吉林大学学报(地球科学版) ›› 2018, Vol. 48 ›› Issue (4): 1105-1120.doi: 10.13278/j.cnki.jjuese.20170303

• 地质与资源 • 上一篇    下一篇

东天山觉罗塔格带黄山地区角闪辉长岩岩体的年代学、地球化学特征及岩石成因

崔亚川1, 于介江1, 杨万志2, 张元厚1, 崔策1, 于介禄1   

  1. 1. 吉林大学地球科学学院, 长春 130061;
    2. 新疆维吾尔自治区地质调查院, 乌鲁木齐 830000
  • 收稿日期:2017-12-21 出版日期:2018-07-26 发布日期:2018-07-26
  • 通讯作者: 于介江(1961-),男,教授,博士,主要从事火成岩岩石学方面的研究,E-mail:yujiejiang@jlu.edu.cn E-mail:yujiejiang@jlu.edu.cn
  • 作者简介:崔亚川(1990-),男,硕士研究生,主要从事火成岩岩石学方面的研究,E-mail:347978034@qq.com
  • 基金资助:
    国家自然科学基金项目（3A416AP74422）；新疆维吾尔自治区地质勘察基金管理中心项目（Y14-5-LQ05）

Geochronology, Geochemistry and Petrogenesis of Hornblende Gabbro in Huangshan Area of Jueluotage Belt, Eastern Tianshan

Cui Yachuan1, Yu Jiejiang1, Yang Wanzhi2, Zhang Yuanhou1, Cui Ce1, Yu Jielu1   

  1. 1. College of Earth Sciences, Jilin University, Changchun 130061, China;
    2. Geological Survey Institute in Xinjiang Autonomous Region, Urumqi 830000, China
  • Received:2017-12-21 Online:2018-07-26 Published:2018-07-26
  • Supported by:
    Supported by National Natural Science Foundation of China (3A416AP74422) and Xinjiang Uygur Autonomous Region Geological Survey Fund Management Center(Y14-5-LQ05)

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摘要： 为了确定东天山觉罗塔格带黄山地区单一的角闪辉长岩岩体的形成时代、源区性质及其构造属性，本文对东天山觉罗塔格带黄山地区早二叠世角闪辉长岩岩体进行了系统的LA-ICP-MS锆石U-Pb定年与地球化学分析。结果表明：2个岩体中的锆石在CL图像上主要呈条痕状吸收，Th/U值较高（0.23~0.58），指示其岩浆成因，成岩年龄为早二叠世（281.1~282.3 Ma）。这些岩体均由单一的角闪辉长岩构成，w（SiO2）为46.45%~52.76%，w（MgO）为5.15%~8.42%，w（Al2O3）为14.52%~16.84%，Mg#主要为0.55~0.63；稀土元素配分模式呈右倾型，LREE/HREE=3.36~5.11，（La/Yb）N=2.64~4.41，δEu值多为1.06~1.98；在微量元素蛛网图上，Rb、Ba、K、Sr等大离子亲石元素相对富集，高场强元素Nb、Ta及Zr、P、Hf相对亏损；εNd（t）=10.66~12.54（t=282 Ma），平均为11.60。综上所述，东天山觉罗塔格带黄山地区早二叠世角闪辉长岩的岩浆源区主要为受俯冲流体交代的亏损地幔楔。结合同时代火成岩的组合特征、沉积作用以及区域构造演化历史，认为东天山觉罗塔格带黄山地区早二叠世角闪辉长岩体形成于吐哈地块与中天山地块碰撞后的伸展背景。

关键词: 东天山觉罗塔格带, 黄山, 早二叠世, 角闪辉长岩, 年代学, 地球化学, 岩石成因

Abstract: Many ore-bearing complexes in Huangshan area of Jueluotage belt in eastern Tianshan become hot spots in recent years. This study focused on the hornblende-gabbro plutons in the area to obtain the formation age, source region of the magma and tectonic implications of the hornblende-gabbro plutons. The research result showed that the selected zircons of two plutons exhibit striped absorption in cathodoluminescence (CL) images, and have high Th/U ratios (0.23-0.58), implying a magmatic origin. The zircon U-Pb dates indicated that they formed in the Early Permian (281.1-282.3 Ma), representing the emplacement age of these plutons. These plutons are composed of the single hornblende gabbro, with w(SiO2)=46.45%-52.76%, w(MgO)=5.15%-8.42%, w(Al2O3)=14.52%-16.84%, and Mg#=0.55-0.63. The rare earth element distribution patterns display as right-leaning, with LREE/HREE=3.36-5.11, (La/Yb)N=2.64-4.41, δEu=1.06-1.98, and the trace element spider diagrams showed that they are enriched in LILE (Rb, Ba, K and Sr), moderately depleted of HFSE (Nb, Ta, Zr, P and Hf), and εNd(t)=10.66-12.54(t=282 Ma),at average of 11.60. The results suggest that the Early Permian hornblende-gabbro in the area was from the partial melting of a depleted mantle wedge metasomatized by the fluid released from a subducted slab. Combining with the composition features, sedimentation and tectonic implications of the volcanic rocks, the Early Permian hornblende-gabbro was formed in post-collisional crust extension setting of the Tuha and central Tianshan blocks.

Key words: Jueluotage belt eastern Tianshan, Huangshan, Early Permian, hornblende-gabbro, geochronology, geochemistry, petrogenesis

中图分类号: 

  • P588.1
[1] Xiao W J, Santosh M. The Western Central Asian Orogenic Belt:A Window to Accretionary Orogenesis and Continental Growth[J]. Gondwana Research, 2014, 25:1429-1444.
[2] Li J Y. Peimian Geodynamic Setting of Northeast China and Adjacent Regions:Closure of the Paleo-Asian Ocean and Subduction of the Paleo-Pacific Plate[J]. Journal of Asian Earth Sciences, 2006, 26:207-224.
[3] Xu W L, Ji W Q, Pei F P,et al. Triassic Volcanism in Eastern Heilongjiang and Jilin Provinces, NE China:Chronology, Geochemistry, and Tectonic Implications[J]. Journal of Asian Earth Sciences, 2009, 34:392-402.
[4] Wu F Y, Sun D Y, Ge W C, et al. Geochronology of the Phanerozoic Granitoids in Northeastern China[J]. Journal of Asian Earth Sciences, 2011, 41:1-30.
[5] Han B F, He G Q, Wang X C, et al. Late Carbo-niferous Collision Between the Tarim and Kazakhstan-Yili Terranes in the Western Segment of the South Tian Shan Orogen, Central Asia, and Implications for the North Xinjiang, Western China[J]. Earth-Science Reviews, 2011, 109:74-93.
[6] 肖序常. 新疆北部及邻区大地构造[M]. 北京:地质出版社,1992:1-169. Xiao Xuchang. Tectionic Evolution of Northern Xinjiang and Its Adjacent Regions[M]. Beijing:Geological Publishing House, 1992:1-169.
[7] 马瑞士. 东天山构造格架及地壳演化[M]. 南京:南京大学出版社,1993:1-225. Ma Ruishi. Tectonic Framework and Crustal Evolution of Eastern Tianshan Mountains[M]. Nanjing:Nanjing University Press, 1993:1-225.
[8] 周济元,崔炳芳,肖惠良,等. 新疆康古尔-黄山对接碰撞带的存在、成矿模式及成矿预测[J]. 火山地质与矿产,2001,22(4):252-263. Zhou Jiyuan, Cui Bingfang, Xiao Huiliang, et al. Kangguertag-Huangshan Collision Zone of Bilateral Subduction and Its Metallogenic Model and Prognosis in Xinjiang, China[J]. Volcanology & Mineral Resources, 2001, 22(4):252-263.
[9] 秦克章,方同辉,王书来,等. 东天山板块构造分区、演化与成矿地质背景研究[J].新疆地质,2002,20(4):302-308. Qin Kezhang, Fang Tonghui, Wang Shulai, et al. Plate Tectonics Division, Evolution and Metallogenic Settings in Eastern Tianshan Mountains, NW-China[J]. Xinjiang Geology, 2002, 20(4):302-308.
[10] 李锦轶. 新疆东部新元古代晚期和古生代构造格局及其演化[J].地质论评,2004,50(3):304-322. Li Jinyi. Late Neoproterozoic and Paleozoic Tectonic Framework and Evolution of Eastern Xinjiang, NW-China[J]. Geological Review, 2004, 50(3):304-322.
[11] 李锦轶,宋彪,王克卓,等. 东天山吐哈盆地南缘二叠纪幔源岩浆杂岩:中亚地区陆壳垂向增生的地质记录[J]. 地球学报,2006,27(5):424-446. Li Jinyi, Song Biao, Wang Kezhuo, et al. Permian Mafic-Ultramafic Complexes on the Southern Margin of the Tu-Ha Basin, East Tianshan Mountains:Geological Records of Vertical Crustal Growth in Central Asia[J]. Acta Geoscientica Sinica, 2006, 27(5):424-446.
[12] 夏明哲,姜常义,钱壮志,等. 新疆东天山黄山东岩体岩石地球化学特征与岩石成因[J]. 岩石学报,2010,26(8):2413-2430. Xia Mingzhe, Jiang Changyi, Qian Zhuangzhi, et al. Geochemistry and Petrogenesis of Huangshandong Intrusion, East Tianshan, Xinjiang[J]. Acta Petroloica Sinica, 2010, 26(8):2413-2430.
[13] Wu Y S, Zhou K F, Li N, et al. Zircon U-Pb Dating and Sr-Nd-Pb-Hf Isotopes of the Ore-Associated Porphyry at the Giant Donggebi Mo Deposit, Eastern Tianshan, NW China[J]. Ore Geology Reviews, 2017, 81(2):794-807.
[14] 毛亚晶,秦克章,唐冬梅,等. 东天山岩浆铜镍硫化物矿床的多期次岩浆侵位与成矿作用:以黄山铜镍矿床为例[J]. 岩石学报,2014,30(6):1575-1594. Mao Yajing, Qin Kezhang, Tang Dongmei, et al. Multiple Stages of Magma Emplacement and Mineralization of Eastern Tianshan, Xinjiang:Examplified by Huangshan Ni-Cu Deposit[J]. Acta Petrologica Sinica, 2014, 30(6):1575-1594.
[15] Deng Y F, Song X Y, Chen L M, et al. Geoche-mistry of the Huangshandong Ni-Cu Deposit in Northwestern China:Implications for the Formation of Magmatic Sulfide Mineralization in Orogenic Belts[J]. Ore Geology Reviews, 2014, 56:181-198.
[16] 方国庆. 新疆东部大地构造特点及演化[J]. 西北地质,1991,12(3):6-11. Fang Guoqing. Tectonic Features and Evolution of Eastern Xinjiang[J]. Northwestern Geology, 1991, 12(3):6-11.
[17] 白云来. 新疆黄山地区蛇绿岩块的地质、地球化学特征及构造意义[J]. 新疆地质,1993,11(1):34-42. Bai Yunlai. Geologocal-Geochemical Characteristics and Tectonic Significance of the Ophiolites Block in Huangshan Area, Xinjiang[J]. Xinjiang Geology, 1993, 11(1):34-42.
[18] 白云来. 新疆哈密黄山-镜儿泉镍铜成矿系统的地质构造背景[J]. 甘肃地质学报,2000,9(2):1-7. Bai Yunlai. Geotectonic Settings of Huangshan-Jingerquan Nickel-Copper Metallogenic System in Hami, Xinjiang[J]. Acta Geologica Gansu, 2000, 9(2):1-7.
[19] 刘德权,唐延龄,周汝洪. 新疆北部古生代地壳演化及成矿系列[J]. 矿床地质,1992,11(4):307-314. Liu Dequan, Tang Yanling, Zhou Ruhong. Evolution of Paleozoic Crust and Metallogenic Series in Northern Xinjiang[J]. Mineral Deposits, 1992, 11(4):307-314.
[20] Xiao W J, Zhang L C, Qin K Z, 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(4):370-395.
[21] 韩宝福,季建清,宋彪,等. 新疆喀拉通克和黄山东含铜镍矿镁铁-超镁铁杂岩体的SHRIMP锆石U-Pb年龄及其地质意义[J]. 科学通报,2004,49(22):2324-2328. Han Baofu, Ji Jianqing, Song Biao, et al. SHRIMP Zircon U-Pb Ages of Kalatongke No.1 and Huangshandong Cu-Ni-Bearing Mafic-Ultramafic Complexes, North Xinjiang, and Geological Implications[J]. Chinese Sciences Bulletin, 2004, 49(22):2324-2328.
[22] Zhang Z H, Mao J W, Du A D, et al. Re-Os Dating of two Cu-Ni Sulfide Deposits in Northern Xinjiang, NW China and Its Geological Significance[J]. Journal of Asian Earth Sciences, 2008, 32(2/3/4):204-217.
[23] Zhou M F, Lesher C M, Yang Z X, et al. Geoche-mistry and Petrogenesis of 270 Ma Ni-Cu-(PGE) Sulfide-Bearing Mafic Intrusions in the Huangshan District Eastern Xinjiang, Northwest China:Implications for the Tectonic Evolution of the Central Asian Orogenic Belt[J].Chemical Geology, 2004, 209:233-257.
[24] 王京彬,王玉往,周涛发. 新疆北部后碰撞与幔源岩浆有关的成矿谱系[J]. 岩石学报,2008,24(4):743-752. Wang Jingbin, Wang Yuwang, Zhou Taofa. Metallogenic Spectrum Related to Post-Collisional Mantle-Derived Magma in North Xinjiang[J]. Acta Petrologica Sinica, 2008, 24(4):743-752.
[25] 夏明哲. 新疆东天山黄山岩带镁铁-超镁铁质岩石成因及成矿作用[D]. 西安:长安大学,2009. Xia Mingzhe. The Mafic-Ultramafic Intrusions in the Huangshan Region Eastern Tianshan, Xinjiang:Petrogenesis and Mineralization Implication[D]. Xi'an:Chang'an University, 2009.
[26] 李锦轶,张进,杨天南,等. 北亚造山区南部及其毗邻地区地壳构造分区与构造演化[J]. 吉林大学学报(地球科学版),2009,39(4):584-605. Li Jinyi, Zhang Jin, Yang Tiannan, et al. Crustal Tectonic Division and Evolution of the Southern Part of the North Asian Orogenic Region and Its Adjacent Areas[J]. Journal of Jilin University(Earth Science Edition), 2009, 39(4):584-605.
[27] 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]. Geology in China, 2006, 33(3):461-469.
[28] 李锦轶,王克卓,孙桂华,等. 东天山吐哈盆地南缘古生代活动陆缘残片:中亚地区古亚洲洋板块俯冲的地质记录[J].岩石学报,2006,22(5):1087-1102. Li Jinyi, Wang Kezhuo, Sun Guihua, et al. Paleozoic Active Margin Slices in the Southern Turfan-Hami Basin:Geological Records of Subduction of the Palro-Asian Ocean Plate in Central Asian Regions[J]. Acta Petrologica Sinica, 2006, 22(5):1087-1102.
[29] 杨兴科,李文明,李有柱,等. 东天山地区火山-岩浆作用研究[R]. 西安:中国地质调查局西安地质调查中心,2003. Yang Xingke, Li Wenming, Li Youzhu, et al. Study on Volcanic Magmatism in the Eastern Tianshan Mountains[R]. Xi'an:Xi'an Geological Survey Center of China Geological Survey, 2003.
[30] Liu Yongsheng, Gao Shan, Hu Zhaochu, et al. Continental and Oceanic Crust Recycling-Induced Melt-Peridotite Interactions in the Trans-North China Orogen:U-Pb Dating, Hf Isotopes and Trace Elements in Zircons from Mantle Xenoliths[J]. Journal of Petrology, 2010, 51(1/2):537-571.
[31] Ludwing K R. Using Isoplot/Ex Version 2, a Geochronological Toolkit for Microsoft Excel[M]. Berkeley:Berkeley Geochronology Centre Special Publications, 1999:1-47.
[32] 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. Wu Yuanbao, Zheng Yongfei. Genetic Mineralogy of Zircon and Its Constraints on the Interpretation of U-Pb Age[J]. Chinese Sciences Bulletin, 2004, 49(16):1589-1604.
[33] Wilson M. Igneous Petrogenesis[M]. London:Unwin Hyman, 1989:245-285.
[34] Irvine N T, Baragar, W R A. A Guide to the Chemical Classification of the Common Vocanic Rocks[J]. Canadian Journal of Earth Sciences, 1971, 8(5):523-548.
[35] Maniar P D, Piccoli P M. Tectonic Discrimination of Granitoids[J]. Geological Society of American Bulletin, 1989, 101:635-643.
[36] Taylor S R, McLennan S M. The Continental Crust:Its Composition and Evolution[M]. Blackwell:Oxford Press, 1985:1-312.
[37] Sun S S,McDonough W F. Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes[J]. Geological Society, Special Publications, 1989, 42(1):313-345.
[38] 赵欣,魏连生,林漳基,等. 元素在长石、云母、角闪石表面吸附的XPS研究Ⅰ. 铯、锶、铕、铈[J]. 核化学与放射化学,1992,14(2):71-78. Zhao Xin, Wei Liansheng, Lin Zhangji, et al. Study of the Sorption of Elements on the Surface of Feldspars, Muscovite and Hornblende by Means of XPSⅠ. Cs, Sr, Eu, Ce[J]. Journal of Nuclear and Radiochemistry, 1992, 14(2):71-78.
[39] 赵振华. 微量元素地球化学原理[M]. 北京:科学出版社,1997:1-238. Zhao Zhenhua. Microelement Geochemical Principle[M]. Beijing:Science Press, 1997:1-238.
[40] 李华芹. 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,1998:1-266. Li Huaqin. Geochronology of Mineralization of Nonferrous Precious Metal Deposits in Northern Xinjiang[M]. Beijing:Geological Publishing House, 1998:1-266.
[41] 孙涛,钱壮志,汤中立,等. 新疆葫芦铜镍矿床锆石U-Pb年代学、铂族元素地球化学特征及其地质意义[J]. 岩石学报,2010,26(11):3339-3349. Sun Tao, Qian Zhuangzhi, Tang Zhongli, et al. Zircon U-Pb Chronology, Platinum Group Element Geochemistry Charateristics of Hulu Cu-Ni Deposit, East Xinjiang and Its Geological Significance[J]. Acta Petrologica Sinica, 2010, 26(11):3339-3349.
[42] 陈继平,廖群安,张雄华,等. 东天山地区黄山东与香山镁铁质-超镁铁质杂岩体对比[J]. 地球科学:中国地质大学学报,2013,38(6):1183-1196. Chen Jiping, Liao Qun'an, Zhang Xionghua, et al. Contrast of Huangshandong and Xiangshan Mafic-Ultramafic Complex, East Tianshan[J]. Earth Science:Journal of China University of Geosciences, 2013, 38(6):1183-1196.
[43] 徐兴旺,秦克章,三金柱,等. 东天山四顶黑山地区545 Ma层状镁铁质-超镁铁质岩体的发现及其大地构造学和成矿学意义[J]. 岩石学报,2006,22(11):2665-2676. Xu Xingwang, Qin Kezhang, San Jinzhu, et al. Discovery of Layered Mafic-Ultramafic Intrusivers Formed in 545 Ma in the Sidingheishan Area, Eastern Tianshan, China and Its Significances for Tectonics and Cu-Ni Mineralization[J]. Acta Petrologica Sinica, 2006, 22(11):2665-2676.
[44] 李文铅,马华东,王冉,等. 东天山康古尔塔格蛇绿岩SHRIMP年龄、Nd-Sr同位素特征及构造意义[J]. 岩石学报,2008,24(4):773-780. Li Wenqian, Ma Huadong, Wang Ran, et al. SHRIMP Dating and Nd-Sr Isotopic Tracing of Kangguertage Ophiolite in Eastern Tianshan, Xinjiang[J]. Acta Petrologica Sinica, 2008, 24(4):773-780.
[45] 顾连兴,张遵忠,吴昌志,等. 关于东天山花岗岩与陆壳的垂向增长的若干认识[J]. 岩石学报,2006,22(5):1103-1120. Gu Lianxing, Zhang Zunzhong, Wu Changzhi, et al. Some Problems on Granites and Vertical Growth of the Continental Crust in the Eastern Tianshan Mountains, NW China[J]. Acta Petrologica Sinica, 2006, 22(5):1103-1120.
[46] Han C M, Xiao W J, Zhao G C, et al. In-Situ U-Pb, Hf and Re-Os Isotopes Analyese of the Xiangshan Ni-Cu-Co Deposit in Eastern Tianshan(Xinjiang), Central Asian Orogenic Belt:Constraints on the Timing and Genewiw of the Mineralization[J]. Lithos, 2010, 120(3):547-562.
[47] Sun T, Qian Z Z, Li Chusi, et al. Petrogenesis and Economic Potential of the Erhongwa Mafic-Ultramafic Intrusion in the Central Asian Orogenic Belt, NW China:Constraints from Olivine Chemistry, U-Pb Age and Hf Isotopes of Zircons, and Whole-Rock Sr-Nd-Pb Isotopes[J]. Lithos, 2013, 182/183:185-199.
[48] 周涛发,袁锋,张达玉,等. 新疆东天山觉罗塔格地区花岗岩类年代学、构造背景及其成矿作用[J]. 岩石学报,2010,26(2):478-502. Zhou Taofa, Yuan Feng, Zhang Dayu, et al. Geochronology, Tectonic Setting and Mineralization of Granitoids in Jueluotage Area, Eastern Tianshan, Xinjiang[J]. Acta Petrologica Sinica, 2010, 26(2):478-502.
[49] 李华芹,陈富文,路远发,等. 东天山三岔口铜矿区矿化岩体SHRIMP U-Pb年代学及锶同位素地球化学特征研究[J]. 地球学报,2004,25(2):191-195. Li Huaqin, Chen Fuwen, Lu Yuanfa, et al. Zircon SHRIMP U-Pb Age and Strontium Isotopes of Mineralized Granitoids in the Sanchakou Copper Polymetallic Depoist, East Tianshan Mountains[J]. Acta Geoscientica Sinica, 2004, 25(2):191-195.
[50] 唐俊华,顾连兴,张遵忠,等. 东天山黄山-镜儿泉过铝质花岗岩矿物学、地球化学及年代学研究[J]. 岩石学报,2008,24(5):921-946. Tang Junhua, Gu Lianxing, Zhang Zunzhong, et al. Peraluminous Granite in Huangshan-Jingerquan Area of Eastern Tianshan:Geochemistry, Mineralogy and Geochronology[J]. Acta Petrologica Sinica, 2008, 24(5):921-946.
[51] Ringwood A E. Composition and Petrology of the Earth'Mantle[M]. New York:McGraw-Hill, 1975:1-618.
[52] Barker J A, Menzies M A, Thirlwall M F, et al. Petrogenesis of Quaternary Intraplate Volcanism Sana'a Yenmen:Implication and Polybaric Melt Hybridization[J]. Journal of Petrology, 1997, 38:1359-1390.
[53] Campbell I H, Griffiths R W. The Evolution of Mantle`s Chemical Structure[J]. Lithos, 1993, 30:389-399.
[54] Mecdonald R, Rogers N W, Fitton J C, et al. Plume Lithosphere Interactions in the Generation of the Basalts of the Kenya Rift, East Africa[J]. Journal of Petrology, 2001, 42:877-900.
[55] Saunders A D, Storey M, Kent R W, et al. Conse-quences of Plume-Lithosphere Interactions[J]. Geological Society of London Special Publication, 1992, 68:41-60.
[56] Woodhead J D, Hergt J M, Davidson J P, et al. Hafnium Isotope Evidence for "Conservative" Element Mobility During Subduction Zone Processes[J]. Earth and Planet Science Letters, 2001, 192:331-346.
[57] Frtton J G, James D, Leeman W P. Basic Mag-matism Associated with Late Cenozoic Extension in the Western United States:Compositional Variations in Space and Time[J]. Journal of Geophysical Research, 1991, 96(B8):13693-13711.
[58] Kepezhinskas P, McDermott F, Defant M J, et al. Trace Element and Sr-Nd-Pb Isotopic Constraints on a Three-Component Model of Kamchatka Arc Petrogenesis[J]. Geochimica et Cosmochimica Acta, 1997, 61(3):577-600.
[59] 胡霭琴,章振根,刘菊英,等. 天山东段中天山隆起带前寒武纪变质岩系时代及演化:据U-Pb年代学研究[J]. 地球化学,1986,1:23-35. Hu Aiqin, Zhang Zhengen, Liu Juying, et al. U-Pb Age and Evolution of Precambrian Metamorphic Rocks of Middle Tianshan Uplift Zone, Eastern Tianshan, China[J]. Geochimica, 1986, 1:23-35.
[60] 刘树文,郭召杰,张志诚,等. 中天山东段前寒武纪变质地块的性质:地质年代学和钕同位素地球化学的约束[J]. 中国科学:D辑:地球科学,2004,34(5):395-403. Liu Shuwen, Guo Zhaojie, Zhang Zhicheng, et al. Characteristics of Precambrian Metamorphic Blocks in the Eastern Section of Middle Tianshan:Constraints of Geochronology and Nd Isotopic Geochemistry[J]. Science in China:Series D:Earth Science, 2004, 34(5):395-403.
[61] 成守德,张湘江. 新疆大地构造基本格架[J]. 新疆地质,2000,18(4):293-296. Cheng Shoude, Zhang Xiangjiang. Geotectonic Division of Xinjiang[J]. Xinjiang Geology, 2000, 18(4):293-296.
[62] 苏春乾,姜常义,夏明哲,等. 新疆觉罗塔格构造带新元古代变质核杂岩锆石U-Pb年龄与地质意义[J]. 岩石学报,2008,24(12):2789-2799. Su Chunqian, Jiang Changyi, Xia Mingzhe, et al. Zircon SHRIMP U-Pb Dating from Granite of the Metamorphic Core Complex System in Jueluotage Tectonic Belt and Its Geological Significance[J]. Acta Petrologica Sinica, 2008, 24(12):2789-2799.
[63] 何国琦,刘德权,李茂松,等. 新疆主要造山带地壳发展的五个阶段模式及成矿系列[J]. 新疆地质,1995,13(2):99-194. He Guoqi, Liu Dequan, Li Maosong, et al. The Five-Stage Model of Crustal Evolution and Metallogenic Series of Chief Orogenic Belts in Xinjiang[J]. Xinjiang Geology, 1995, 13(2):99-194.
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