东昆仑祁漫塔格阿确墩地区侵入岩U-Pb年代学、地球化学及其地质意义

李婷; 李猛; 胡朝斌; 李瑶; 孟杰; 高晓峰; 查显锋

doi:10.3799/dqkx.2018.224

东昆仑祁漫塔格阿确墩地区侵入岩U-Pb年代学、地球化学及其地质意义

doi: 10.3799/dqkx.2018.224

李婷^1,2,,
李猛^1,2,
胡朝斌^1,2,
李瑶^1,2,
孟杰^1,2,
高晓峰^1,2,
查显锋^1,2

1.
中国地质调查局西安地质调查中心, 造山带地质研究中心, 陕西西安 710054
2.
自然资源部岩浆作用成矿与找矿重点实验室, 陕西西安 710054

基金项目:

中国地质调查局项目 DD20160002

详细信息

作者简介:
李婷(1984-), 女, 硕士, 工程师, 矿物学、岩石学、矿床学专业

中图分类号: P581
计量
- 文章访问数: 5282
- HTML全文浏览量: 1723
- PDF下载量: 31
- 被引次数: 0
出版历程
- 收稿日期: 2018-06-29
- 刊出日期: 2018-12-15

Zircon U-Pb Geochronology, Geochemistry and Its Geological Implications of Intrusions in Aquedun Area from Qimantag, East Kunlun, China

Li Ting^{1,2
,},
Li Meng^1,2,
Hu Chaobin^1,2,
Li Yao^1,2,
Meng Jie^1,2,
Gao Xiaofeng^1,2,
Zha Xianfeng^1,2

1.
Xi'an Center of Geological Survey, Orogen Research Center, China Geological Survey, Xi'an 710054, China
2.
Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, Ministry of Natural Resources, Xi'an 710054, China

摘要

摘要: 祁漫塔格地区岩浆岩的成岩时代和形成环境的确定能对东昆仑造山带加里东期构造演化时限加以约束.对祁漫塔格西北部阿确墩地区石英闪长岩和二长花岗岩进行了年代学和岩石地球化学研究，结果显示，石英闪长岩属准铝质-弱过铝质钙碱性系列岩石；轻重稀土分馏明显，具中等-轻微铕负异常（δEu=0.79~0.90）；相对富集Rb、K、Hf、Zr、Tb、Nd等元素，不同程度地亏损Ba、P、Ti、Nd、Ta、Y；具有I型花岗岩类特征.二长花岗岩属弱过铝质钙碱性系列岩石；轻重稀土分异程度极大，具明显铕负异常（δEu=0.42~0.45）；富集大离子亲石元素（如Rb、K、La、Ce、Nd、Tb等），亏损高场强元素（P、Ti、Nd、Ta）和Ba、Sr、U等元素；为高分异I型花岗岩.Nd/Th、Nb/Ta、Mg^#值等指标显示石英闪长岩为壳源特征且受到幔源岩浆的影响，推测是幔源岩浆底侵地壳物质发生部分熔融形成的；二长花岗岩则是壳源的，可能与幔源岩浆底侵诱发的上地壳物质部分熔融有关，且经历了强烈的结晶分离作用.石英闪长岩和二长花岗岩的LA-ICP-MS锆石U-Pb年龄分别为448.8±3.9 Ma和405.2±3.6 Ma，代表其形成时代.石英闪长岩总体显示出与俯冲消减作用有关的岛弧岩浆岩地球化学特征；二长花岗岩在构造环境图解中显示为碰撞背景，但微量元素与同碰撞花岗岩典型特征不符，综合分析认为形成于后碰撞构造背景下.结合区域构造演化，推测东昆仑祁漫塔格地区在晚奥陶世持续处于俯冲消减环境中，早泥盆世之前进入后碰撞造山阶段.
- 东昆仑造山带 /
- 祁漫塔格 /
- 阿确墩地区 /
- 侵入岩 /
- 锆石U-Pb定年 /
- 地球化学
Abstract: The determination of formation time and tectonic setting of intrusions in Qimantag area can limit the time of Caledonian tectonic evolution in East Kunlun orogen. Zircon U-Pb geochronology, geochemistry of quartz diorite and monzonite adamellite in Aquedun of northwestern Qimantag area are studied in this paper. Results show that quartz diorite belongs to metaluminous-weakly peraluminous and calc-alkaline series of I-type granite, with moderate Eu negative abnormality (δEu=0.79-0.90) and significant fractionation between light REE and heavy REE, enriched in Rb, K, Hf, Zr, Tb, Nd and depleted of Ba, P, Ti, Nd, Ta, Y.Monzonite adamellite belongs to weakly peraluminous and calc-alkaline series of high-fractionated I-type granite, with significant negative Eu abnormality (δEu=0.42-0.45) and significant fractionation between light REE and heavy REE, enriched in LILE(Rb, K, La, Ce, Nd, Tb) and depleted in HFSE(P, Ti, Nd, Ta) and Ba, Sr, U.The ratios of Nd/Th, Nb/Ta and Mg^# of quartz diorite show crustal characteristics with the addition of small amount of mantle-derived materials, produced by partial melting of the continental crust induced by mantle derived magmas underplating. The ratios of Nd/Th, Nb/Ta and Mg^# of monzonite adamellite show crustal characteristics, produced by partial melting of the upper continental crust induced by mantle derived magmas underplating and may have experienced the fractional crystallization at the same time. Zircon LA-ICP-MS U-Pb age of the quartz diorite and monzonite adamellite are 448.8±3.9 Ma and 405.2±3.6 Ma, respectively, which represents their formation time. The chemical characteristics of quartz diorite are closely related to the island-arc environments in subduction belt.Monzonite adamellite falls into the zone of collision setting with tectonic setting discrimination diagrams, but the trace elements do not match with typical collision-orogenic granite, so we think monzonite adamellite is post-collision-orogenic granite.Combined with the regional tectonic evolution, it is concluded that Qimantag block of East Kunlun orogen maybe is in the subduction stage in Late Ordovician, and in the post-collision stage before Early Devonian.
- East Kunlun orogen /
- Qimantag /
- Aquedun area /
- intrusion /
- zircon U-Pb dating /
- geochemistry

HTML全文

图 1 东昆仑阿确墩地区地质简图

Fig. 1. The sketch geological map of the Aquedun area in the East Kunlun orogen

下载: 全尺寸图片幻灯片

图 2 东昆仑阿确墩地区岩体主量元素判别图解

a.据Middlemost(1994)清绘；b.岩石类型边界引自Rickwood(1989)

Fig. 2. Major element diagrams of intrusions in Aquedun area in the East Kunlun orogen

下载: 全尺寸图片幻灯片

图 3 东昆仑阿确墩地区岩体REE球粒陨石标准化配分型式(a)和微量元素原始地幔标准化蛛网图(b)

球粒陨石和原始地幔标准化值据Sun and McDonough(1989)

Fig. 3. Chondrite-normalized REE pattern (a) and primitive mantle-normalized trace element pattern (b) of intrusions in Aquedun area in the East Kunlun orogen

下载: 全尺寸图片幻灯片

图 4 东昆仑阿确墩地区岩体锆石CL图像

Fig. 4. CL images of zircons of intrusions in Aquedun area in the East Kunlun orogen

下载: 全尺寸图片幻灯片

图 5 东昆仑阿确墩地区岩体LA-ICP-MS锆石U-Pb年龄谐和图和表面加权平均年龄图

Fig. 5. LA-ICP-MS zircon U-Pb condordia diagrams and weighted average ages of intrusions in Aquedun area in the East Kunlun orogen

下载: 全尺寸图片幻灯片

图 6 东昆仑阿确墩地区岩体地球化学图解

FG.分异的M、I、S型花岗岩；OGT.未分异的M、I、S型花岗岩

Fig. 6. Diagrams of intrusions in Aquedun area in the East Kunlun orogen

下载: 全尺寸图片幻灯片

图 7 东昆仑阿确墩地区岩体Nb-Nb/Ta图解

据Barth et al.(2000)

Fig. 7. Nb-Nb/Ta diagram of intrusions in Aquedun area in the East Kunlun orogen

下载: 全尺寸图片幻灯片

图 8 东昆仑阿确墩地区岩体Sr-Ba图解

据Li et al.(2007)；PlAn50.斜长石(An=50)；PlAn15.斜长石(An=15)；Kfs.钾长石；Amp.角闪石；Grt.石榴石；Ms.白云母；Bt.黑云母

Fig. 8. Sr-Ba diagram of intrusions in Aquedun area in the East Kunlun orogen

下载: 全尺寸图片幻灯片

图 9 东昆仑阿确墩地区岩体构造环境判别图

1.地幔斜长岩幔源花岗岩；2.钙碱性更长花岗岩-板块碰撞前消减地区花岗岩；3.高钾钙碱性花岗岩-板块碰撞后隆起区花岗岩；4.造山晚期-晚造山期花岗岩(二长岩)；5.非造山期A型花岗岩；6.同碰撞花岗岩(S型)；7.造山后期A型花岗岩.a、c.据Pearce et al.(1984)；b.据Harris et al.(1986)

Fig. 9. Tectonic setting discrimination diagrams of intrusions in Aquedun area in the East Kunlun orogen

下载: 全尺寸图片幻灯片

参考文献(85)

[1]	Barth, M.G., McDonough, W.F., Rudnick, R.L., 2000.Tracking the Budget of Nb and Ta in the Continental Crust.Chemical Geology, 165(3-4):197-213. https://doi.org/10.1016/s0009-2541(99)00173-4
[2]	Bea, F., Arzamastsev, A., Montero, P., et al., 2001.Anomalous Alkaline Rocks of Soustov, Kola:Evidence of Mantle-Derived Metasomatic Fluids Affecting Crustal Materials.Contributions to Mineralogy and Petrology, 140(5):554-566. https://doi.org/10.1007/s004100000211
[3]	Chappell, B.W., White, A.J.R., 2001.Two Contrasting Granite Types:25 Years Later.Australian Journal of Earth Sciences, 48(4):489-499. https://doi.org/10.1046/j.1440-0952.2001.00882.x
[4]	Chen, H.W., Luo, Z.H., Mo, X.X., et al., 2006.SHRIMP Ages of Kayakedengtage Complex in the East Kunlun Mountains and Their Geological Implications.Acta Petrologica et Mineralogica, 25(1):25-32 (in Chinese with English abstract). http://www.cnki.com.cn/Article/CJFDTotal-YSKW200601002.htm
[5]	Chen, N.S., Wang, Q.Y., Chen, Q., et al., 2007.Components and Metamorphism of the Basements of the Qaidam and Oulongbuluke Micro-Continental Blocks, and a Tentative Interpretation of Paleocontinental Evolution in NW-Central China.Earth Science Frontiers, 14(1):43-55 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dxqy200701004
[6]	Cui, M.H., Meng, F.C., Wu, X.K., 2011.Early Ordovician Island Arc of Qimantag Mountain, Eastern Kunlun:Evidences from Geochemistry, Sm-Nd Isotope and Geochronology of Intermediate-Basic Igneous Rocks.Acta Petrologica Sinica, 27(11):3365-3379 (in Chinese with English abstract). doi: 10.1097-TP.0b013e3182295bed/
[7]	Feng, J.Y., Pei, X.Z., Yu, S.L., et al., 2010.The Discovery of the Mafic-Ultramafic Melange in Kekesha Area of Dulan County, East Kunlun Region, and Its LA-ICP-MS Zircon U-Pb Age.Geology in China, 37(1):28-38 (in Chinese with English abstract). http://d.wanfangdata.com.cn/Periodical/zgdizhi201001003
[8]	Gao, X.F., Xiao, P.X., Jia, Q.Z., 2011.Redetermination of the Tanjianshan Group:Geochronological and Geochemical Evidence of Basalts from the Margin of the Qaidam Basin.Acta Geologica Sinica, 85(9):1452-1463 (in Chinese with English abstract). https://doi.org/11-1951/P.20110907.1101.004
[9]	Gao, X.F., Xiao, P.X., Xie, C.R., et al., 2010.Zircon LA-ICP-MS U-Pb Dating and Geological Significance of Bashierxi Granite in the Eastern Kunlun Area, China.Geological Bulletin of China, 29(7):1001-1008(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz201007005
[10]	Gao, Y.B., Li, W.Y., 2011.Petrogenesis of Granites Containing Tungsten and Tin Ores in the Baiganhu Deposit, Qimantage, NW China:Constraints from Petrology, Chronology and Geochemistry.Geochimica, 40(4):324-336 (in Chinese with English abstract). https://doi.org/10.19700/j.0379-1726.2011.04.002
[11]	Hao, N.N., Yuan, W.M., Zhang, A.K., et al., 2014.Late Silurian to Early Devonian Granitoids in the Qimantage Area, East Kunlun Mountains:LA-ICP-MS Zircon U-Pb Ages, Geochemical Features and Geological Setting.Geological Review, 60(1):201-215 (in Chinese with English abstract). https://doi.org/10.16509/j.georeview.2014.01.022
[12]	Harris, N.B.W., Pearce, J.A., Tindle, A.G., 1986.Geochemical Characteristics of Collision-Zone Magmatism.Collision Tectonics, 19(5):67-81. doi: 10.1144-GSL.SP.1986.019.01.04/
[13]	King, P.L., White, A.J.R., Chappell, B.W., et al., 1997.Characterization and Origin of Aluminous A-Type Granites from the Lachlan Fold Belt, Southeastern Australia.Journal of Petrology, 38(3):371-391. https://doi.org/10.1093/petroj/38.3.371
[14]	Li, R.B., Pei, X.Z., Li, Z.C., et al., 2014.Age, Geochemical Characteristics and Tectonic Significance of Yikehalaer Granodiorite in Buqingshan Tectonic Melange Belt, Southern Margin of East Kunlun.Acta Geoscientica Sinica, 35(4):434-444 (in Chinese with English abstract). https://doi.org/10.3975/cagsb.2014.04.05
[15]	Li, R.S., Ji, W.H., Zhao, Z.M., et al., 2007.Progress in the Study of the Early Paleozoic Kunlun Orogenic Belt.Geological Bulletin of China, 26(4):373-382 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz200704002
[16]	Li, W.Y., Li, S.G., Guo, A.L., et al., 2007.Zircon SHRIMP U-Pb Age and Trace Element Geochemistry of Kuhai Gabbro and Deer Ni Diorite, Southern Tectonic Belt, Eastern Kunlun, Qinghai-Constraints on the South Boundary of Late Neoproterozoic-Early Ordovician Archipelagic Ocean.Science in China (Series D:Earth Sciences), 37(Suppl.1):288-294(in Chinese). doi: 10.1007/s11430-007-6003-4
[17]	Li, X.H., Li, Z.X., Li, W.X., et al., 2007.U-Pb Zircon, Geochemical and Sr-Nd-Hf Isotopic Constraints on Age and Origin of Jurassic I-and A-Type Granites from Central Guangdong, SE China:A Major Igneous Event in Response to Foundering of a Subducted Flat-Slab? Lithos, 96(1-2):186-204. https://doi.org/10.1016/j.lithos.2006.09.018
[18]	Liu, B., Ma, C.Q., Jiang, H.A., et al., 2013.Early Paleozoic Tectonic Transition from Ocean Subduction to Collisional Orogeny in the Eastern Kunlun Region:Evidence from Huxiaoqin Mafic Rocks.Acta Petrologica Sinica, 29(6):2093-2106 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201306017
[19]	Liu, B., Ma, C.Q., Zhang, J.Y., et al., 2012.Petrogenesis of Early Devonian Intrusive Rocks in the East Part of Eastern Kunlun Orogen and Implication for Early Palaeozoic Orogenic Processes.Acta Petrologica Sinica, 28(6):1785-1807 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201206007
[20]	Liu, G.Z., Zhang, Y.X., Xue, J.Q., et al., 2014.Zircon LA-ICPMS U-Pb Dating and Geochemistry of Basement Granites from North Kunlun Faults Zone, Western Qaidam Basin and Their Geological Implications.Acta Petrologica Sinica, 30(6):1615-1627 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201406007
[21]	Liu, Z.Q., Pei, X.Z., Li, R.B., et al., 2011a.Early Paleozoic Intermediate-Acid Magmatic Activity in Bairiqiete Area along the Buqingshan Tectonic Mélange Belt on the Southern Margin of East Kunlun:Constraints from Zircon U-Pb Dating and Geochemistry.Geology in China, 38(5):1150-1167 (in Chinese with English abstract). doi: 10.1016-j.ophtha.2011.06.005/
[22]	Liu, Z.Q., Pei, X.Z., Li, R.B., et al., 2011b.LA-ICP-MS Zircon U-Pb Geochronology of the Two Suites of Ophiolites at the Buqingshan Area of the A'nyemaqen Orogenic Belt in the Southern Margin of East Kunlun and Its Tectonic Implication.Acta Geologica Sinica, 85(2):185-194 (in Chinese with English abstract).
[23]	Lu, L., Zhang, Y.L., Wu, Z.H., et al., 2013.Zircon U-Pb Dating of Early Paleozoic Granites from the East Kunlun Mountains and Its Geological Significance.Acta Geoscientica Sinica, 34(4):447-454(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqxb201304007
[24]	Ludwig, K.R., 2003.ISOPLOT 3.00: A Geochronological Toolkit for Microsoft Excel.Berkeley Geochronology Center, Berkeley.
[25]	Meng, F.C., Cui, M.H., Jia, L.H., et al., 2015.Paleozoic Continental Collision of the East Kunlun Orogen:Evidence from Protoliths of the Eclogites.Acta Petrologica Sinica, 31(12):3581-3594 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201512006
[26]	Middlemost, E.A.K., 1994.Naming Materials in the Magma/Igneous Rock System.Earth-Science Reviews, 37(3-4):215-224. https://doi.org/10.1016/0012-8252(94)90029-9
[27]	Miller, C.F., McDowell, S.M., Mapes, R.W., 2003.Hot and Cold Granites? Implications of Zircon Saturation Temperatures and Preservation of Inheritance.Geology, 31(6):529.https://doi.org/10.1130/0091-7613(2003)031<0529:hacgio>2.0.co;2 doi: 10.1130/0091-7613(2003)031<0529:hacgio>2.0.co;2
[28]	Mo, X.X., Luo, Z.H., Deng, J.F., et al., 2007.Granitoids and Crustal Growth in the East-Kunlun Orogenic Belt.Geological Journal of China Universities, 13(3):403-414 (in Chinese with English abstract). http://adsabs.harvard.edu/abs/2011AGUFM.T51D2370M
[29]	Pearce, J.A., Harris, N.B.W., Tindle, A.G., 1984.Trace Element Discrimination Diagrams for the Tectonic Interpretation of Granitic Rocks.Journal of Petrology, 25(4):956-983. https://doi.org/10.1093/petrology/25.4.956
[30]	Qi, S.S., Song, S.G., Shi, L.C., et al., 2014.Discovery and Its Geological Significance of Early Paleozoic Eclogite in Xiarihamu-Suhaitu Area, Western Part of the East Kunlun.Acta Petrologica Sinica, 30(11):3345-3356(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201411018
[31]	Qi, X.P., Yang, J., Fan, X.G., et al., 2016.Age, Geochemical Characteristics and Tectonic Significance of Changshishan Ophiolite in Central East Kunlun Tectonic Mélange Belt along the East Section of East Kunlun Mountains.Geology in China, 43(3):797-816 (in Chinese with English abstract). https://doi.org/10.12029/gc20160308
[32]	Qiu, J.S., Xiao, E., Hu, J., et al., 2008.Petrogenesis of Highly Fractionated I-Type Granites in the Coastal Area of Northeastern Fujian Province:Constraints from Zircon U-Pb Geochronology, Geochemistry, and Nd-Hf Isotopes.Acta Petrologica Sinica, 24 (11):2468-2484 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200811003.htm
[33]	Raith, J.G., 1995.Petrogenesis of the Concordia Granite Gneiss and Its Relation to W-Mo Mineralization in Western Namaqualand, South Africa.Precambrian Research, 70(3-4):303-335. https://doi.org/10.1016/0301-9268(94)00049-w
[34]	Rapp, R.P., Watson, E.B., 1995.Dehydration Melting of Metabasalt at 8-32 kbar:Implications for Continental Growth and Crust-Mantle Recycling.Journal of Petrology, 36(4):891-931. https://doi.org/10.1093/petrology/36.4.891
[35]	Ren, E.F., Zhang, G.L., Qiu, W., et al., 2012.Characteristics of Geochemistry and Tectonic Significance of Caledonian Granite in the Maerzheng Region in the South Area of East Kunlun.Geoscience, 26(1):36-44(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xddz201201004
[36]	Rickwood, P.C., 1989.Boundary Lines within Petrologic Diagrams Which Use Oxides of Major and Minor Elements.Lithos, 22(4):247-263. https://doi.org/10.1016/0024-4937(89)90028-5
[37]	Shi, B., Zhu, Y.H., Zhong, Z.Q., et al., 2016.Petrological, Geochemical Characteristics and Geological Significance of the Caledonian Peraluminous Granites in Heihai Region, Eastern Kunlun.Earth Science, 41(1):35-54(in Chinese with English abstract). https://doi.org/10.3799/dqkx.2016.003
[38]	Sun, S.S., McDonough, W.F., 1989.Chemical and Isotopic Systematics of Oceanic Basalts:Implications for Mantle Composition and Processes.Geological Society, London, Special Publications, 42(1):313-345. https://doi.org/10.1144/gsl.sp.1989.042.01.19
[39]	Tian, G.K., Meng, F.C., Fan, Y.Z., et al., 2016.The Characteristics of Early Paleozoic Post-Orogenic Granite in the East Kunlun Orogen:A Case Study of Dagangou Granite.Acta Petrologica et Mineralogica, 35(3):371-390(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSKW201603001.htm
[40]	Wang, B.Z., Luo, Z.H., Pan, T., et al., 2012.Petrotectonic Assemblages and LA-ICP-MS Zircon U-Pb Age of Early Paleozoic Volcanic Rocks in Qimantag Area, Tibetan Plateau.Geological Bulletin of China, 31(6):860-874 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ZQYD201206005.htm
[41]	Wang, G.C., Chen, N.S., Zhu, Y.H., et al., 2003.Geochronology Evidence and Implication of Late Caledonian Ductile Shear Deformation of Thrusting-Type in Kunzhong Orogenic Belt, East Kunlun.Acta Geologica Sinica, 77(3):432 (in Chinese).
[42]	Whalen, J.B., Currie, K.L., Chappell, B.W., 1987.A-Type Granites:Geochemical Characteristics, Discrimination and Petrogenesis.Contributions to Mineralogy and Petrology, 95(4):407-419. https://doi.org/10.1007/bf00402202
[43]	Wu, F.Y., Li, X.H., Yang, J.H., et al., 2007.Discussions on the Petrogenesis of Granites.Acta Petrologica Sinica, 23(6):1217-1238(in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-YSXB200706000.htm
[44]	Yang, L., Zhou, H.W., Zhu, Y.H., et al., 2014.Geochemical Characteristics and LA-ICP-MS Zircon U-Pb Ages of Intermediate to Mafic Dyke Swarms in Haxiya Area, Golmud, Qinghai Province.Geological Bulletin of China, 33(6):804-819 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgqydz201406004
[45]	Yu, M., Feng, C.Y., He, S.Y., et al., 2017.The Qiman Tagh Orogen as a Window to the Crustal Evolution of the Northern Tibetan Plateau.Acta Geologica Sinica, 91(4):703-723 (in Chinese with English abstract). http://www.sciencedirect.com/science/article/pii/S0012825216303713
[46]	Zhang, Q., Jin, W.J., Li, C.D., et al., 2010.Revisiting the New Classification of Granitic Rocks Based on Whole-Rock Sr and Yb Contents:Index.Acta Petrologica Sinica, 26(4):985-1015 (in Chinese with English abstract).
[47]	Zhang, Q., Wang, Y., Li, C.D., et al., 2006.Granite Classification on the Basis of Sr and Yb Contents and Its Implications.Acta Petrologica Sinica, 22(9):2249-2269 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200609000.htm
[48]	Zhang, Y.F., Pei, X.Z., Ding, S.P., et al., 2010.LA-ICP-MS Zircon U-Pb Age of Quartz Diorite at the Kekesha Area of Dulan County, Eastern Section of the East Kunlun Orogenic Belt, China and Its Significance.Geological Bulletin of China, 29(1):79-85 (in Chinese with English abstract). http://www.cqvip.com/qk/95894A/201001/34053570.html
[49]	Zheng, Z., Chen, Y.J., Deng, X.H., et al., 2016.Muscovite ⁴⁰Ar/³⁹Ar Dating of the Baiganhu W-Sn Orefield, Qimantag, East Kunlun Mountains, and Its Geological Implications.Geology in China, 43(4):1341-1352(in Chinese with English abstract). https://doi.org/10.12029/gc20160419
[50]	Zhou, J.H., Feng, C.Y., Shen, D.L., et al., 2015.Geochronology, Geochemistry and Tectonic Implications of Granodiorite in the Northwest of Weibao Deposit, Xinjiang Qimantage.Acta Geologica Sinica, 89(3):473-486(in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE201503003.htm
[51]	谌宏伟, 罗照华, 莫宣学, 等, 2006.东昆仑喀雅克登塔格杂岩体的SHRIMP年龄及其地质意义.岩石矿物学杂志, 25(1):25-32. doi: 10.3969/j.issn.1000-6524.2006.01.003
[52]	陈能松, 王勤燕, 陈强, 等, 2007.柴达木和欧龙布鲁克陆块基底的组成和变质作用及中国中西部古大陆演化关系初探.地学前缘, 14(1):43-55. doi: 10.3321/j.issn:1005-2321.2007.01.004
[53]	崔美慧, 孟繁聪, 吴祥珂, 2011.东昆仑祁漫塔格早奥陶世岛弧:中基性火成岩地球化学、Sm-Nd同位素及年代学证据.岩石学报, 27(11):3365-3379. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201111017
[54]	冯建赟, 裴先治, 于书伦, 等, 2010.东昆仑都兰可可沙地区镁铁-超镁铁质杂岩的发现及其LA-ICP-MS锆石U-Pb年龄.中国地质, 37(1):28-38. http://d.old.wanfangdata.com.cn/Periodical/zgdizhi201001003
[55]	高晓峰, 校培喜, 贾群子, 2011.滩间山群的重新厘定——来自柴达木盆地周缘玄武岩年代学和地球化学证据.地质学报, 85(9):1452-1463. http://www.cqvip.com/QK/95080X/201109/39502296.html
[56]	高晓峰, 校培喜, 谢从瑞, 等, 2010.东昆仑阿牙克库木湖北巴什尔希花岗岩锆石LA-ICP-MS U-Pb定年及其地质意义.地质通报, 29(7):1001-1008. doi: 10.3969/j.issn.1671-2552.2010.07.005
[57]	高永宝, 李文渊, 2011.东昆仑造山带祁漫塔格地区白干湖含钨锡矿花岗岩:岩石学、年代学、地球化学及岩石成因.地球化学, 40(4):324-336. http://d.old.wanfangdata.com.cn/Periodical/dqhx201104002
[58]	郝娜娜, 袁万明, 张爱奎, 等, 2014.东昆仑祁漫塔格晚志留世-早泥盆世花岗岩:年代学、地球化学及形成环境.地质论评, 60(1):201-215. http://d.wanfangdata.com.cn/Periodical/dzlp201401019
[59]	李瑞保, 裴先治, 李佐臣, 等, 2014.东昆仑南缘布青山构造混杂带亿可哈拉尔花岗闪长岩年代学、地球化学特征及构造意义研究.地球学报, 35(4):434-444. http://d.old.wanfangdata.com.cn/Periodical/dqxb201404008
[60]	李荣社, 计文化, 赵振明, 等, 2007.昆仑早古生代造山带研究进展.地质通报, 26(4):373-382. doi: 10.3969/j.issn.1671-2552.2007.04.002
[61]	李王晔, 李曙光, 郭安林, 等, 2007.青海东昆南构造带苦海辉长岩和德尔尼闪长岩的锆石SHRIMP U-Pb年龄及痕量元素地球化学——对"祁-柴-昆"晚新元古代-早奥陶世多岛洋南界的制约.中国科学(D辑:地球科学), 37(增刊1):288-294. http://www.cqvip.com/QK/98491X/2007A01/25024361.html
[62]	刘彬, 马昌前, 蒋红安, 等, 2013.东昆仑早古生代洋壳俯冲与碰撞造山作用的转换:来自胡晓钦镁铁质岩石的证据.岩石学报, 29(6):2093-2106. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201306017
[63]	刘彬, 马昌前, 张金阳, 等, 2012.东昆仑造山带东段早泥盆世侵入岩的成因及其对早古生代造山作用的指示.岩石学报, 28(6):1785-1807. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201206007
[64]	刘桂珍, 张玉修, 薛建勤, 等, 2014.柴达木盆地西部昆北断阶带基底花岗岩锆石U-Pb年龄、地球化学特征及其地质意义.岩石学报, 30(6):1615-1627. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201406007
[65]	刘战庆, 裴先治, 李瑞保, 等, 2011a.东昆仑南缘布青山构造混杂岩带早古生代白日切特中酸性岩浆活动:来自锆石U-Pb测年及岩石地球化学证据.中国地质, 38(5):1150-1167. http://d.old.wanfangdata.com.cn/Periodical/zgdizhi201105003
[66]	刘战庆, 裴先治, 李瑞保, 等, 2011b.东昆仑南缘阿尼玛卿构造带布青山地区两期蛇绿岩的LA-ICP-MS锆石U-Pb定年及其构造意义.地质学报, 85(2):185-194. http://d.old.wanfangdata.com.cn/Periodical/dizhixb201102004
[67]	陆露, 张延林, 吴珍汉, 等, 2013.东昆仑早古生代花岗岩锆石U-Pb年龄及其地质意义.地球学报, 34(4):447-454. http://d.old.wanfangdata.com.cn/Periodical/dqxb201304007
[68]	孟繁聪, 崔美慧, 贾丽辉, 等, 2015.东昆仑造山带早古生代的大陆碰撞:来自榴辉岩原岩性质的证据.岩石学报, 31(12):3581-3594. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201512006
[69]	莫宣学, 罗照华, 邓晋福, 等, 2007.东昆仑造山带花岗岩及地壳生长.高校地质学报, 13(3):403-414. doi: 10.3969/j.issn.1006-7493.2007.03.010
[70]	祁生胜, 宋述光, 史连昌, 等, 2014.东昆仑西段夏日哈木-苏海图早古生代榴辉岩的发现及意义.岩石学报, 30(11):3345-3356. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201411018
[71]	祁晓鹏, 杨杰, 范显刚, 等, 2016.东昆仑东段东昆中构造混杂岩带长石山蛇绿岩年代学、地球化学特征及其构造意义.中国地质, 43(3):797-816. http://d.old.wanfangdata.com.cn/Periodical/zgdizhi201603008
[72]	邱检生, 肖娥, 胡建, 等, 2008.福建北东沿海高分异Ⅰ型花岗岩的成因:锆石U-Pb年代学、地球化学和Nd-Hf同位素制约.岩石学报, 24(11):2468-2484. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200811002
[73]	任二峰, 张桂林, 邱炜, 等, 2012.东昆南马尔争地区加里东期花岗岩岩石地球化学特征及构造意义.现代地质, 26(1):36-44. doi: 10.3969/j.issn.1000-8527.2012.01.004
[74]	施彬, 朱云海, 钟增球, 等, 2016.东昆仑黑海地区加里东期过铝质花岗岩岩石学、地球化学特征及地质意义.地球科学, 41(1):35-54. http://earth-science.net/WebPage/Article.aspx?id=3217
[75]	田广阔, 孟繁聪, 范亚洲, 等, 2016.东昆仑早古生代造山后花岗岩的特征——以大干沟花岗岩为例.岩石矿物学杂志, 35(3):371-390. doi: 10.3969/j.issn.1000-6524.2016.03.001
[76]	王秉璋, 罗照华, 潘彤, 等, 2012.青藏高原祁漫塔格地区早古生代火山岩岩石构造组合和LA-ICP-MS锆石U-Pb年龄.地质通报, 31(6):860-874. doi: 10.3969/j.issn.1671-2552.2012.06.005
[77]	王国灿, 陈能松, 朱云海, 等, 2003.东昆仑东段昆中构造带晚加里东期逆冲型韧性剪切变形的年代学证据及其意义.地质学报, 77(3):432. http://d.old.wanfangdata.com.cn/Periodical/dizhixb200303024
[78]	吴福元, 李献华, 杨进辉, 等, 2007.花岗岩成因研究的若干问题.岩石学报, 23(6):1217-1238. doi: 10.3969/j.issn.1000-0569.2007.06.001
[79]	杨柳, 周汉文, 朱云海, 等, 2014.青海格尔木哈希牙地区中基性岩墙群地球化学特征与LA-ICP-MS锆石U-Pb年龄.地质通报, 33(6):804-819. doi: 10.3969/j.issn.1671-2552.2014.06.004
[80]	于淼, 丰成友, 何书跃, 等, 2017.祁漫塔格造山带——青藏高原北部地壳演化窥探.地质学报, 91(4):703-723. doi: 10.3969/j.issn.0001-5717.2017.04.001
[81]	张旗, 金惟俊, 李承东, 等, 2010.再论花岗岩按照Sr-Yb的分类:标志.岩石学报, 26(4):985-1015. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201004001
[82]	张旗, 王焰, 李承东, 等, 2006.花岗岩的Sr-Yb分类及其地质意义.岩石学报, 22(9):2249-2269. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200609001
[83]	张亚峰, 裴先治, 丁仨平, 等, 2010.东昆仑都兰县可可沙地区加里东期石英闪长岩锆石LA-ICP-MS U-Pb年龄及其意义.地质通报, 29(1):79-85. doi: 10.3969/j.issn.1671-2552.2010.01.010
[84]	郑震, 陈衍景, 邓小华, 等, 2016.东昆仑祁漫塔格地区白干湖钨锡矿田白云母⁴⁰Ar/³⁹Ar定年及地质意义.中国地质, 43(4):1341-1352. http://www.cqvip.com/QK/90050X/201604/669848900.html
[85]	周建厚, 丰成友, 沈灯亮, 等, 2015.新疆祁漫塔格维宝矿区西北部花岗闪长岩年代学、地球化学及其构造意义.地质学报, 89(3):473-486. doi: 10.3969/j.issn.1006-0995.2015.03.037