新疆乌伦布拉克铜矿流体包裹体特征及含矿岩体年代学

孙万龙; 彭素霞; 白建科; 刘建朝; 王德明; 邵博琪; 李天石

doi:10.3799/dqkx.2018.166

新疆乌伦布拉克铜矿流体包裹体特征及含矿岩体年代学

doi: 10.3799/dqkx.2018.166

1.
长安大学地球科学与资源学院, 陕西西安 710054
2.
中国地质调查局西安地质调查中心, 陕西西安 710054
3.
新疆地矿局第二区域地质调查大队, 新疆昌吉 831100
4.
中国地质大学地球科学与资源学院, 北京 100083

基金项目:

陕西省自然科学基金项目 2018JM4001

中国地质调查局地质矿产调查评价项目 DD20160006

详细信息

作者简介:
孙万龙(1992-), 男, 硕士研究生, 矿物学、岩石学、矿床学专业

中图分类号: P53
计量
- 文章访问数: 5308
- HTML全文浏览量: 2251
- PDF下载量: 31
- 被引次数: 0
出版历程
- 收稿日期: 2018-03-31
- 刊出日期: 2018-12-15

Fluid Inclusions and Geochronology of Wulunbulake Copper Deposit in Xinjiang

1.
School of Earth Science and Resources, Chang'an University, Xi'an 710054, China
2.
Xi'an Center of Geological Survey, China Geological Survey, Xi'an 710054, China
3.
Regional Geological Survey Brigade No.2, Xinjiang Bureau of Geology and Mineral Resources, Changji 831100, China
4.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China

摘要

摘要: 乌伦布拉克铜矿位于新疆东准噶尔野马泉-琼河坝铜多金属成矿带中，其矿床成因和成矿时代存在较大争议，从流体包裹体和锆石U-Pb定年等方面做了研究探讨.矿床主要发育富液相包裹体，成矿流体为低温（136.9~224.5℃）、低盐度（1.7%~5.6% NaCl eqv.）、低密度（0.97~1.01 g/cm³）流体，估算的成矿压力为2.76×10⁷~4.49×10⁷ Pa，对应的成矿深度为1.04~1.95 km，属于浅成矿床.激光拉曼探针测试结果表明流体液相组分主要为水，气相组分除水蒸气外，还含有一定量CH₄、N₂和H₂.锆石U-Pb测年结果显示含矿石英闪长岩年龄为440.5±3.3 Ma，不含矿石英斑岩年龄为419.7±3.3 Ma，表明研究区至少经历了2期岩浆活动，成矿作用从早志留世就已开始.矿床由内向外发育典型的"斑岩型"蚀变分带（强硅化带-钾化带-绢英岩化带-青磐岩化带），表明乌伦布拉克铜矿为斑岩型铜矿，形成于志留纪古亚洲洋向南俯冲的岛弧环境.东准噶尔甚至新疆北部地区在志留纪处于岛弧环境，该时期的岩浆岩带是形成和寻找斑岩型铜矿的有利地区.
- 流体包裹体 /
- 锆石U-Pb定年 /
- 斑岩型铜矿 /
- 东准噶尔 /
- 地质年代学
Abstract: Wulunbulake copper deposit is located at the north-western segment of the Yemaquan-Qiongheba Cu-polymetallic metallogenic belt, East Junggar, Xinjiang. However, its genetic type and mineralizing age has been debated. This study presents new results on fluid inclusions and zircon U-Pb dating to precisely constrain the type and time of mineralization. The dominant fluid inclusions in Wulunbulake copper deposit are liquid-rich type, with low homogenization temperature (136.9-224.5℃), low salinity (1.7%~5.6% NaCl eqv.) and low density (0.97-1.01 g/cm³), the mineralizing pressure is 2.76×10⁷-4.49×10⁷ Pa and the corresponding depth is 1.04-1.95 km. The laser Raman spectroscopy results indicate that the ore-forming fluids consist of H₂O, CH₄, N₂, H₂. Zircon U-Pb dating results show that the formation age of ore-bearing quartz diorite and quartz porphyry is 440.5±3.3 Ma, and 419.7±3.3 Ma, respectively, indicating that there had experienced two-stage magmatic activities from Early Silurian. From the interior to the outer part of the deposit, there exist typical alteration zonation characteristics of porphyry deposits (silica alternation-potassic alternation-phyllic alternation-propylitization), and the geochemical characteristics of ore-bearing indicate that they were most possibly formed in arc setting. Its genetic type should be typical porphyry copper deposit and related to the southward subduction of the Paleo-Asian oceanic crust in the Early Silurian period. The East Junggar even northern Xinjiang was in the island arc environment in the Silurian, and the magmatic zone is a potential area for formation and prospecting of porphyritic Cu deposit.
- fluid inclusion /
- zircon U-Pb dating /
- porphyry copper deposit /
- East Junggar /
- geochronology

HTML全文

图 1 乌伦布拉克铜矿区域地质图(a)与矿区地质图(b)

Fig. 1. Regional geologic map (a) and ore district map (b) of Wulunbulake copper deposit

下载: 全尺寸图片幻灯片

图 2 乌伦布拉克铜矿区照片

a.砾岩与石英闪长岩不整合接触关系；b.砾岩中石英闪长岩砾石

Fig. 2. Photographs in Wulunbulake copper deposit

下载: 全尺寸图片幻灯片

图 3 乌伦布拉克铜矿矿石及蚀变照片

a.脉状-浸染状黄铁矿和黄铜矿矿石；b.脉状黄铁矿和黄铜矿矿石；c.浸染状斑铜矿、黄铜矿和黄铁矿；d.隐爆角砾岩中孔雀石化；e.强硅化石英闪长岩中发育脉状-浸染状黄铁矿和黄铜矿；f.钾化蚀变石英闪长岩中发育浸染状黄铁矿；g.黄铜矿充填于黄铁矿裂隙中；h.黄铜矿呈脉状分布于黄铁矿中；f.黄铜矿、黄铁矿与辉钼矿共生.Py.黄铁矿；Ccp.黄铜矿；Mlb.辉钼矿

Fig. 3. Various ore types and alterations in Wulunbulake copper deposit

下载: 全尺寸图片幻灯片

图 4 乌伦布拉克铜矿流体包裹体照片

L.液相；V.气相

Fig. 4. Photographs of the fluid inclusions from Wulunbulake copper deposit

下载: 全尺寸图片幻灯片

图 5 乌伦布拉克铜矿均一温度(a)及盐度分布直方图(b)

Fig. 5. Histograms of homogenization temperatures (a) and salinity (b) of the fluid inclusions from Wulunbulake copper deposit

下载: 全尺寸图片幻灯片

图 6 乌伦布拉克铜矿流体包裹体盐度-均一温度分布图(a)和氢氧同位素组成图解(b)

图b数据1引自喻亨祥等(1998)；数据2和3引自夏佐铎(2000)

Fig. 6. Homogenization-salinity (a) and δ¹⁸O vs. δD (b) diagrams of the fluid inclusions from Wulunbulake copper deposit

下载: 全尺寸图片幻灯片

图 7 乌伦布拉克铜矿流体包裹体拉曼光谱

Fig. 7. The laser Raman spectroscopy of the fluid inclusions from Wulunbulake copper deposit

下载: 全尺寸图片幻灯片

图 8 锆石阴极发光图像

圆圈为分析点位置

Fig. 8. Cathodoluminescence (CL) images of zircon

下载: 全尺寸图片幻灯片

图 9 锆石U-Pb年龄谐和图及²⁰⁶Pb/²³⁸U加权平均年龄

Fig. 9. Zircon U-Pb concordia diagrams and weighted mean ²⁰⁶Pb/²³⁸U ages

下载: 全尺寸图片幻灯片

表 1 乌伦布拉克铜矿流体包裹体显微测温数据及估算参数

Table 1. Microthermometric data and estimation parameters of the fluid inclusions in quartz from Wulunbulake copper deposit

样品编号	测试点号	寄主矿物	冰点温度(℃)	均一温度(℃)	校正后均一温度(℃)	盐度(% NaCl eqv.)	密度(g/cm³)	压力(10⁵ Pa)	深度(km)
	1		-3.4	144.6	194.6	5.6	1.00	389.5	1.47
	2		-3.4	136.3	186.3	5.6	1.01	367.3	1.39
WL1	3	石英	-2.8	135.4	185.4	4.6	1.00	361.0	1.36
	4		-2.8	135.4	185.4	4.6	1.00	361.0	1.36
	5		-2.6	133.0	183.0	4.3	0.99	353.1	1.33
	1		-1.8	137.2	162.2	3.1	0.98	354.4	1.34
	2		-1.7	135.5	160.5	2.9	0.97	348.2	1.31
	3		-1.7	135.4	160.4	2.9	0.97	348.0	1.31
WL2	4	石英	-2.0	138.7	163.7	3.4	0.98	361.4	1.36
	5		-1.2	130.5	155.5	2.1	0.97	323.1	1.22
	6		-1.2	130.1	155.1	2.1	0.97	322.3	1.22
	1		-2.4	155.7	210.7	4.0	0.98	411.0	1.55
	2		-2.5	169.5	224.5	4.2	0.97	448.8	1.69
WL3	3	石英	-1.2	115.3	138.3	2.1	0.98	285.6	1.08
	4		-1.2	114.0	137.0	2.1	0.98	282.4	1.07
	5		-1.0	113.9	136.9	1.7	0.98	275.6	1.04
	1		-2.0	135.5	160.5	3.4	0.98	353.0	1.33
	2		-1.8	131.5	156.5	3.1	0.98	339.7	1.28
	3		-1.8	131.5	156.5	3.1	0.98	339.7	1.28
WL4	4	石英	-1.5	130.4	155.4	2.6	0.97	331.1	1.25
	5		-1.5	130.3	155.3	2.6	0.97	330.9	1.25
	6		-1.3	130.1	155.1	2.2	0.97	325.3	1.23

下载: 导出CSV

表 2 石英闪长岩(WLBLK-2)和石英斑岩(WLBLK-3)LA-ICP-MS锆石U-Pb分析结果

Table 2. LA-ICP-MS zircon U-Pb data for the quartz diorite (WLBLK-2) and the quartz porphyry (WLBLK-3)

测试点	含量(10^-6)			Th/U	²⁰⁷Pb/²⁰⁶Pb		²⁰⁷Pb/²³⁵U		²⁰⁶Pb/²³⁸U		²⁰⁸Pb/²³²Th		²⁰⁶Pb/²³⁸U
测试点	Pb	Th	U	Th/U	比值	1σ	比值	1σ	比值	1σ	比值	1σ	年龄(Ma)	1σ
WLBLK-2-01	52.93	437.13	522.87	0.84	0.055 0	0.000 8	0.539 7	0.008 0	0.070 6	0.000 4	0.021 0	0.000 3	440	3
WLBLK-2-02	36.73	311.34	348.12	0.89	0.056 1	0.000 9	0.557 9	0.009 2	0.071 5	0.000 5	0.021 2	0.000 3	445	3
WLBLK-2-03	44.36	361.58	441.44	0.82	0.057 5	0.000 9	0.563 1	0.008 6	0.070 7	0.000 5	0.021 1	0.000 3	440	3
WLBLK-2-04	26.93	192.03	290.94	0.66	0.057 5	0.001 1	0.575 1	0.010 0	0.072 2	0.000 5	0.021 3	0.000 3	450	3
WLBLK-2-05	55.11	462.76	537.19	0.86	0.055 9	0.000 9	0.555 9	0.008 5	0.071 6	0.000 5	0.021 3	0.000 3	446	3
WLBLK-2-06	113.17	1 087.73	967.23	1.12	0.055 8	0.000 8	0.556 0	0.008 0	0.071 7	0.000 5	0.021 9	0.000 3	446	3
WLBLK-2-07	53.77	479.74	540.83	0.89	0.056 9	0.000 9	0.541 4	0.008 8	0.068 4	0.000 5	0.020 4	0.000 3	427	3
WLBLK-2-08	34.57	286.25	353.75	0.81	0.058 2	0.001 0	0.561 0	0.009 8	0.069 4	0.000 5	0.021 2	0.000 3	432	3
WLBLK-2-09	20.59	117.24	199.95	0.59	0.075 0	0.001 6	0.767 4	0.015 8	0.073 8	0.000 6	0.030 6	0.000 6	459	3
WLBLK-2-10	66.13	575.20	633.08	0.91	0.056 5	0.000 8	0.558 4	0.007 6	0.071 3	0.000 4	0.021 5	0.000 3	444	3
WLBLK-2-11	90.13	689.54	911.77	0.76	0.058 5	0.000 8	0.577 3	0.007 9	0.071 2	0.000 5	0.023 8	0.000 3	443	3
WLBLK-2-12	83.15	774.59	755.11	1.03	0.057 0	0.000 8	0.556 7	0.008 2	0.070 3	0.000 5	0.021 6	0.000 3	438	3
WLBLK-2-13	9.21	42.13	109.67	0.38	0.064 0	0.001 6	0.656 9	0.016 0	0.074 5	0.000 7	0.025 7	0.000 6	459	4
WLBLK-2-14	16.34	122.02	171.89	0.71	0.057 4	0.001 4	0.566 7	0.013 5	0.071 7	0.000 6	0.022 2	0.000 4	447	3
WLBLK-2-15	81.12	781.73	749.04	1.04	0.055 9	0.000 7	0.537 6	0.007 4	0.069 5	0.000 4	0.020 7	0.000 3	433	3
WLBLK-2-16	44.63	347.71	467.74	0.74	0.056 6	0.000 9	0.555 3	0.009 0	0.070 9	0.000 4	0.021 7	0.000 3	442	3
WLBLK-2-17	46.09	356.96	508.70	0.70	0.055 6	0.000 9	0.531 1	0.008 2	0.069 1	0.000 4	0.021 4	0.000 3	431	3
WLBLK-2-18	40.81	333.74	415.98	0.80	0.057 6	0.000 9	0.556 1	0.008 5	0.069 9	0.000 4	0.021 8	0.000 3	435	3
WLBLK-2-19	9.73	54.34	116.06	0.47	0.061 1	0.001 5	0.599 2	0.014 0	0.071 6	0.000 6	0.024 6	0.000 6	446	4
WLBLK-2-20	25.32	202.88	247.16	0.82	0.058 0	0.001 1	0.572 1	0.010 7	0.071 7	0.000 5	0.022 9	0.000 3	446	3
WLBLK-3-01	6.01	37.08	88.58	0.42	0.050 8	0.001 7	0.469 2	0.016 1	0.067 2	0.000 7	0.016 0	0.000 5	419	4
WLBLK-3-02	9.76	72.40	135.89	0.53	0.053 6	0.001 6	0.487 4	0.013 7	0.066 3	0.000 6	0.014 9	0.000 3	414	4
WLBLK-3-03	5.79	32.51	83.29	0.39	0.053 2	0.001 7	0.491 1	0.014 5	0.067 6	0.000 6	0.015 5	0.000 5	422	4
WLBLK-3-04	4.60	23.42	61.40	0.38	0.058 2	0.002 3	0.563 7	0.021 1	0.071 7	0.000 8	0.020 1	0.000 7	447	5
WLBLK-3-05	12.21	83.69	176.08	0.48	0.049 2	0.001 2	0.450 3	0.010 6	0.066 3	0.000 5	0.015 3	0.000 3	414	3
WLBLK-3-06	4.50	25.32	62.18	0.41	0.057 7	0.002 3	0.532 3	0.019 8	0.068 1	0.000 9	0.018 9	0.000 7	425	5
WLBLK-3-07	7.24	45.50	104.15	0.44	0.053 5	0.001 5	0.500 5	0.013 8	0.068 0	0.000 6	0.015 4	0.000 4	424	4
WLBLK-3-08	5.04	29.66	70.81	0.42	0.052 8	0.002 0	0.492 1	0.017 1	0.068 4	0.000 8	0.015 9	0.000 5	427	5
WLBLK-3-09	11.93	97.18	148.18	0.66	0.051 6	0.001 4	0.479 6	0.012 0	0.067 7	0.000 6	0.016 6	0.000 3	422	4
WLBLK-3-10	5.38	31.34	68.18	0.46	0.052 9	0.002 1	0.518 0	0.019 8	0.072 4	0.000 8	0.017 2	0.000 6	450	5
WLBLK-3-11	4.57	27.73	66.07	0.42	0.056 1	0.002 2	0.499 4	0.018 1	0.066 3	0.000 8	0.016 8	0.000 5	414	5
WLBLK-3-12	4.37	26.98	58.82	0.46	0.058 3	0.002 5	0.534 4	0.021 2	0.068 5	0.000 8	0.017 1	0.000 5	427	5
WLBLK-3-13	6.74	40.37	91.57	0.44	0.055 2	0.001 9	0.510 3	0.016 3	0.068 0	0.000 7	0.017 6	0.000 5	424	4
WLBLK-3-14	4.97	31.69	66.11	0.48	0.057 3	0.002 4	0.522 8	0.020 1	0.068 1	0.000 7	0.017 1	0.000 5	425	4
WLBLK-3-15	3.71	12.23	39.70	0.31	0.091 8	0.003 9	0.872 5	0.035 6	0.070 7	0.001 0	0.037 3	0.001 3	425	6
WLBLK-3-16	6.63	43.74	84.44	0.52	0.057 7	0.001 9	0.530 5	0.016 7	0.067 5	0.000 7	0.018 1	0.000 5	421	4
WLBLK-3-17	10.48	74.61	136.93	0.54	0.052 4	0.001 6	0.475 6	0.014 5	0.066 1	0.000 6	0.017 1	0.000 4	413	3
WLBLK-3-18	8.40	64.09	111.42	0.58	0.051 9	0.001 7	0.463 6	0.014 5	0.065 2	0.000 6	0.015 9	0.000 4	407	4
WLBLK-3-19	5.15	27.55	72.49	0.38	0.054 7	0.002 0	0.516 4	0.018 7	0.068 9	0.000 7	0.017 8	0.000 5	430	4
WLBLK-3-20	3.79	19.54	51.71	0.38	0.057 3	0.002 3	0.523 3	0.019 8	0.068 0	0.000 9	0.018 2	0.000 7	424	5

下载: 导出CSV

参考文献(65)

Chen, J., Xu, Y.B., Wang, F., et al., 2013.Mineralization Regularities of Porphyry Copper Deposits in Qiongheba Area, Xinjiang.Non-Ferrous Metals of Xinjiang, 36(S2):1-4(in Chinese).
Chen, W.F., Chen, P.R., Zhou, X.M., et al., 2006.Single-Zircon LA-ICP-MS U-Pb Dating of the Yangmingshan Granitic Pluton in Hunan, South China and Its Petrogenetic Study.Acta Geologica Sinica, 80(7):1065-1077(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dizhixb200607013
Cheng, Z.P., Liu, J.Y., 2007.Geologic and Geophysical Features of Wulunbulake Copper-Molybdenum Mine and Its Exploration.Journal of Guilin University of Technology, 27(4):463-468 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=glgxy200704001
Compston, W., Williams, I.S., Kirschvink, J.L., et al., 1992.Zircon U-Pb Ages for the Early Cambrian Time-Scale.Journal of the Geological Society, 149(2):171-184. https://doi.org/10.1144/gsjgs.149.2.0171
Dong, L.H., Xu, X.W., Qu, X., et al., 2009.Tectonic Setting and Formation Mechanism of the Circum-Junggar Porphyritic Copper Deposit Belts.Acta Petrologica Sinica, 25(4):713-737 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200904001
Du, S.J., Qu, X., Deng, G., et al., 2010.Chronology and Tectonic Setting of the Intrusive Bodies and Associated Porphyry Copper Deposit in Hersai Area, Eastern Junggar.Acta Petrologica Sinica, 26(10):2981-2996(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201010010
Guo, L.S., Zhang, R., Liu, Y.L., et al., 2009.Zircon U-Pb Age of Tonghualing Intermediate-Acid Intrusive Rocks, Eastern Junggar, Xinjiang.Acta Scientiarum Naturalium Universitatis Pekinensis, 45(5):819-824(in Chinese with English abstract).https://doi.org/10.13209/j.0479-8023.2009.122 http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK200902455571
Hall, D.L., Sterner, S.M., Bodnar, R.J., 1988.Freezing Point Depression of NaCl-KCl-H₂O Solutions.Economic Geology, 83(1):197-202. https://doi.org/10.2113/gsecongeo.83.1.197
Li, J.X., Qin, K.Z., Li, G.M., et al., 2006.Basic Characteristics of Gold-Rich Porphyry Copper Deposits and Their Ore Sources and Evolving Processes of High Oxidation Magma and Ore-Forming Fluid.Acta Petrologica Sinica, 22(3):678-688(in Chinese with English abstract). http://cpfd.cnki.com.cn/Article/CPFDTOTAL-DZDQ200702001157.htm
Liu, B., Duan, G.X., 1987.The Density and Isochoric Formulae for NaCl-H₂O Fluid Inclusions and Their Application.Acta Mineralogica Sinica, 7(4):345-352(in Chinese with English abstract).https://doi.org/10.16461/j.cnki.1000-4734.1987.04.011
Liu, X.L., Li, W.C., Yin, G.H., et al., 2013.The Geochronology, Mineralogy and Geochemistry Study of the Pulang Porphyry Copper Deposit in Geza Arc of Yunnan Province.Acta Petrologica Sinica, 29(9):3049-3064(in Chinese with English abstract).
Lu, H.Z., Fan, H.R., Ni, P., et al., 2004.Fluid Inclusions.Science Press, Beijing, 11-274 (in Chinese).
Ohmoto, H., 1986.Stable Isotope Geochemistry of Ore Deposits.Reviews in Mineralogy, 16(6):491-559. http://d.old.wanfangdata.com.cn/Periodical/kwysdqhxtb201801010
Pattrick, R.A.D., 1986.A Practical Guide to Fluid Inclusion Studies.Mineralogical Magazine, 50(356):352-353. https://doi.org/10.1180/minmag.1986.050.356.32
Potter, R.W., 1977.Pressure Correction for Fluid Inclusion Homogenization Based on the Volumetre Properties of the System NaCl-H₂O.J.Res.vs.Geol.Surv., 5:603-607.
Qu, X., 2011.Mineralization Regularities and Prediction of Targets of Porphyry Copper Deposits in East Junggar, Xinjiang, China (Dissertation).China University of Geosciences, Beijing (in Chinese with English abstract).
Qu, X., Xu, X.W., Liang, G.L., et al., 2009.Geological and Geochemical Characteristics of the Mengxi Cu-Mo Deposit and Its Constraint to Tectonic Setting of the Qiongheba Magmatic Arc in Eastern Junggar, Xinjiang.Acta Petrologica Sinica, 25(4):765-776(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98200904004
Shao, J.L., 1988.Prospecting Mineralogy of Gold Deposits.China University of Geosciences Press, Wuhan, 38-45(in Chinese).
Shen, P., Dong, L.H., Feng, J., et al., 2010.Distribution, Age and Metallogenic Characteristics of the Porphyry Copper Deposits in Xinjiang, China.Xinjiang Geology, 28(4):358-364(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=xjdz201004003
Sun, S.D., Chen, C., Du, J.S., et al., 2016.Magneitc Characteristics and Tectonic Implications of Crust in Junggar Basin and Its Surroundings.Earth Science, 41(7):1216-1224(in Chinese with English abstract).https://doi.org/10.3799/dqkx.2016.099 http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-DQKX201607011.htm
Sun, W.D., Arculus, R.J., Kamenetsky, V.S., et al., 2004.Release of Gold-Bearing Fluids in Convergent Margin Magmas Prompted by Magnetite Crystallization.Nature, 431(7011):975-978. https://doi.org/10.1038/nature02972
Tang, G.J., Wang, Q., Zhao, Z.H., et al., 2009.Geochronology and Geochemistry of the Ore-Bearing Porphyries in the Baogutu Area(Western Junggar):Petrogenesis and Their Implications for Tectonics and Cu-Au Mineralization.Earth Science, 34(1):56-74(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dqkx200901007
Wang, J., Li, T.D., Geng, S.F., et al., 2010.Geological Characteristics and Genesis of Porphyry Copper Deposits in East Junggar Region.Acta Geoscientica Sinica, 31(3):423-433(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqxb201003015
Xia, Z.D., 2000.The Characteristic of Ore-Bearing Magma and Cu-Mo Metallization in Wulunbulake, Xinjinag (Dissertation).Guilin University of Technology, Guilin (in Chinese).
Xiao, W.J., Han, C.M., Yuan, C., et al., 2006.Unique Carboniferous-Permian Tectonic-Metallogenic Framework of Northern Xinjiang (NW China):Constraints for the Tectonics of the Southern Paleoasian Domain.Acta Petrologica Sinica, 22(5):1062-1076(in Chinese with English abstract).
Xiao, W.J., Windley, B.F., Yuan, C., et al., 2009.Paleozoic Multiple Subduction-Accretion Processes of the Southern Altaids.American Journal of Science, 309(3):221-270. https://doi.org/10.2475/03.2009.02
Xu, Q.Q., Zhao, L., Niu, B.G., et al., 2015.Determination of the Early Paleozoic Granite in Zhifang Area, East Junggar, Xinjiang and Its Geological Implications.Journal of Geomechanics, 21(4):502-516(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dzlxxb201504006
Xu, X.W., Dong, L.H., Qu, X., et al., 2013.Metallogenetic Regularity and Prognosis of Porphyry Copper Deposit in the East Junggar.Geological Publishing House, Beijing, 21-56(in Chinese).
Xu, X.W., Wu, Q., Huang, X.F., et al., 2012.Formation Mechanism and Evolution Process of Copper-Rich Porphyry Magma.Acta Petrologica Sinica, 28(2):421-432(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201202007
Xu, X.W., Zhang, B.L., Liang, G.H., et al., 2012.Zoning of Mineralization in Hypogene Porphyry Copper Deposits:Insight from Comb Microfractures within Quartz-Chalcopyrite Veins in the Hongshan Porphyry Cu Deposit, Western Yunnan, SW China.Journal of Asian Earth Sciences, 56:218-228. https://doi.org/10.1016/j.jseaes.2012.05.017
Yang, L.Q., Deng, J., Ge, L.S., et al., 2007a.Metallogenic Epoch and Genesis of the Gold Deposits in Jiaodong Peninsula, Eastern China:A Regional Review.Progress in Natural Science, 17(2):138-143. https://doi.org/10.1080/10020070612331343237
Yang, L.Q., Deng, J., Zhang, J., et al., 2007b.Preliminary Studies of Fluid Inclusions in Damoqujia Gold Deposit along Zhaoping Fault Zone, Shandong Province, China.Acta Petrologica Sinica, 23(1):153-160.
Yang, L.Q., Deng, J., Guo, C.Y., et al., 2009.Ore-Forming Fluid Characteristics of the Dayingezhuang Gold Deposit, Jiaodong Gold Province, China.Resource Geology, 59(2):181-193.https://doi.org/10.1111/j.1751-3928.2009.00089.x doi: 10.1111/rge.2009.59.issue-2
Yu, H.X., Lin, J.F., Liu, J.Y., et al., 1998.Metallogenic Features of the Wulunbulake Porphyry Copper Deposit Hosted in Cryptoexplosion Baeccia Pipe, Xinjiang.Geology and Prospecting, 34(5):8-13(in Chinese with English abstract).
Yu, H.X., Xia, B., Liu, J.Y., et al., 2002.Geochemistry of the Wulunbulake Copper Ore Deposit and Its Genesis, Xinjiang, China.Geotectonic et Metallogenia, 26(2):172-178(in Chinese with English abstract).
Zhai, Y.S., 1999.On the Metallogenic System.Earth Sciencce Frontiers, 6(1):13-27(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/dxqy201002003
Zhang, R.F., Yuan, F., Zhou, T.F., et al., 2015.Geological Characteristics, Geochronology and Geochemical Characteristics of Volcanic Hydrothermal Type Copper Deposits (Points) in Taerbahatai-Xiemisitai Region, West Junggar.Acta Petrologica Sinica, 31(8):2259-2276(in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201508010
Zhang, Y., Liang, G.L., Qu, X., et al., 2010.Evidence of U-Pb Age and Hf Isotope of Zircons for Early Paleozoic Magmatism in the Qiongheba Arc, East Junggar.Acta Petrologica Sinica, 26(8):2389-2398(in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=ysxb98201008013
陈疆, 徐永波, 王芳, 等, 2013.新疆琼河坝地区斑岩型铜矿成矿规律研究.新疆有色金属, 36(S2):1-4. http://d.old.wanfangdata.com.cn/Periodical/xjysjs2013z1001
陈卫锋, 陈培荣, 周新民, 等, 2006.湖南阳明山岩体的LA-ICP-MS锆石U-Pb定年及成因研究.地质学报, 80(7):1065-1077. doi: 10.3321/j.issn:0001-5717.2006.07.013
程志平, 刘家远, 2007.乌伦布拉克铜钼矿床地质地球物理特征及扩大找矿前景.桂林工学院学报, 27(4):463-468. doi: 10.3969/j.issn.1674-9057.2007.04.001
董连慧, 徐兴旺, 屈迅, 等, 2009.初论环准噶尔斑岩铜矿带的地质构造背景与形成机制.岩石学报, 25(4):713-737. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200904001
杜世俊, 屈迅, 邓刚, 等, 2010.东准噶尔和尔赛斑岩铜矿成岩成矿时代与形成的构造背景.岩石学报, 26(10):2981-2996. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201010010
郭丽爽, 张锐, 刘玉琳, 等, 2009.新疆东准噶尔铜华岭中酸性侵入体锆石U-Pb年代学研究.北京大学学报(自然科学版), 45(5):819-824. doi: 10.3321/j.issn:0479-8023.2009.05.014
李金祥, 秦克章, 李光明, 等, 2006.富金斑岩型铜矿床的基本特征、成矿物质来源与成矿高氧化岩浆-流体演化.岩石学报, 22(3):678-688. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200603017
刘斌, 段光贤, 1987.NaCl-H₂O溶液包裹体的密度式和等容式及其应用.矿物学报, 7(4):345-352. doi: 10.3321/j.issn:1000-4734.1987.04.010
刘学龙, 李文昌, 尹光侯, 等, 2013.云南格咱岛弧普朗斑岩型铜矿年代学、岩石矿物学及地球化学研究.岩石学报, 29(9):3049-3064. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201309008
卢焕章, 范宏瑞, 倪培, 等, 2004.流体包裹体.北京:科学出版社, 11-274.
屈迅, 2011.新疆东准噶尔斑岩成矿规律及靶区预测(博士学位论文).北京:中国地质大学.
屈迅, 徐兴旺, 梁广林, 等, 2009.蒙西斑岩型铜钼矿地质地球化学特征及其对东准噶尔琼河坝岩浆岛弧构造属性的制约.岩石学报, 25(4):765-776. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200904004
邵洁涟, 1988.金矿找矿矿物学.武汉:中国地质大学出版社, 38-45.
申萍, 董连慧, 冯京, 等, 2010.新疆斑岩型铜矿床分布、时代及成矿特点.新疆地质, 28(4):358-364. doi: 10.3969/j.issn.1000-8845.2010.04.003
孙石达, 陈超, 杜劲松, 等, 2016.准噶尔盆地及邻区地壳磁性特征及其构造意义.地球科学, 41(7):1216-1224. http://earth-science.net/WebPage/Article.aspx?id=3330
唐功建, 王强, 赵振华, 等, 2009.西准噶尔包古图成矿斑岩年代学与地球化学:岩石成因与构造、铜金成矿意义.地球科学, 34(1):56-74. doi: 10.3321/j.issn:1000-2383.2009.01.007
王军, 李廷栋, 耿树方, 等, 2010.新疆东准噶尔地区斑岩铜矿地质特征与成因.地球学报, 31(3):423-433. http://d.old.wanfangdata.com.cn/Periodical/dqxb201003015
夏佐铎, 2000.新疆乌伦布拉克矿区成矿岩浆岩特征及其铜、钼成矿作用(硕士学位论文).桂林:桂林工学院.
肖文交, 韩春明, 袁超, 等, 2006.新疆北部石炭纪-二叠纪独特的构造-成矿作用:对古亚洲洋构造域南部大地构造演化的制约.岩石学报, 22(5):1062-1076. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200605002
徐芹芹, 赵磊, 牛宝贵, 等, 2015.新疆东准噶尔纸房地区早古生代花岗岩的确定及其地质意义.地质力学学报, 21(4):502-516. doi: 10.3969/j.issn.1006-6616.2015.04.006
徐兴旺, 董连慧, 屈迅, 等, 2013.东准噶尔斑岩型铜矿成矿规律与成矿预测.北京:地质出版社, 21-56.
徐兴旺, 吴琪, 黄雪飞, 等, 2012.富铜斑岩岩浆形成机制与演化过程.岩石学报, 28(2):421-432. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201202007
喻亨祥, 林锦富, 刘家远, 等, 1998.新疆乌伦布拉克隐爆角烁岩筒型斑岩铜矿成矿地质特征.地质与勘探, 34(5):8-13. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=QK199800069833
喻亨祥, 夏斌, 刘家远, 等, 2002.新疆乌伦布拉克铜矿床成矿地质地球化学及矿床成因.大地构造与成矿学, 26(2):172-178. doi: 10.3969/j.issn.1001-1552.2002.02.011
翟裕生, 1999.论成矿系统.地学前缘, 6(1):13-27. doi: 10.3321/j.issn:1005-2321.1999.01.002
张若飞, 袁峰, 周涛发, 等, 2015.西准噶尔塔尔巴哈台-谢米斯台地区火山热液型铜矿床(点)地质及含矿火山岩年代学、地球化学特征.岩石学报, 31(8):2259-2276. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201508010
张永, 梁广林, 屈迅, 等, 2010.东准噶尔琼河坝岛弧早古生代岩浆活动的锆石U-Pb年龄和Hf同位素证据.岩石学报, 26(8):2389-2398. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201008013