 哈密沙东大型钨矿床地质特征及成因探讨[J]. 新疆地质,2012, 30(1):31-35. Jiang Xiao,Guo Yongming,Yang Liangzhe,et al. Geological Characteristics and Preliminary Origin of Shadong Large Tungsten Deposit in Hami, Xinjiang[J]. Xinjiang Geology, 2012, 30(1):31-35.
[28] 陈超,吕新彪,吴春明,等. 新疆库米什地区钨矿成矿远景探讨[J]. 矿床地质,2013, 32(3):579-590. Chen Chao, Lü Xinbiao, Wu Chunming, et al. A Prospective Analysis of Tungsten Mineralization in Kumux Area, Xinjiang[J]. Mineral Deposits, 2013, 32(3):579-590.
[29] 于明杰,王京彬,毛启贵,等. 新疆东天山卡拉塔格矿集区梅岭铜锌(金)矿床成矿流体特征及地质意义[J]. 矿床地质,2016, 35(4):829-845. Yu Mingjie, Wang Jingbin, Mao Qigui, et al. Characteristics of Ore-Forming Fluids of Meiling Copper-Zinc (Gold) Deposit in Kalatage Ore Concentration Area of East Tianshan Mountains, Xinjiang, and Their Geological Significance[J].Mineral Deposits, 2016, 35(4):829-845.
[30] 方同辉,秦克章,王书来,等. 浅析卡拉塔格铜金矿成矿地质背景[J].矿床地质,2002, 21(增刊1):380-383. Fang Tonghui, Qin Kezhang, Wang Shulai, et al. Elementary Analysis of Geological Background of Kalatage Copper and Gold Deposit[J]. Mineral Deposits, 2002, 21(Sup.1):380-383.
[31] Jackson S E, Pearson N J, Griffin W L, et al. Belousova the Application of Laser Ablation Inductively Coupled Plasma-Mass Spectrometry to in Situ U-Pb Zircon Geochronology[J].Chemical Geology, 2004, 211(1/2):47-69.
[32] 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. Li Yanguang, Wang Shuangshuang, Liu Minwu, et al. U-Pb Dating Study of Baddeleyite by LA-ICP-MS Technique and Application[J].Acta Geologica Sinica, 2015, 89(12):2400-2418.
[33] Chombong N N, Suh E C, Ilouga C D C. New Detrital Zircon U-Pb Ages from BIF-Related Metasediments in the Ntem Complex (Congo Craton) of Southern Cameroon, West Africa[J]. Natural Science, 2013, 5(7):835-847.
[34] 侯可军,李延河,邹天人,等. LA-MC-ICP-MS锆石Hf同位素的分析方法及地质应用[J].岩石学报,2007, 23(10):2595-2604. Hou Kejun, Li Yanhe, Zou Tianren, et al. Laser Ablation-MC-ICP-MS Technique for Hf Isotope Microanalysis of Zircon and Its Geological Applications[J]. Acta Petrologica Sinica, 2007, 23(10):2595-2604.
[35] Sun S S, McDonough W F. Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes[C]//Saunders A D, Norry M J. Magmatism in the Ocean Basins.London:Special Publication, 1989:313-345.
[36] Wendlandt R F, Altherr R, Neumann E R, et al. Petrology, Geochemistry, Isotopes[M]. Amsterdam:Elsevier, 1995:47-60.
[37] Macdonald R, Hawkesworth C J, Heath E.The Lesser Antilles Volcanic Chain:A Study in Arc Magmatism[J]. Earth Science Reviews, 2000, 49:1-76.
[38] 夏林圻,夏祖春,徐学义,等.利用地球化学方法判别大陆玄武岩和岛弧玄武岩[J].岩石矿物学杂志,2007, 26(1):77-89. Xia Linqi,Xia Zuchun,Xu Xueyi,et al.The Discrimination Between Continental Basaltand Island Arc Basalt Based on Geochemical Method[J].Acta Petrologica et Mineralogica, 2007, 26(1):77-89.
[39] Wilson M. Igneous Petrogenesis[M]. London:Unwin Hyman, 1989:1-464.
[40] Thompson R N, Morrison M A, Hendry G L, et al. An Assessment of the Relative Roles of a Crust and Mantle in Magma Genesis:An Elemental Approach[J]. Philosophical Transactions of the Royal Society of London, 1984, A310:549-590.
[41] Rudnick R L, Gao Shan. Composition of the Continental Crust[J]. Treatise Geochem, 2003, 3(1):1-64.
[42] 车自成,刘良,刘洪福,等.论伊犁古裂谷[J].岩石学报,1996, 12(3):478-489. Che Zicheng, Liu Liang, Liu Hongfu, et al. Review on the Ancient Yili Rift,Xinjiang,China[J].Acta Petrologica Sinica, 1996, 12(3):478-489.
[43] 陈丹玲,刘良,车自成,等.中天山骆驼沟火山岩的岩石地球化学特征及其构造环境[J].岩石学报,2001, 17(3):378-384. Chen Danling,Liu Liang,Che Zicheng, et al. Geochemical Characteristics and Tectonic Implication of Carboniferous Volcanites in the Luotuogou Area of Middle Tianshan[J]. Acta Petrologica Sinica, 2001, 17(3):378-384.
[44] 顾连兴,胡受奚,于春水,等.论博格达俯冲撕裂型裂谷的形成与演化[J].岩石学报,2001, 17(4):585-597. Gu Lianxing, Hu Shouxi, Yu Chunshui, et al. Initiation and Evolution of the Bogda Subduction-Torn-Type Rift[J]. Acta Petrologica Sinica, 2001, 17(4):585-597.
[45] 夏林圻,夏祖春,徐学义,等. 天山古生代洋陆转化特点的几点思考[J]. 西北地质,2002, 35(4):9-20. Xia Linqi, Xia Zuchun, Xu Xueyi, et al. Some Thoughts on the Characteristics of Paleozoic Ocean-Continent Transition from Tianshan Mountains[J].Northwestern Geology, 2002, 35(4):9-20.
[46] Xia Linqi, Xu Xueyi, Xia Zuchun, et al.Carboniferous Post-Collisional Rift Volcanism of the Tianshan Mountains, Northwestern China[J].Acta Geologica Sinica, 2003, 77(3):338-360.
[47] Xia Linqi, Xu Xueyi, Xia Zuchun, et al. Petrogenesis of Carboniferous Rift-Related Volcanic Rocks in the Tianshan, Northwestern China[J]. Geological Society of America Bulletin, 2004, 116(3):419-433.
[48] 罗婷,陈继平,廖群安,等. 东天山巴里坤地区晚石炭世双峰式火山岩年代学、地球化学及其构造意义[J]. 地球科学,2018, 43(9):3018-3035. Luo Ting, Chen Jiping, Liao Qun'an, et al. Geochronology, Geochemistry and Geological Significance of the Late Carboniferous Bimodal Volcanic Rocks in the Balikun Area,Eastern Tianshan[J]. Earth Science, 2018, 43(9):3018-3035.
[49] 陈根文,邓腾,刘睿,等.西天山阿吾拉勒地区二叠系塔尔得套组双峰式火山岩地球化学研究[J].岩石学报,2015, 31(1):105-118. Chen Genwen, Deng Teng, Liu Rui, et al. Geochemistry of Bimodal Volcanic Rocks in Permian Taerdetao Formation in Awulale Area of Western Tianshan, Xinjiang[J]. Acta Petrologica Sinica,2015,31(1):105-118.
[50] 葛海龙,张艳,王圣柱,等. 西准噶尔萨吾尔地区吉木乃组火山岩锆石U-Pb年代学、地球化学特征及构造背景[J].吉林大学学报(地球科学版),2020, 50(4):1075-1089. Ge Hailong, Zhang Yan, Wang Shengzhu, et al. Zircon U-Pb Age, Geochemical Characteristics and Tectonic Settings of Volcanic Rocks in Jimunai Formation,West Junggar Basin[J].Journal of Jilin University(Earth Science Edition), 2020, 50(4):1075-1089.
[51] 陈维民,尚海军.东天山大南湖阿克塔格晚石炭世A型花岗岩的确定及其地质意义[J].岩石矿物学杂志,2015, 34(2):159-170. Chen Weimin, Shang Haijun. Recognition of the Late Carboniferous Dananhu Aketag A-Type Granite from the Eastern Tianshan Mountains and Its Implications[J]. Acta Petrologica et Mineralogica, 2015, 34(2):159-170.
[52] 余吉远,孟勇,李建星,等.东天山阿拉塔格花岗岩体地球化学特征及其构造意义[J].吉林大学学报(地球科学版),2013, 43(3):765-775. Yu Jiyuan, Meng Yong, Li Jianxing, et al. Geochemical Characteristics and Tectonic Significance of Granitoid Rock in Alatage, Eastern Tianshan[J]. Journal of Jilin University (Earth Science Edition), 2013, 43(3):765-775.
[53] 殷绍泉,张保科.西准噶尔北部比图岩体的地球化学特征及构造环境[J].世界地质,2017, 36(3):682-690. Yin Shaoquan, Zhang Baoke. Geochemical Characteristics and Tectonic Setting of Bitu Complex in Northern West Junggar[J]. Global Geology, 2017, 36(3):682-690.
[54] 于介禄,于介江,杨万志,等.东天山觉罗塔格带东段早志留世中酸性侵入岩的年代学、地球化学及构造意义[J].吉林大学学报(地球科学版),2019, 49(3):690-708. Yu Jielu, Yu Jiejiang, Yang Wanzhi, et al. Geochronology, Geochemistry and Tectonic Implications of Early Silurian Intermediate-Acid Intrusive Rocks in East of Jueluotage Belt,Eastern Tianshan[J]. Journal of Jilin University (Earth Science Edition), 2019, 49(3):690-708.

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新疆东天山卡拉塔格二叠纪火山岩成因及构造意义

Permian Volcanic Rocks in Kalatage Area, Eastern Tianshan, Xinjiang: Petrogenesis and Tectonic Implications

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