ZIRCON U-PB DATING, GEOCHEMICAL CHARACTERISTICS AND METALLOGENIC SIGNIFICANCE OF GRONODIORITE PORPHYRY FROM THE XIZANGDAGOU GOLD DEPOSIT IN EAST KUNLUN, QINGHAI PROVINCE
-
摘要: 利用LA-ICP-MS锆石U-Pb定年,对位于东昆仑地区巴颜喀拉成矿带的西藏大沟金矿床进行研究,首次获得与成矿有密切关系的花岗闪长斑岩加权平均年龄为(225.0±1.2)Ma,厘定为晚三叠世;岩石明显富集大离子亲石元素(Rb、Sr、Ba、K)、轻稀土元素和Pb,明显亏损高场强元素(如Nb、Ta、P、Ti),显示轻稀土元素强烈富集的右倾式稀土配分型式。结合东昆仑地区区域构造演化及金矿成矿年代学资料分析认为,西藏大沟金矿床花岗闪长斑岩形成于挤压向伸展转换阶段,西藏大沟金矿床成矿时间应介于225.0~218.6 Ma,属晚三叠世。Abstract: The Xizangdagou gold deposit lies in the Bayan Har tectonic belt of East Kunlun. LA-ICP-MS zircon U-Pb dating shows that the weighted mean age of granodiorite porphyry, which is closely related with the mineralization of the Xizangdagou gold deposit, is (225.0±1.2)Ma, in the Late Triassic. This suite of rocks are enriched in LILE (such as Rb, Sr, Ba, K), LREE and Pb, relatively depleting in HFSE (such as Nb, Ta, P, Ti), with rich LREE and low HREE. Based on the study of evolutionary characteristics of regional structures and chronologic data of gold deposits in East Kunlun, the authors suggest that the granodiorite porphyry in the Xizangdagou gold deposit was formed under a conversion tectonic setting from compressional to extensional, and the Xizangdagou gold deposit formed at 225.0~218.6 Ma, in the Late Triassic.
-
Key words:
- geochemistry /
- zircon U-Pb dating /
- granodiorite porphyry /
- Xizangdagou /
- East Kunlun
-
图 6 西藏大沟花岗闪长斑岩的微量元素原始地幔标准化蛛网图及稀土元素球粒陨石标准化配分曲线图(标准化数值据文献[29])
Figure 6. Primitive mantle-normalized trace element patterns and chondrite-normalized REE patterns of Xizangdagou granodiorite porphyry
表 1 西藏大沟花岗闪长斑岩主量元素(wt%)和微量元素含量(10-6)
Table 1. Contents of major elements(wt%)and trace elements(×10-6)of the Xizangdagou granodiorite porphyry
编号 14XZH01 14XZH02 14XZH03 14XZH04 14XZH05 编号 14XZH01 14XZH02 14XZH03 14XZH04 14XZH05 SiO2 61.37 63.20 63.04 63.81 63.40 Zr 85.80 115.00 105.00 104.00 112.00 TiO2 0.45 0.47 0.52 0.48 0.48 Hf 2.84 3.49 3.26 3.12 3.36 Al2O3 15.49 16.18 16.55 16.62 16.58 Y 11.00 11.40 12.60 12.30 10.60 Fe2O3 0.50 0.42 0.93 0.50 0.34 La 19.20 19.20 20.60 20.40 18.70 FeO 3.57 3.44 3.30 3.45 3.49 Ce 36.60 34.20 38.20 38.90 34.80 MnO 0.10 0.09 0.08 0.09 0.07 Pr 3.93 3.84 4.31 4.28 3.82 MgO 4.03 3.22 3.22 2.85 2.83 Nd 13.80 13.50 16.00 15.90 13.60 CaO 5.50 4.65 5.02 4.99 3.32 Sm 2.81 2.84 3.24 3.06 2.82 Na2O 3.10 3.00 3.05 3.25 2.98 Eu 0.97 0.92 1.07 1.08 0.73 K2O 1.42 1.86 2.02 1.80 2.23 Gd 2.72 2.65 2.93 3.06 2.53 P2O5 0.12 0.12 0.14 0.12 0.13 Tb 0.43 0.43 0.46 0.46 0.40 LOI 4.36 3.33 2.12 2.01 4.13 Dy 2.11 2.15 2.53 2.38 2.18 Total 100.01 99.98 99.99 99.97 99.98 Ho 0.42 0.43 0.50 0.48 0.44 A/CNK 0.931 1.05 1.013 1.015 1.242 Er 1.20 1.20 1.39 1.31 1.20 Rb 57.30 77.80 72.90 75.60 97.60 Tm 0.18 0.18 0.21 0.20 0.18 Ba 572.00 535.00 636.00 562.00 434.00 Yb 1.17 1.20 1.34 1.32 1.16 Th 6.19 6.55 6.57 6.94 6.86 Lu 0.18 0.18 0.21 0.20 0.18 U 2.63 2.76 2.32 2.96 3.01 ΣREE 85.72 82.92 92.99 93.03 82.74 Ta 0.80 0.78 0.75 0.74 0.73 LREE/HREE 9.19 8.85 8.72 8.89 9.00 Nb 9.92 10.10 9.62 9.61 8.76 LaN/YbN 11.77 11.48 11.03 11.09 11.56 Pb 14.60 12.00 15.60 15.20 16.60 δEu 1.07 1.03 1.06 1.08 0.84 Sr 457.00 458.00 401.00 413.00 308.00 δCe 1.03 0.98 0.99 1.02 1.01 表 2 西藏大沟金矿床花岗闪长斑岩锆石LA-ICP-MS测年结果
Table 2. LA-ICP-MS dating data of zircons from the Xizangdagou granodiorite porphyry
样品编号 含量/10-6 Th/U 207Pb/206Pb 207Pb/235U 206Pb/238U 207Pb/206Pb 207Pb/235U 206Pb/238U 232Th 238U 比值 1σ 比值 1σ 比值 1σ 年龄/Ma 1σ 年龄/Ma 1σ 年龄/Ma 1σ 14XZDG-1 68.2 389.5 0.18 0.0481 0.0010 0.2359 0.0050 0.0356 0.0005 102.1 47.9 215.0 4.1 225.4 3.4 14XZDG-2 81.3 549.4 0.15 0.0514 0.0010 0.2529 0.0050 0.0357 0.0005 258.5 42.7 228.9 4.0 226.0 3.3 14XZDG-3 94.3 458.4 0.21 0.0525 0.0010 0.2579 0.0051 0.0356 0.0005 308.5 41.9 232.9 4.1 225.5 3.3 14XZDG-4 151.5 1133.3 0.13 0.0517 0.0008 0.2526 0.0043 0.0354 0.0005 273.1 35.0 228.7 3.5 224.3 3.2 14XZDG-5 76.4 724.2 0.11 0.0521 0.0010 0.2539 0.0050 0.0354 0.0005 288.3 42.1 229.8 4.0 224.0 3.3 14XZDG-6 112.0 760.7 0.15 0.0499 0.0008 0.2452 0.0044 0.0356 0.0005 191.5 37.7 222.7 3.6 225.6 3.2 14XZDG-7 121.1 748.0 0.16 0.0495 0.0008 0.2435 0.0043 0.0357 0.0005 171.6 37.7 221.3 3.5 226.0 3.2 14XZDG-8 197.0 1092.2 0.18 0.0501 0.0008 0.2454 0.0043 0.0355 0.0005 200.7 37.0 222.8 3.5 224.9 3.2 14XZDG-9 193.6 870.5 0.22 0.0513 0.0009 0.2509 0.0046 0.0354 0.0005 255.8 38.4 227.3 3.7 224.5 3.2 14XZDG-10 109.7 611.5 0.18 0.0499 0.0009 0.2441 0.0045 0.0355 0.0005 187.8 39.0 221.8 3.6 224.9 3.2 14XZDG-11 128.1 840.2 0.15 0.0491 0.0008 0.2422 0.0044 0.0358 0.0005 151.6 39.1 220.2 3.6 226.6 3.2 14XZDG-12 115.7 557.6 0.21 0.0519 0.0011 0.2536 0.0054 0.0355 0.0006 279.0 46.4 229.5 4.3 224.6 3.4 14XZDG-14 292.9 1310.7 0.22 0.0511 0.0017 0.2516 0.0080 0.0357 0.0007 246.7 74.7 227.8 6.5 226.0 4.2 14XZDG-15 97.9 771.1 0.13 0.0509 0.0011 0.2516 0.0057 0.0359 0.0006 235.4 50.5 227.8 4.6 227.1 3.5 14XZDG-16 173.9 774.2 0.22 0.0514 0.0010 0.2472 0.0049 0.0349 0.0005 257.9 42.8 224.3 4.0 221.1 3.3 14XZDG-17 257.1 990.7 0.26 0.0515 0.0010 0.2511 0.0051 0.0354 0.0005 263.0 44.8 227.5 4.2 224.0 3.4 14XZDG-18 150.9 1032.4 0.15 0.0507 0.0008 0.2470 0.0044 0.0353 0.0005 227.4 37.3 224.1 3.6 223.7 3.2 14XZDG-19 155.2 864.0 0.18 0.0516 0.0010 0.2536 0.0049 0.0356 0.0005 268.1 42.1 229.5 4.0 225.7 3.3 14XZDG-20 209.7 1348.9 0.16 0.0489 0.0008 0.2393 0.0042 0.0355 0.0005 142.3 37.2 217.8 3.4 224.8 3.2 14XZDG-21 90.7 597.6 0.15 0.0515 0.0008 0.2510 0.0045 0.0354 0.0005 260.9 37.2 227.4 3.6 224.1 3.2 14XZDG-22 143.6 817.6 0.18 0.0503 0.0010 0.2464 0.0052 0.0355 0.0005 208.7 47.0 223.7 4.2 225.0 3.4 14XZDG-23 112.1 868.9 0.13 0.0520 0.0010 0.2569 0.0052 0.0358 0.0005 286.7 44.6 232.2 4.2 226.8 3.4 14XZDG-24 275.9 1263.1 0.22 0.0520 0.0016 0.2544 0.0075 0.0355 0.0007 283.0 68.7 230.2 6.1 225.0 4.0 14XZDG-25 57.2 485.9 0.12 0.0505 0.0010 0.2455 0.0050 0.0352 0.0005 219.4 45.2 222.9 4.1 223.2 3.3 14XZDG-26 79.0 532.1 0.15 0.0506 0.0012 0.2473 0.0060 0.0354 0.0006 223.4 55.1 224.4 4.9 224.4 3.6 14XZDG-27 203.2 1235.9 0.16 0.0507 0.0009 0.2477 0.0047 0.0355 0.0005 225.7 40.5 224.7 3.8 224.6 3.2 14XZDG-28 250.1 1017.6 0.25 0.0497 0.0007 0.2450 0.0040 0.0358 0.0005 179.4 33.5 222.5 3.3 226.5 3.1 14XZDG-29 95.4 602.4 0.16 0.0505 0.0009 0.2483 0.0045 0.0357 0.0005 218.5 39.1 225.2 3.7 225.8 3.2 14XZDG-30 130.0 776.8 0.17 0.0483 0.0012 0.2354 0.0060 0.0354 0.0006 112.0 59.6 214.6 4.9 224.0 3.6 -
[1] 姜春发, 王宗起, 李锦轶, 等.中央造山带开合构造[M].北京:地质出版社, 2000, 1~54.JIANG Chunfa, WANG Zongqi, LI Jinyi, et al. Opening-closing tectonics of the central orogenic belt[M]. Beijing:Geological Publishing House, 2000, 1~54. (in Chinese) [2] 莫宣学, 罗照华, 邓晋福, 等.东昆仑造山带花岗岩及地壳生长[J].高校地质学报, 2007, 13(3):403~414. https://www.wenkuxiazai.com/doc/e563188071fe910ef12df80b-4.htmlMO Xuanxue, LUO Zhaohua, DENG Jinfu, et al. Granitoids and crustal growth in the East-Kunlun Orogenic Belt[J]. Geological Journal of China Universities, 2007, 13(3):403~414. (in Chinese with English abstract) https://www.wenkuxiazai.com/doc/e563188071fe910ef12df80b-4.html [3] 李金超. 青海东昆仑地区金矿成矿规律及成矿预测[D]. 西安: 长安大学, 2017. http://cdmd.cnki.com.cn/Article/CDMD-10710-1017869244.htmLI Jinchao. Metallogenic regularity and metallogenic prognosis of gold deposit in the East Kunlun orogen, Qinghai Province[D]. Xi'an: Chang'an University, 2017. (in Chinese with English abstract) http://cdmd.cnki.com.cn/Article/CDMD-10710-1017869244.htm [4] 李金超, 孔会磊, 栗亚芝, 等.青海东昆仑瑙木浑金矿蚀变绢云母Ar-Ar年龄、石英闪长岩锆石U-Pb年龄和岩石地球化学特征[J].地质学报, 2017, 91(5):979~991. http://www.cnki.com.cn/Article/CJFDTOTAL-NFGT201703006.htmLI Jinchao, KONG Huilei, LI Yazhi, et al. Ar-Ar age of altered sericite, zircon U-Pb age of quartz diorite and geochemistry of the Naomuhun gold deposit, East Kunlun[J]. Acta Geologica Sinica, 2017, 91(5):979~991. (in Chinese with English abstract) http://www.cnki.com.cn/Article/CJFDTOTAL-NFGT201703006.htm [5] 李碧乐, 孙丰月, 于晓飞, 等.东昆中隆起带东段闪长岩U-Pb年代学和岩石地球化学研究[J].岩石学报, 2012, 28(4):1163~1172. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201204013LI Bile, SUN Fengyue, YU Xiaofei, et al. U-Pb dating and geochemistry of diorite in the eastern section from eastern Kunlun middle uplifted basement and granitic belt[J]. Acta Petrologica Sinica, 2012, 28(4):1163~1172. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201204013 [6] 岳维好. 东昆仑东段沟里金矿集区典型矿床地质地球化学及成矿机理研究[D]. 昆明: 昆明理工大学, 2013. http://cdmd.cnki.com.cn/Article/CDMD-10674-1014178547.htmYUE Weihao. Mineral deposits geochemistry and metallogenic mechanism in Gouli Gold Deposit, East Kunlun[D]. Kunming: Kunming University of Science and Technology, 2013. (in Chinese) http://cdmd.cnki.com.cn/Article/CDMD-10674-1014178547.htm [7] 李金超, 贾群子, 杜玮, 等.东昆仑东段阿斯哈矿床石英闪长岩LA-ICP-MS锆石U-Pb定年及岩石地球化学特征[J].吉林大学学报(地球科学版), 2014, 44(4):1188~1199. http://www.oalib.com/paper/4355282LI Jinchao, JIA Qunzi, DU Wei, et al. LA-ICP-MS zircon dating and geochemical characteristics of quartz diorite in Asiha gold deposit in East Segment of the Eastern Kunlun[J]. Journal of Jilin University (Earth Science Edition), 2014, 44(4):1188~1199. (in Chinese with English abstract) http://www.oalib.com/paper/4355282 [8] 李金超, 杜玮, 孔会磊, 等.青海省东昆仑大水沟金矿英云闪长岩锆石U-Pb测年、岩石地球化学及其找矿意义[J].中国地质, 2015, 42(3):509~520. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi201503009LI Jinchao, DU Wei, KONG Huilei, et al. Zircon U-Pb dating and geochemical characteristics of the Tonalite in the Dashuigou gold deposit of Eastern Kunlun Mountains, Qinghai Province[J]. Geology in China, 2015, 42(3):509~520. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=zgdizhi201503009 [9] 南卡俄吾, 贾群子, 李文渊, 等.青海东昆仑哈西亚图铁多金属矿区石英闪长岩LA-ICP-MS锆石U-Pb年龄和岩石地球化学特征[J].地质通报, 2014, 33(6):841~849. http://industry.wanfangdata.com.cn/dl/Detail/Periodical?id=Periodical_zgqydz201406007NAMKHA Norbu, JIA Qunzi, LI Wenyuan, et al. LA-ICP-MS zircon U-Pb age and geochemical characteristics of quartz diorite from the Haxiyatu iron-polymetallic ore district in Eastern Kunlun[J]. Geological Bulletin of China, 2014, 33(6):841~849. (in Chinese with English abstract) http://industry.wanfangdata.com.cn/dl/Detail/Periodical?id=Periodical_zgqydz201406007 [10] 胡荣国, 赖健清, 张绍宁, 等.青海省都兰县果洛龙洼金矿床地质地球化学特征[J].地质与勘探, 2010, 46(5):931~941. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzykt201005019HU Rongguo, LAI Jianqing, ZHANG Shaoning, et al. Geological and geochemical characteristics of the Guoluolongwa gold deposit, Dulan county, Qinghai Province[J]. Geology and Exploration, 2010, 46(5):931~941. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzykt201005019 [11] 李碧乐, 沈鑫, 陈广俊, 等.青海东昆仑阿斯哈金矿Ⅰ号脉成矿流体地球化学特征和矿床成因[J].吉林大学学报(地球科学版), 2012, 42(6):1676~1687. http://www.cnki.com.cn/Article/CJFDTotal-CCDZ201206013.htmLI Bile, SHEN Xin, CHEN Guangjun, et al. Geochemical features of ore-forming fluids and metallogenesis of vein Ⅰin Asiha gold ore deposit, Eastern Kunlun, Qinghai Province[J]. Journal of Jilin University (Earth Science Edition), 2012, 42(6):1676~1687. (in Chinese with English abstract) http://www.cnki.com.cn/Article/CJFDTotal-CCDZ201206013.htm [12] 丁清峰, 王冠, 孙丰月, 等.青海省曲麻莱县大场金矿床成矿流体演化:来自流体包裹体研究和毒砂地温计的证据[J].岩石学报, 2010, 26(12):3709~3719. http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20101221DING Qingfeng, WANG Guan, SUN Fengyue, et al. Ore-forming fluid evolution of Dachang gold deposit in Qumalai County, Qinghai Province:evidence from fluid inclusion study and arsenopyrite geothermometer[J]. Acta Petrologica Sinica, 2010, 26(12):3709~3719. (in Chinese with English abstract) http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20101221 [13] 丁清峰, 金圣凯, 王冠, 等.青海省都兰县果洛龙洼金矿成矿流体[J].吉林大学学报(地球科学版), 2013, 43(2):415~426. http://www.oalib.com/paper/4355465DING Qingfeng, JIN Shengkai, WANG Guan, et al. Ore-forming fluid of the Guoluolongwa gold deposit in Dulan County, Qinghai province[J]. Journal of Jilin University (Earth Science Edition), 2013, 43(2):415~426. (in Chinese with English abstract) http://www.oalib.com/paper/4355465 [14] 丰成友, 张德全, 李大新, 等.青海东昆仑造山型金矿硫、铅同位素地球化学[J].地球学报, 2003, 24(6):593~598. http://www.oalib.com/paper/4893595FENG Chengyou, ZHANG Dequan, LI Daxin, et al. Sulfur and lead isotope geochemistry of the orogenic gold deposits in East Kunlun area, Qinghai Province[J]. Acta Geoscientica Sinica, 2003, 24(6):593~598. (in Chinese with English abstract) http://www.oalib.com/paper/4893595 [15] Ding Q F, Jiang S Y, Sun F Y, et al. Origin of the Dachang gold deposit, NW China:constraints from H, O, S, and Pb isotope data[J]. International Geology Review, 2013, 55(15):1885~1901. doi: 10.1080/00206814.2013.804687 [16] 赵俊伟. 青海东昆仑造山带造山型金矿床成矿系列研究[D]. 长春: 吉林大学, 2008. http://cdmd.cnki.com.cn/article/cdmd-10183-2008126364.htmZHAO Junwei. Study on orogenic gold mettallogenic series in Eastern Kunlun orogenic belt, Qinghai Province[D]. Changchun: Jilin University, 2008. (in Chinese with English abstract) http://cdmd.cnki.com.cn/article/cdmd-10183-2008126364.htm [17] 袁万明, 王世成, 王兰芬.东昆仑五龙沟金矿床成矿热历史的裂变径迹热年代学证据[J].地球学报, 2000, 21(4):389~395. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqxb200004008YUAN Wanming, WANG Shicheng, WANG Lanfen. Metallogenic thermal history of the Wulonggou gold deposits in East Kunlun Mountains in the light of fission track thermochronology[J]. Acta Geoscientia Sinica, 2000, 21(4):389~395. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqxb200004008 [18] 丰成友. 青海东昆仑地区的复合造山过程及造山型金矿床成矿作用[D]. 北京: 中国地质科学院, 2002. http://cdmd.cnki.com.cn/Article/CDMD-82501-2007213482.htmFENG Chengyou. Multiple orogenic processes and mineralization of orogenic gold deposits in the East Kunlun orogen, Qinghai Province[D]. Beijing: Chinese Academy of Geologecal Sciences, 2002. (in Chinese with English abstract) http://cdmd.cnki.com.cn/Article/CDMD-82501-2007213482.htm [19] 张德全, 党兴彦, 佘宏全, 等.柴北缘-东昆仑地区造山型金矿床的Ar-Ar测年及其地质意义[J].矿床地质, 2005, 24(4):87~98. http://www.oalib.com/paper/4573062ZHANG Dequan, DANG Xingyan, SHE Hongquan, et al. Ar-Ar dating of orogenic gold deposits in northern margin of Qaidam and East Kunlun mountains and its geological significance[J]. Mineral Deposits, 2005, 24(4):87~98. (in Chinese with English abstract) http://www.oalib.com/paper/4573062 [20] 肖晔, 丰成友, 李大新, 等.青海省果洛龙洼金矿区年代学研究与流体包裹体特征[J].地质学报, 2014, 88(5):895~902. http://www.oalib.com/paper/4885599XIAO Ye, FENG Chengyou, LI Daxin, et al. Chronology and fluid inclusions of the Guoluolongwa gold deposit in Qinghai Province[J]. Acta Geologica Sinica, 2014, 88(5):895~902. (in Chinese with English abstract) http://www.oalib.com/paper/4885599 [21] 刘具仓. 青海省格尔木市西藏大沟南金成矿地质特征与找矿标志[D]. 北京: 中国地质大学(北京), 2013. http://cdmd.cnki.com.cn/Article/CDMD-11415-1014125456.htmLIU Jucang. Gold metallogenic geological characteristics and ore-prospecting criterian south of Tibet gully, in Golmud Qinghai province[D]. Beijing: China University of Geosciences (Beijing), 2013. (in Chinese with English abstract) http://cdmd.cnki.com.cn/Article/CDMD-11415-1014125456.htm [22] 梁亚运. 胶东早白垩世基性脉岩岩石成因与成矿动力学驱动[D]. 北京: 中国地质大学(北京), 2017. http://cdmd.cnki.com.cn/Article/CDMD-11415-1017126694.htmLIANG Yayun. Petrogenesis of the Early Cretaceous Mafic Dikes and Metallogenic Dynamics in Jiaodong Peninsula[D]. Beijing: China University of Geosciences (Beijing), 2017. (in Chinese with English abstract) http://cdmd.cnki.com.cn/Article/CDMD-11415-1017126694.htm [23] Goldfarb R J, Taylor R D, Collins G S, et al. Phanerozoic continental growth and gold metallogeny of Asia[J]. Gondwana Research, 2014, 25(1):48~102. doi: 10.1016/j.gr.2013.03.002 [24] 杨立强, 邓军, 王中亮, 等.胶东中生代金成矿系统[J].岩石学报, 2014, 30(9):2447~2467. http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20140901&journal_id=ysxbYANG Liqiang, DENG Jun, WANG Zhongliang, et al. Mesozoic gold metallogenic system of the Jiaodong gold province, eastern China[J]. Acta Petrologica Sinica, 2014, 30(9):2447~2467. (in Chinese with English abstract) http://www.ysxb.ac.cn/ysxb/ch/reader/view_abstract.aspx?file_no=20140901&journal_id=ysxb [25] 夏锐. 东昆仑古特提斯造山过程与金成矿作用[D]. 北京: 中国地质大学(北京), 2017. http://cdmd.cnki.com.cn/Article/CDMD-11415-1017126695.htmXIA Rui. Paleo-tethys orogenic process and gold metallogenesis of the East Kunlun[D]. Beijing: China University of Geosciences (Beijing), 2017. (in Chinese with English abstract) http://cdmd.cnki.com.cn/Article/CDMD-11415-1017126695.htm [26] Yang L Q, Deng J, Goldfarb R J, et al. 40Ar/39Ar geochronological constraints on the formation of the Dayingezhuang gold deposit:new implications for timing and duration of hydrothermal activity in the Jiaodong gold province, China[J]. Gondwana Research, 2014, 25(4):1469~1483. doi: 10.1016/j.gr.2013.07.001 [27] 张凯, 苟荣涛, 刘树林, 等.东昆仑大干沟一带铜金锑矿特征及找矿意义[J].地质力学学报, 2012, 18(4):401~409. http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20120405&flag=1ZHANG Kai, GOU Rongtao, LIU Shulin, et al. Characteristics and significance of the copper-gold-antimony deposits in Dagangou area, East Kunlun[J]. Journal of Geomechanics, 2012, 18(4):401~409. (in Chinese with English abstract) http://journal.geomech.ac.cn/ch/reader/view_abstract.aspx?file_no=20120405&flag=1 [28] 杜玉良, 贾群子, 韩生福.青海东昆仑成矿带中生代构造-岩浆-成矿作用及铜金多金属找矿研究[J].西北地质, 2012, 45(4):69~75. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xbdz201204007DU Yuliang, JIA Qunzi, HAN Shengfu. Mesozoic tectono-mineralization and copper-gold polymetallic ore prospecting research in East Kunlun metallogenic belt in Qinghai[J]. Northwestern Geology, 2014, 45(4):69~75. (in Chinese with English abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xbdz201204007 [29] 南卡俄吾, 贾群子, 李文渊, 等.青海省火成岩同位素地质年代学与构造岩浆热事件对比研究[J].西北地质, 2014, 47(2):51~61. doi: 10.3969/j.issn.1009-6248.2014.02.007NAMKHA Norbu, JIA Qunzi, LI Wenyuan, et al. A comparative study on isotopic geochronology and tectonic-magmatic hydrothermal events of igneous rock in Qinghai Province[J]. Northwestern Geology, 2014, 47(2):51~61. (in Chinese with English abstract) doi: 10.3969/j.issn.1009-6248.2014.02.007 [30] 孔会磊, 李金超, 栗亚芝, 等.青海东昆仑东段加当辉长岩LA-ICP-MS锆石U-Pb测年及其地质意义[J].地质与勘探, 2017, 53(5):889~902. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzkt201705006&dbname=CJFD&dbcode=CJFQKONG Huilei, LI Jinchao, LI Yazhi, et al. Zircon LA-ICP-MS U-Pb dating and its geological significance of the Jiadang gabbro in the eastern section of East Kunlun, Qinghai Province[J]. Geology and Exploration, 2017, 53(5):889~902. (in Chinese with English abstract) http://kns.cnki.net/KCMS/detail/detail.aspx?filename=dzkt201705006&dbname=CJFD&dbcode=CJFQ [31] 孔会磊, 李金超, 栗亚芝, 等.青海东昆仑哈陇休玛辉石橄榄岩LA-ICP-MS锆石U-Pb测年及其地质意义[J].地质科技情报, 2017, 36(1):41~47. http://mall.cnki.net/magazine/magadetail/DZKQ201701.htmKONG Huilei, LI Jinchao, LI Yazhi, et al. Zircon LA-ICP-MS U-Pb dating and its geological significance of the Halongxiuma pyroxene peridotite in East Kunlun, Qinghai Province[J]. Geological Science and Technology Information, 2017, 36(1):41~47. (in Chinese with English abstract) http://mall.cnki.net/magazine/magadetail/DZKQ201701.htm [32] 张斌, 孔会磊, 李智明, 等.东昆仑哈日扎铅锌多金属矿区英云闪长岩锆石U-Pb定年、地球化学及其地质意义[J].地质科技情报, 2016, 35(5):9~17. http://www.cqvip.com/QK/93477A/201605/670156659.htmlZHANG Bin, KONG Huilei, LI Zhiming, et al. Zircon U-Pb dating, geochemical and geological significance of the tonalites from the Harizha lead-zinc polymetallic mine in East Kunlun Mountains[J]. Geological Science and Technology Information, 2016, 35(5):9~17. (in Chinese with English abstract) http://www.cqvip.com/QK/93477A/201605/670156659.html [33] Sun S S, McDonough W F. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes[A]. Saunders A D, Norry M J. Magmatism in the Ocean Basins[M]. Geological Society, London, Special Publication, 1989, 42(1): 313~345. [34] McKenzie D. Some remarks on the movement of small melt fractions in the mantle[J]. Earth and Planetary Science Letters, 1989, 95(1/2):53~72. http://www.sciencedirect.com/science/article/pii/0012821X89901672 [35] Taylor S R, McLennan S M. The geochemical evolution of the continental crust[J]. Reviews of Geophysics, 1995, 33(2):241~265. http://www.researchgate.net/publication/264685686_The_geochemical_evolution_of_the_continental_crust [36] Rudnick L R, Fountain M D. Nature and composition of the continental crust:a lower crustal perspective[J]. Reviews of Geophysics, 1995, 33(3):267~309. doi: 10.1029/95RG01302/full [37] 郭正府, 邓晋福, 许志琴, 等.青藏东昆仑晚古生代末-中生代中酸性火成岩与陆内造山过程[J].现代地质, 1998, 12(3):344~352. http://www.cqvip.com/QK/96868X/1998003/3127961.htmlGUO Zhengfu, DENG Jinfu, XU Zhiqin, et al. Late Palaeozoic-Mesozoic intracontinental orogenic process and intermedate acidic igneous rocks from the Eastern Kunlun Mountains of Northwestern China[J]. Geoscience, 1998, 12(3):344~352. (in Chinese with English abstract) http://www.cqvip.com/QK/96868X/1998003/3127961.html [38] 孔会磊, 李金超, 黄军, 等.东昆仑小圆山铁多金属矿区斜长花岗斑岩锆石U-Pb测年、岩石地球化学及找矿意义[J].中国地质, 2015, 42(3):521~532. https://www.wenkuxiazai.com/doc/e68e3f8f0066f5335a8121f2.htmlKONG Huilei, LI Jinchao, HUANG Jun, et al. Zircon U-Pb dating and geochemical characteristics of the plagiogranite porphyry from the Xiaoyuanshan iron-polymetallic ore district in East Kunlun Mountains[J]. Geology in China, 2015, 42(3):521~532. (in Chinese with English abstract) https://www.wenkuxiazai.com/doc/e68e3f8f0066f5335a8121f2.html