西藏达布矿区含矿岩体的时代、岩石地球化学特征及岩石成因

李世杰; 魏启荣; 次琼; 邓小俊; 郑秋平; 卢浩东; 吉雪峰; 王健; 许欢; 杨长青

doi:10.3799/dqkx.2018.231

西藏达布矿区含矿岩体的时代、岩石地球化学特征及岩石成因

doi: 10.3799/dqkx.2018.231

1.
中国地质大学资源学院, 湖北武汉 430074
2.
西藏自治区地质矿产勘查开发局第二地质大队, 西藏拉萨 850000
3.
四川省地质矿产勘查开发局404地质队, 四川西昌 615000
4.
河南省地质调查院, 河南郑州 450001

基金项目:

中国地质调查局项目 DD20160015

详细信息

作者简介:
李世杰(1991-), 男, 硕士研究生, 主要从事岩浆岩与成矿研究

通讯作者:
魏启荣

中图分类号: P581
计量
- 文章访问数: 4740
- HTML全文浏览量: 1401
- PDF下载量: 24
- 被引次数: 0
出版历程
- 收稿日期: 2018-04-09
- 刊出日期: 2018-09-15

Geochronology, Petrogeochemistry and Petrogenesis of Ore-Bearing Rock Massif in Dabu Mining Area, Tibet

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
No.2 Geological Party, Tibet Autonomous Region Geological and Mineral Exploration and Development Bureau, Lhasa 850000, China
3.
No. 404 Geological Team, Sichuan Bureau of Geology and Mineral Resources, Xichang 615000, China
4.
Henan Institute of Geological Survey, Zhengzhou 450001, China

摘要

摘要: 达布矿区位于冈底斯成矿带中段南侧，具较大的铜（钼）成矿潜力.通过对达布矿区含矿花岗闪长岩体开展岩石学、LA-ICP-MS锆石U-Pb定年和岩石地球化学等方面的分析研究，结果显示达布矿区花岗闪长岩体是主要的含矿岩体之一，其LA-ICP-MS锆石U-Pb年龄为16.5±0.3 Ma~16.0±0.4 Ma，属中新世（N₁）.岩体具高Al（Al₂O₃=15.6%~16.5%）、高Na（Na₂O=4.51%~4.82%）、钙碱性系列、弱过铝质；稀土元素具弱正铕异常（Eu/Eu^*=1.02~1.27）和正铈异常（Ce/Ce^*=0.99~1.53）；富集Rb、Ba、Sr和亏损Nb、Ta、Ti、Y.达布矿区花岗闪长岩体属Ⅰ型花岗岩，类似于典型的C型埃达克岩，明显有别于冈底斯带中新世高K埃达克岩；为印度-亚洲大陆碰撞后局部伸展背景下，由加厚下地壳物质（石榴石角闪岩）较高程度部分熔融的岩浆产物.
- 花岗闪长岩体 /
- 锆石U-Pb年龄 /
- 岩石学 /
- 地球化学 /
- 岩石成因 /
- 达布矿区 /
- 西藏
Abstract: Dabu mining area is located in the southern part of the middle Gangdese metallogenic belt, which has great metallogenic potential of Cu (Mo) deposit. In this paper, petrology, LA-ICP-MS zircon U-Pb dating, rock geochemistry of the Dabu ore-bearing granodiorite body are systematically studied. The results suggest that the Dabu granodiorite pluton is one of the major ore-bearing rock body, and its LA-ICP-MS zircon U-Pb age is 16.5±0.3 Ma-16.0±0.4 Ma, with the corresponding age of Miocene (N₁). The rock mass has high Al (Al₂O₃=15.6%-16.5%), high Na (Na₂O=4.51%-4.82%), and it is calc-alkaline and weakly peraluminous. REE elements have weak positive Eu anomalies (Eu/Eu^*=1.02-1.27) and positive Ce anomalies (Ce/Ce^*=0.99-1.53). Trace elements ratio spider diagram displays apparent enrichments of Rb, Ba, Sr and marked depletions of Nb, Ta, Ti, Y. The Dabu granodiorite pluton belongs to Ⅰ-type granite, which is similar to the typical C-type adakite, but is obviously different from the Miocene high-K adakite in the Gangdese belt. It is concluded that Dabu granodiorite pluton is a relatively high degree of partial melting of the thickened lower crust material (garnet amphibolite) formed in the background of partial extension of the India Asian continent post-collision.
- granodiorite /
- zircon U-Pb dating /
- petrology /
- geochemistry /
- petrogenesis /
- mining area of Dabu /
- Tibet

HTML全文

图 1 西藏达布铜(钼)矿区地质简图

Ⅰ.喜马拉雅板块；Ⅰ-1.高喜马拉雅带；Ⅰ-2.特提斯喜马拉雅带；Ⅱ.冈底斯-念青唐古拉板块；Ⅱ-1.冈底斯-下察隅晚燕山-喜山期岩浆弧带；Ⅱ-2.隆格尔-念青唐古拉复合古岛弧带；Ⅱ-3.革吉-申扎弧后盆地带；Ⅱ-4.它日错-班戈-那曲前陆盆地；Ⅲ.羌南-保山板块；①STDS-藏南拆离系；②印度河-雅鲁藏布江板块缝合带；③狮泉河-永珠-嘉黎弧后蛇绿岩带；④班公湖-怒江板块缝合带；1.第四系全新统洪冲积；2.中新世花岗闪长岩；3.中新世二长花岗斑岩；4.始新世石英闪长岩；5.石英脉；6.花岗斑岩脉；7.花岗细晶岩脉；8.地质界线；9.走滑断层；10.逆断层；11.大断裂带；12.拆离断裂带；13.板块缝合带；14.铜(钼)矿体；15.研究区范围；16.硅酸盐样；17.同位素年龄样；18.平硐及其编号；图a据潘桂棠(2013)；图b据郑高峰等(2011)、高一鸣等(2012)修编

Fig. 1. Geological sketch of the Dabu Cu (Mo) mining area in Tibet

下载: 全尺寸图片幻灯片

图 2 达布矿区花岗闪长岩体野外特征和显微结构特征

Qtz.石英；Pl.斜长石；Or.正长石；Kfs.钾长石；Amp.角闪石；Bi.黑云母；a.含浸染状黄铁矿、黄铜矿的花岗闪长岩；b.含石英-黄铁矿、辉钼矿脉的花岗闪长岩；c, d.花岗闪长岩体显微结构特征，正交偏光

Fig. 2. Field characteristics and microstructure characteristics of the granodiorite in Dabu mining area

下载: 全尺寸图片幻灯片

图 3 达布矿区花岗闪长岩体锆石阴极发光电子(CL)图像

Fig. 3. Cathodoluminescence (CL) images of zircons of the granodiorite in Dabu mining area

下载: 全尺寸图片幻灯片

图 4 达布矿区花岗闪长岩体LA-ICP-MS锆石U-Pb年龄谐和图

Fig. 4. LA-ICP-MS U-Pb concordia diagrams of zircons of the granodiorite in Dabu mining area

下载: 全尺寸图片幻灯片

图 5 达布矿区花岗闪长岩体TAS分类图解

1.橄榄辉长岩；2.辉长岩；3.辉长闪长岩；4.闪长岩；5.花岗闪长岩；6.花岗岩；7.硅英岩；8.二长辉长岩；9.二长闪长岩；10.二长岩；11.石英二长岩；12.正长岩；13.似长辉长岩；14.似长二长闪长岩；15.似长正长闪长岩；16.似长正长岩；17.似长岩；18.霓方钠岩/磷霞岩/粗白榴岩；Ir为Irvine分界线(Irvine and Baragar, 1971)；A.碱性系列；S.亚碱性系列；底图据Cox et al.(1979)

Fig. 5. The TAS classification diagram of the granodiorite in Dabu mining area

下载: 全尺寸图片幻灯片

图 6 达布矿区花岗闪长岩体AFM(a)、K₂O-SiO₂(b)、K₂O-Na₂O(c)和A/NK-A/CNK(d)图解

TH.拉斑玄武岩系列；CA.钙碱性系列；图b, c中达布(1)据夏抱本等(2007)，驱龙据郑有业等(2004)，拉抗俄、南木、厅宫据侯增谦等(2003a)，达布(2)本文；图a底图据Irvine and Baragar(1971)；图b底图据Peccerillo and Taylor(1976)、Middlemost(1985)；图c底图据Middlemost(1975)；图d底图据Maniar and Piccoli(1989)

Fig. 6. AFM (a), K₂O-SiO₂ (b), K₂O-Na₂O (c) and A/NK-A/CNK (d) diagrams of the granodiorite in Dabu mining area

下载: 全尺寸图片幻灯片

图 7 达布矿区花岗闪长岩稀土元素配分模式(a)和微量元素比值蛛网图(b)

图a球粒陨石标准化值和图b原始地幔标准化值据Sun and McDonough(1989)

Fig. 7. REE pattern (a) and trace elements spider diagram (b) of the granodiorite in Dabu mining area

下载: 全尺寸图片幻灯片

图 8 达布矿区花岗闪长岩体Na₂O-K₂O图(a)和Sr/Y-Y图(b)

Ⅰ型.Ⅰ型花岗岩；S型.S型花岗岩；A型.A型花岗岩；图a, b中达布(1)据夏抱本等(2007)，驱龙据郑有业等(2004)，拉抗俄、南木、厅宫据侯增谦等(2003a)，达布(2)本文；图a底图据Collins et al.(1982)；图b底图据Defant and Drummond(1990)

Fig. 8. Na₂O-K₂O (a) and Sr/Y-Y (b) diagram of the granodiorite type in Dabu mining area

下载: 全尺寸图片幻灯片

图 9 达布矿区花岗闪长岩体Zr/Sm-Y(a)和Sm/Yb-Y(b)图解

底图据侯增谦等(2005)

Fig. 9. Zr/Sm-Y (a) and Sm/Yb-Y (b) diagrams of the granodiorite in Dabu mining area

下载: 全尺寸图片幻灯片

图 10 达布矿区花岗闪长岩体A/MF-C/MF图(a)和La_N/Yb_N-Yb_N图(b)

图b中达布(1)据夏抱本等(2007)，拉抗俄、南木、厅宫据侯增谦等(2003a)，达布(2)本文；图a底图据Altherr et al.(2000)；图b底图据Drummond and Defant(1990)；图b中曲线刻度为源区部分熔融程度

Fig. 10. A/MF-C/MF (a) and La_N/Yb_N-Yb_N (b) diagram of the granodiorite in Dabu mining area

下载: 全尺寸图片幻灯片

图 11 达布矿区花岗闪长岩R1-R2构造环境判别图

①地幔分异产物；②板块碰撞前；③碰撞后；④造山晚期；⑤非造山；⑥同碰撞；⑦造山后；底图据Batchelor and Bowden(1985)

Fig. 11. R1-R2 tectonic setting discrimination diagram of the granodiorite in the Dabu mining area

下载: 全尺寸图片幻灯片

表 1 达布矿区花岗闪长岩体LA-ICP-MS锆石U-Pb同位素分析结果

Table 1. LA-ICP-MS U-Pb data for zircons from the granodiorite in Dabu mining area

测点序号	Pb(10^-6)	Th(10^-6)	U(10^-6)	²³²Th/²³⁸U	同位素比值						年龄(Ma)
测点序号	Pb(10^-6)	Th(10^-6)	U(10^-6)	²³²Th/²³⁸U	²⁰⁷Pb^/²⁰⁶Pb^	±1σ	²⁰⁷Pb^*/²³⁵U	±1σ	²⁰⁶Pb^*/²³⁸U	±1σ	²⁰⁷Pb/²³⁵U	±1σ	²⁰⁶Pb/²³⁸U	±1σ
样品BD205-1(中细粒花岗闪长岩)
BD205-1_01	11.0	399	485	0.82	0.078 84	0.013 68	0.021 93	0.003 11	0.002 57	0.000 10	22.0	3.1	16.6	0.7
BD205-1_02	12.7	785	897	0.88	0.047 82	0.006 30	0.015 45	0.001 33	0.002 62	0.000 09	15.6	1.3	16.9	0.6
BD205-1_03	9.9	688	818	0.84	0.088 80	0.010 28	0.026 69	0.001 85	0.002 51	0.000 08	26.7	1.8	16.2	0.5
BD205-1_04	9.2	761	767	0.99	0.055 73	0.011 36	0.014 26	0.001 76	0.002 54	0.000 09	14.4	1.8	16.4	0.6
BD205-1_05	16.1	1 187	1 038	1.14	0.073 86	0.007 57	0.024 23	0.002 33	0.002 59	0.000 09	24.3	2.3	16.7	0.6
BD205-1_06	69.5	6 252	2 246	2.78	0.066 43	0.007 56	0.023 61	0.002 62	0.002 55	0.000 06	23.7	2.6	16.4	0.4
BD205-1_07	7.1	461	580	0.80	0.074 10	0.014 24	0.021 09	0.004 09	0.002 49	0.000 11	21.2	4.1	16.0	0.7
BD205-1_08	18.5	1 476	961	1.54	0.066 94	0.007 68	0.021 61	0.001 83	0.002 58	0.000 07	21.7	1.8	16.6	0.5
BD205-1_09	16.5	848	825	1.03	0.071 20	0.008 67	0.021 53	0.001 99	0.002 54	0.000 08	21.6	2.0	16.4	0.5
BD205-1_10	8.8	641	680	0.94	0.068 02	0.016 81	0.016 37	0.002 39	0.002 55	0.000 09	16.5	2.4	16.4	0.6
BD205-1_11	6.0	499	483	1.03	0.088 32	0.015 77	0.023 29	0.003 22	0.002 54	0.000 10	23.4	3.2	16.3	0.7
样品BD206-1(中细粒花岗闪长岩)
BD206-1_01	14.3	942	794	1.19	0.051 69	0.009 80	0.016 86	0.002 62	0.002 53	0.000 10	17.0	2.6	16.3	0.6
BD206-1_02	5.6	406	512	0.79	0.092 10	0.021 28	0.023 32	0.004 22	0.002 42	0.000 19	23.4	4.2	15.6	1.2
BD206-1_03	21.7	1 856	1 275	1.46	0.057 06	0.005 33	0.018 62	0.001 44	0.002 43	0.000 06	18.7	1.4	15.7	0.4
BD206-1_04	5.8	427	419	1.02	0.059 58	0.014 69	0.015 63	0.003 01	0.002 56	0.000 11	15.8	3.0	16.5	0.7
BD206-1_05	12.4	985	893	1.10	0.065 29	0.008 14	0.021 61	0.002 05	0.002 54	0.000 08	21.7	2.0	16.4	0.5
BD206-1_06	21.7	1 822	1 253	1.45	0.061 79	0.006 51	0.019 02	0.001 61	0.002 46	0.000 06	19.1	1.6	15.8	0.4
BD206-1_07	11.3	922	816	1.13	0.065 61	0.013 27	0.020 02	0.002 72	0.002 47	0.000 11	20.1	2.7	15.9	0.7
BD206-1_08	10.6	615	693	0.89	0.110 92	0.023 29	0.030 94	0.004 05	0.002 47	0.000 11	30.9	4.0	15.9	0.7
BD206-1_09	72.6	6 508	2 497	2.61	0.044 65	0.007 99	0.014 61	0.002 22	0.002 48	0.000 09	14.7	2.2	16.0	0.6
注：Pb^*代表放射性成因铅；分析测试在中国地质大学(武汉)地质过程与矿产资源国家重点实验室完成.

下载: 导出CSV

表 2 达布矿区花岗闪长岩体主量元素分析结果(%)

Table 2. Major elements (%) of the granodiorite in Dabu mining area

样号	BD203-1	BD205-1	BD205-2	BD205-3	BD205-4	BD205-5	BD206-1	BD206-2
SiO₂	65.3	65.8	66.1	65.8	67.8	66.1	65.0	65.5
TiO₂	0.46	0.42	0.44	0.44	0.40	0.42	0.45	0.43
Al₂O₃	16.5	16.2	16.1	16.1	15.6	15.7	16.0	15.9
Fe₂O₃	0.37	0.33	1.42	0.31	0.55	0.22	0.67	0.83
FeO	3.94	2.99	2.40	2.99	2.36	2.80	2.80	2.59
MnO	0.04	0.04	0.04	0.04	0.03	0.03	0.05	0.05
MgO	1.57	1.37	1.48	1.48	1.43	1.38	1.44	1.43
CaO	2.85	2.88	2.63	2.82	1.77	2.62	3.13	3.03
Na₂O	4.79	4.68	4.71	4.82	4.81	4.53	4.51	4.71
K₂O	2.66	2.52	2.77	2.41	2.56	2.94	2.59	2.78
P₂O₅	0.20	0.18	0.18	0.20	0.18	0.18	0.18	0.19
H₂O⁺	0.61	1.08	0.93	0.95	1.20	0.90	1.13	0.95
CO₂	0.33	0.54	0.27	0.65	0.33	0.54	0.71	0.71
Total	99.6	99.1	99.5	99.0	99.0	98.4	98.7	99.1
σ	2.48	2.27	2.42	2.29	2.19	2.42	2.28	2.50
A/CNK	1.03	1.03	1.04	1.03	1.12	1.02	1.01	0.97
c	1.80	2.28	1.71	2.45	2.92	2.03	2.23	1.73
注：分析测试单位为西南冶金地质测试所，下同.

下载: 导出CSV

表 3 达布矿区花岗闪长岩体稀土元素分析结果(10^-6)

Table 3. Rare earth elements (10^-6) of the granodiorite in Dabu mining area

样号	BD203-1	BD205-1	BD205-2	BD205-3	BD205-4	BD205-5	BD206-1	BD206-2
La	18.5	16.3	17.1	19.1	13.9	15.7	17.4	16.2
Ce	49.1	47.3	43.9	44.7	33.5	41.3	49.4	30.6
Pr	4.01	3.54	3.46	4.04	2.86	3.36	3.70	3.53
Nd	16.8	14.6	14.4	17.4	12.0	13.8	17.6	14.9
Sm	2.82	2.49	2.44	3.01	1.98	2.31	2.60	2.49
Eu	0.85	0.74	0.75	1.14	0.59	0.76	0.77	0.74
Gd	2.21	1.91	1.88	2.50	1.55	1.71	1.94	1.77
Tb	0.26	0.23	0.23	0.33	0.18	0.21	0.22	0.21
Dy	1.20	1.09	1.10	1.68	0.75	1.05	1.06	0.93
Ho	0.25	0.23	0.24	0.30	0.15	0.22	0.21	0.18
Er	0.96	0.83	0.85	0.92	0.54	0.70	0.76	0.49
Tm	0.12	0.11	0.11	0.10	0.05	0.11	0.09	0.06
Yb	0.89	0.83	0.86	0.67	0.64	0.82	0.72	0.80
Lu	0.16	0.15	0.16	0.10	0.06	0.15	0.12	0.07
Y	6.59	6.14	6.84	6.82	5.58	6.74	6.88	6.71
∑REE	98.1	90.4	87.5	95.9	68.7	82.3	96.6	73.0
(La/Yb)_N	15.0	14.1	14.3	20.5	15.6	13.8	17.2	14.6
Eu/Eu^*	1.04	1.04	1.08	1.27	1.02	1.16	1.04	1.08
Ce/Ce^*	1.40	1.53	1.40	1.25	1.30	1.39	1.51	0.99

下载: 导出CSV

表 4 达布矿区花岗闪长岩体微量元素分析结果(10^-6)

Table 4. Trace elements (10^-6) of the granodiorite in Dabu mining area

样号	BD203-1	BD205-1	BD205-2	BD205-3	BD205-4	BD205-5	BD206-1	BD206-2
Rb	98.7	87.8	106	98.0	94.7	107	89.5	92.4
Sr	915	884	852	885	751	836	866	856
Ba	763	700	735	674	694	717	736	764
Th	8.23	10.9	10.6	9.73	8.93	8.96	9.05	9.23
U	1.34	2.39	1.15	2.32	1.18	2.03	1.96	2.23
Ta	0.20	0.20	0.16	0.17	0.13	0.14	0.23	0.25
Nb	3.54	3.32	2.61	2.70	2.00	2.30	3.40	3.95
Zr	130	118	121	132	118	111	115	118
Hf	3.85	3.45	3.67	4.33	4.45	5.14	3.41	3.35
Sc	8.44	3.09	5.84	5.89	6.62	8.73	4.76	6.75
V	75.7	66.0	66.2	70.9	62.8	67.6	68.5	75.1
Cr	35.8	27.4	32.5	23.7	18.9	21.4	24.8	21.1
Co	9.30	7.93	7.90	7.44	6.83	8.70	8.70	8.41
Ni	12.1	10.5	12.3	13.2	12.0	11.8	11.9	12.7
Cu	917	764	864	1536	1819	2877	872	678
Pb	23.0	21.2	20.5	18.7	19.4	20.2	18.8	17.6
Zn	35.0	30.4	30.4	31.5	33.1	35.1	32.0	35.3

下载: 导出CSV

表 5 达布花岗闪长岩体与Ⅰ型花岗岩的矿物及化学成分特征对比

Table 5. Comparison of mineral and chemical composition characteristics between Dabu granodiorite and Ⅰ-type granite

矿物	Ⅰ型	达布矿区花岗闪长岩体
长英质矿物的差异	石英不太多，长石可呈粉红色	石英20%~25%，可见肉红色钾长石
常见铁镁矿物	黑云母Mg/Fe高，白云母较罕见	黑云母、角闪石(少)
不透明矿物	磁铁矿物±钛铁矿±黄铁矿物	黄铜矿±黄铁矿±磁铁矿±辉钼矿(多)，钛铁矿±赤铁矿(少)
SiO₂含量	53%~76%	65.0%~67.8%
Na₂O含量	＞3.2%	4.51%~4.82%
K₂O/ Na₂O	低(＜1)	0.50~0.65
A/CNK	低(＜1.0)，准铝质-过铝质	0.97~1.12，准铝质-弱过铝质
SiO₂含量为66%时的CaO含量	＞3.7%	1.72%~3.18%
CIPW刚玉分子	＜1%	1.71%~2.92%
包含岩类	花岗闪长岩-闪长岩	花岗闪长岩-石英二长岩
矿床	Cu-Mo-W	Cu-Mo
注：Ⅰ型花岗岩据路凤香和桑隆康(2002)、桑隆康和马昌前(2012).

下载: 导出CSV

表 6 达布花岗闪长岩体与埃达克岩的地球化学特征对比

Table 6. Comparison of geochemical characteristics of the Dabu granodiorite and adakitic rocks

	埃达克岩	达布矿区花岗闪长岩体
岩石组合	石英闪长岩、花岗闪长岩、英云闪长岩等	花岗闪长岩、石英二长岩
岩石系列	钙碱性	钙碱性
SiO₂	≥56	65.0~67.8
Al₂O₃	≥15	15.6~16.5
MgO	≤3	1.37~1.57
Na₂O	4±	4.51~4.82
K₂O	1~2	2.41~2.94
K₂O/Na₂O	＜0.5	0.50~0.65
Mg^#	＞47	39.6~47.2
Sr	＞400	751~915
Yb	≤1.9	0.64~0.89
Y	≤18	5.58~6.88
Sr/Y	＞20~40	124~144
(La/Yb)_N	＞20	13.8~20.5
Eu/Eu^*	＞1	1.02~1.27
注：主量元素单位为%；微量元素单位为10^-6；埃达克岩数据据Defant and Drummond(1990).

下载: 导出CSV

参考文献(100)

[1]	Altherr, R., Holl, A., Hegner, E., et al., 2000.High-Potassium, Calc-Alkaline Ⅰ-Type Plutonism in the European Variscides:Northern Vosges (France) and Northern Schwarzwald (Germany).Lithos, 50(1-3):51-73. https://doi.org/10.1016/s0024-4937(99)00052-3
[2]	Batchelor, R.A., Bowden, P., 1985.Petrogenetic Interpretation of Granitoid Rock Series Using Multicationic Parameters.Chemical Geology, 48(1-4):43-55. https://doi.org/10.1016/0009-2541(85)90034-8
[3]	Chappell, B.W., White, A.J.R, 1974.Two Contrasting Granite Type.Pacific Geology, 8:173-174. http://d.old.wanfangdata.com.cn/NSTLQK/NSTL_QKJJ027419645/
[4]	Collins, W.J., Beams, S.D., White, A.J.R., et al., 1982.Nature and Origin of A-Type Granites with Particular Reference to Southeastern Australia.Contributions to Mineralogy and Petrology, 80(2):189-200. https://doi.org/10.1007/bf00374895
[5]	Cox, K.G., Bell, J.D., Pankhurst, R.J., 1979.The Interpretation of Igneous Rocks.Allen and Unwin, London.
[6]	Defant, M.J., Drummond, M.S., 1990.Derivation of Some Modern Arc Magmas by Melting of Young Subducted Lithosphere.Nature, 347(6294):662-665. https://doi.org/10.1038/347662a0
[7]	DePaolo, D.J., Daley, E.E., 2000.Neodymium Isotopes in Basalts of the Southwest Basin and Range and Lithospheric Thinning during Continental Extension.Chemical Geology, 169(1-2):157-185. https://doi.org/10.1016/s0009-2541(00)00261-8
[8]	Drummond, M.S., Defant, M.J., 1990.A Model for Trondhjemite-Tonalite-Dacite Genesis and Crustal Growth via Slab Melting:Archean to Modern Comparisons.Journal of Geophysical Research Solid Earth, 95(B13):21503-21521. https://doi.org/10.1029/JB095iB13p21503
[9]	Gao, Y.M., Chen, Y.C., Tang, J.X., et al., 2012.A Study of Diagenetic and Metallogenic Geochronology of the Dagbo Cu (Mo) Deposit in Quxur County of Tibet and Its Geological Implications.Acta Geoscientica Sinica, 33(4):613-623 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqxb201204021
[10]	Geng, R.R., 2014.Characteristics of Ore-Forming Fluid of Dabu Porphyry Cu-Mo Deposit in Tibet (Dissertation).China University of Geosciences, Beijing (in Chinese with English abstract).
[11]	Hoskin, P.W.O., 2003.The Composition of Zircon and Igneous and Metamorphic Petrogenesis.Reviews in Mineralogy and Geochemistry, 53(1):27-62. https://doi.org/10.2113/0530027
[12]	Hou, Z.Q., Gao, Y.F., Meng, X.J., et al., 2004.Genesis of Adaltitic Porphyry and Tectonic Controls on the Gangdese Miocene Porphyry Copper Belt in the Tibetan Orogen.Acta Petrologica Sinica, 20(2):239-248 (in Chinese with English abstract).
[13]	Hou, Z.Q., Meng, X.J., Qu, X.M., et al., 2005.Copper Ore Potential of Adakitic Intrusives in Gangdese Porphyry Copper Belt:Constrains from Rock Phase and Deep Melting Process.Mineral Deposits, 24(2):108-121 (in Chinese with English abstract).
[14]	Hou, Z.Q., Mo, X.X., Gao, Y.F., et al., 2003a.Adakite, A Possible Host Rock for Porphyry Copper Deposits:Case Studies of Porphyry Copper Belts in Tibetan Plateau and in Northern Chile.Mineral Deposits, 22(1):1-12 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-KCDZ200301000.htm
[15]	Hou, Z.Q., Mo, X.X., Gao, Y.F., et al., 2006.Early Processes and Tectonic Model for the Indian-Asian Contiental Collision Evidence from the Cenozoic Gangdese Igneous Rocks in Tibet.Acta Geologica Sinica, 80(9):1233-1248 (in Chinese with English abstract).
[16]	Hou, Z.Q., Qu, X.M., Wang, S.X., et al., 2003b.Re-Os Ages of Molybdenite in the Gangdese Porphyry Copper Belt in South Tibet:Duration of Mineralization and Application of the Dynamic Setting.Science in China (Series D), 33(7):609-618 (in Chinese).
[17]	Irvine, T.N., Baragar, W.R.A., 1971.A Guide to the Chemical Classification of the Common Volcanic Rocks.Canadian Journal of Earth Sciences, 8(5):523-548. https://doi.org/10.1139/e71-055
[18]	Ji, W.Q., Wu, F.Y., Zhong, S.L, et al., 2009.Geochronology and Petrogenesis of Granitic Rocks in Gangdese Batholiths, Southern Tibet.Science in China (Series D), 39(7):849-871 (in Chinese).
[19]	Kay, S.M., Mpodozis, C., 2001.Central Andean Ore Deposits Linked to Evolving Shallow Subduction Systems and Thickening Crust.GSA Today, 11(3):4.https://doi.org/10.1130/1052-5173(2001)011<0004:caodlt>2.0.co;2 doi: 10.1130/1052-5173(2001)011<0004:caodlt>2.0.co;2
[20]	Lai, S.C., Qin, J.F., Zhu, R.Z., et al., 2015.Petrogenesis and Tectonic Implication of the Neoproterozoic Peraluminous Granitoids from the Tianquan Area, Western Yangtze Block, South China.Acta Petrologica Sinica, 31(8):2245-2258 (in Chinese with English abstract). http://d.old.wanfangdata.com.cn/Periodical/ysxb98201508009
[21]	Leng, Q.F., Tang, J.X., Zheng, W.B., et al., 2016.Geochronology, Geochemistry and Zircon Hf Isotopic Compositions of the Ore-Bearing Porphyry in the Lakang'e Porphyry Cu-Mo Deposit, Tibet.Earth Science, 41(6):999-1015 (in Chinese with English abstract). https://doi.org/ 10.3799/dqkx.2016.083
[22]	Li, G.M., Duan, Z.M., Huang, Y., et al., 2017.Gangdese-Himalayan Geology and Mineralization in Tibet.China University of Geosciences Press, Wuhan (in Chinese).
[23]	Li, G.M., Rui, Z.Y., 2004.Diagenetic and Mineralization Ages for the Porphyry Copper Deposits in the Gangdise Metallogenic Belt, Southern Xizang.Geotectonica et Metallogenia, 28(2):165-170 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DGYK200402007.htm
[24]	Li, Y.W., Wei, Q.R., Wang, C., et al., 2017.Zircon U-Pb Dating and Geochemistry of Late Triassic Intermediate Dykes in Suyingdi, Eastern Section of West Kunlun and Their Geological Significance.Earth Science, 42(6):909-926 (in Chinese with English abstract). https://doi.org/ 10.3799/dqkx.2017.083
[25]	Liu, Y.S., Hu, Z.C., Gao, S., et al., 2008.In Situ Analysis of Major and Trace Elements of Anhydrous Minerals by LA-ICP-MS without Applying an Internal Standard.Chemical Geology, 257(1-2):34-43. https://doi.org/10.1016/j.chemgeo.2008.08.004
[26]	Lu, F.X., Sang, L.K., 2002.Petrology.Geological Publishing House, Beijing, 93-94 (in Chinese).
[27]	Ludwig, K.R., 2003.User's Manual for Isoplot 3.6: A Geochronological Toolkit for Microsoft Excel.Berkeley Geochronology Center, Berkeley.
[28]	Maniar, P.D., Piccoli, P.M., 1989.Tectonic Discrimination of Granitoids.Geological Society of America Bulletin, 101(5):635-643.https://doi.org/10.1130/0016-7606(1989)101<0635:tdog>2.3.co;2 doi: 10.1130/0016-7606(1989)101<0635:tdog>2.3.co;2
[29]	Mao, X.L., Wang, G.Z., Chen, J.J., et al., 2013.Comparison of Geochemical Characteristics of Granite Porphyry and Typical Adakitic Rocks in the Dabu Area, Tibet, China.Acta Mineralogica Sinica, (S2):341-342 (in Chinese).
[30]	Meng, X.J., 2004.The Metallogeny of the Miocene Gangdese Porphyry Copper Belt in Tibetan Collisional Orogen (Dissertation).Chinese Academy of Geological Sciences, Beijing (in Chinese with English abstract).
[31]	Meng, Y.K., 2016.Tectonic Evolution of the Southern Region in the Middle Gangdese Batholith, Southern Tibet (Dissertation).Chinese Academy of Geological Sciences, Beijing (in Chinese with English abstract).
[32]	Middlemost, E.A.K., 1975.The Basalt Clan.Earth-Science Reviews, 11(4):337-364. https://doi.org/10.1016/0012-8252(75)90039-2
[33]	Middlemost, E.A.K., 1985.Magmas and Magmatic Rocks: An Introduction to Igneous Petrology.Longman, New York. http://adsabs.harvard.edu/abs/1986MinM...50..185M
[34]	Misra, K.C., 1999.Understanding Mineral Deposits.Kluwer Academic Publishers, New York, 353-413.
[35]	Mo, X.X., Pan, G.T., 2006.From the Tethys to the Formation of the Qinghai Tibet Plateau:Constrained by Tectone Magmatic Events.Earth Science Frontiers, 13(6):43-51 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-DXQY200606007.htm
[36]	Mo, X.X., Zhao, Z.D., Deng, J.F., et al., 2003.Response of Volcanism to the India Asia Conllision.Earth Science Frontiers, 10(3):135-148 (in Chinese with English abstract).
[37]	Moyen, J.F., 2009.High Sr/Y and La/Yb Ratios:The Meaning of the"Adakitic Signature".Lithos, 112(3-4):556-574. https://doi.org/10.1016/j.lithos.2009.04.001
[38]	Mungall, J.E., 2002.Roasting the Mantle:Slab Melting and the Genesis of Major Au and Au-Rich Cu Deposits.Geology, 30(10):915.https://doi.org/10.1130/0091-7613(2002)030<0915:rtmsma>2.0.co;2 doi: 10.1130/0091-7613(2002)030<0915:rtmsma>2.0.co;2
[39]	Pan, G.T., Mo, X.X., Hou, Z.Q., et al., 2006.Spatial-Temporal Framework of the Gangdese Orogenic Belt and Its Evolution.Acta Petrologica Sinica, 22 (3):521-533 (in Chinese with English abstract). http://www.oalib.com/paper/1472080
[40]	Pan, G.T., 2013.Tectonic Maps and Manuals of the Qinghai-Tibet Plateau and Its Adjacent Areas.Geological Publishing House, Beijing (in Chinese).
[41]	Peccerillo, A., Taylor, S.R., 1976.Geochemistry of Eocene Calc-Alkaline Volcanic Rocks from the Kastamonu Area, Northern Turkey.Contributions to Mineralogy and Petrology, 58(1):63-81. https://doi.org/10.1007/bf00384745
[42]	Qu, X.M., Hou, Z.Q., Huang, W., 2001.Is Gangdese Porphyry Copper Belt the Second "Yulong" Copper Belt?Mineral Deposits, 20(4):355-366 (in Chinese with English abstract).
[43]	Qu, X.M., Hou, Z.Q., Xin, H.B., 2006.Zircon SHRIMP Ages and Geochemical Characteristics of Two Generations of Adakite from Gangdese Collisional Orogenic Belt, Tibet.Mineral Deposits, (S1):419-422 (in Chinese).
[44]	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
[45]	Reich, M., Parada, M.A., Palacios, C., et al., 2003.Adakite-Like Signature of Late Miocene Intrusions at the Los Pelambres Giant Porphyry Copper Deposit in the Andes of Central Chile:Metallogenic Implications.Mineralium Deposita, 38(7):876-885. https://doi.org/10.1007/s00126-003-0369-9
[46]	Rui, Z.Y., Li, G.M., Wang, L.S., 2004.Metallic Mineral Resources on the Qinghai-Tibet Plateau.Geological Bulletin of China, 23(1):20-23 (in Chinese).
[47]	Rui, Z.Y., Zhang, H.T., Chen, R Y., et al., 2006.An Approach to Some Problems of Porphyry Copper Deposits.Mineral Deposits, 25(4):491-500 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kcdz200604014
[48]	Sang, L.K., Ma, C.Q., 2012.Petrology (Second Edition).Geological Publishing House, Beijing, 188 (in Chinese).
[49]	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
[50]	Tang, J.X., Duo, J., Liu, H.F., et al., 2012.Minerogenetic Series of Ore Deposits in the East Part of the Gangdese Metallogenic Belt.Acta Geoscientica Sinica, 33(4):393-410 (in Chinese with English abstract). http://www.oalib.com/paper/1559914
[51]	Wang, Q., Xu, J.F., Zhao, Z.H., 2001.The Summary and Comment on Research on a New Kind of Igneous Rock—Adakite.Advance in Earth Sciences, 16(2):201-208 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dqkxjz200102010
[52]	Wang, Y.Y., Tang, J.X., Zheng, W.B., et al., 2015.Mechanism of Metal Precipitation in Dabu Porphyry Cu-Mo Deposit, Quxu Country, Tibet.Mineral Deposits, 34(1)81-97 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTotal-KCDZ201501006.htm
[53]	Wu, F.Y., Huang, B.C., Ye, K., et al., 2008.Collapsed Himalayan-Tibetan Orogen and the Rising Tibetan Plateau.Acta Petrologica Sinica, 24(1):1-30 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-YSXB200801002.htm
[54]	Wu, Y.B., Zheng, Y.F., 2004.Genesis of Zircon and Its Constraints on Interpretation of U-Pb Age.Chinese Science Bulletin, 49(16):1589-1604 (in Chinese). doi: 10.1007%2FBF03184122
[55]	Xia, B.B., Xia, B., Wang, B.D., et al., 2007.Ore-Bearing Adakitic Porphyry in the Middle of Gangdese:Thickened Lower Crustal Melting and the Genesis of Porphyry Cu-Mo Deposit.Geological Science and Technology Information, 26(4):19-26 (in Chinese with English abstract).
[56]	Xiong, X.L., Adam, J., Green, T.H., 2005.Rutile Stability and Rutile/Melt HFSE Partitioning during Partial Melting of Hydrous Basalt:Implications for TTG Genesis.Chemical Geology, 218(3-4):339-359. https://doi.org/10.1016/j.chemgeo.2005.01.014
[57]	Yang, Z., Jiang, H., Yang, M.G., et al., 2017.Zircon U-Pb and Molybdenite Re-Os Dating of the Gangjiang Porphyry Cu-Mo Deposit in Central Gangdese and Its Geological Significance.Earth Science, 42(03):339-356 (in Chinese with English abstract). https://doi.org/10.3799/dqkx.2017.026
[58]	Zhang, Q., Wang, Y., Qian, Q., et al., 2001.The Characteristics and Tectonic-Metallogenic Significances of the Adakites in Yanshan Period from Eastern China.Acta Petrologica Sinica, 17(2):236-244 (in Chinese with English abstract). https://www.researchgate.net/publication/279686768_The_characteristics_and_tectonic-metallogenic_significances_of_the_adakites_in_Yanshan_period_from_Eastern_China
[59]	Zheng, G.F., Zhong, K.H., Gou, J., et al., 2011.Geology and Prospecting of Dabu Porphyry Cu-Mo Type Deposit of Qushui Country in Tibet.Sichuan Nonferrous Metals, (3):9-13 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-ACJS201103003.htm
[60]	Zheng, Y.Y., Xue, Y.X., Cheng, L.J., et al., 2004.Finding, Characteristics and Significances of Qulong Superlarge Porphyry Copper (Molybdenum) Deposit, Tibet.Earth Science, 29(1):103-108 (in Chinese with English abstract). https://doi.org/10.3321/j.issn:1000-2383.2004.01.018
[61]	Zheng, Y.Y., Zhang, G.Y., Xu, R.K., et al., 2007.Geochronolosic Constraints on Masmatic Intrusions and Mineralization of the Zhunuo Porphyry Copper Deposit in Gangdese, Tibet.Chinese Science Bulletin, 52(21):2542-2548 (in Chinese).
[62]	Zhu, D.C., Duan, L.P., Liao, Z.L., et al., 2002.Discrimination for Two Kinds of Adakites.Journal of Mineralogy and Petrology, 22(3):5-9 (in Chinese with English abstract). http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=kwys200203002
[63]	高一鸣, 陈毓川, 唐菊兴, 等, 2012.西藏曲水县达布斑岩铜(钼)矿床成岩成矿年代学研究.地球学报, 33(4): 613-623. doi: 10.3975/cagsb.2012.04.21
[64]	耿瑞瑞, 2014.西藏达布斑岩铜钼矿床成矿流体特征(硕士学位论文).北京: 中国地质大学. http://cdmd.cnki.com.cn/Article/CDMD-11415-1014238657.htm
[65]	侯增谦, 高永丰, 孟祥金, 等, 2004.西藏冈底斯中新世斑岩铜矿带:埃达克质斑岩成因与构造控制.岩石学报, 20(2): 239-248. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200402006
[66]	侯增谦, 孟祥金, 曲晓明, 等, 2005.西藏冈底斯斑岩铜矿带埃达克质斑岩含矿性:源岩相变及深部过程约束.矿床地质, 24(2): 108-121. doi: 10.3969/j.issn.0258-7106.2005.02.003
[67]	侯增谦, 莫宣学, 高永丰, 等, 2003a.埃达克岩:斑岩铜矿的一种可能的重要含矿母岩——以西藏和智利斑岩铜矿为例.矿床地质, 22(1): 1-12. http://d.old.wanfangdata.com.cn/Periodical/cckjdxxb200901012
[68]	侯增谦, 莫宣学, 高永丰, 等, 2006.印度大陆与亚洲大陆早期碰撞过程与动力学模型——来自西藏冈底斯新生代火成岩证据.地质学报, 80(9): 1233-1248. doi: 10.3321/j.issn:0001-5717.2006.09.001
[69]	侯增谦, 曲晓明, 王淑贤, 等, 2003b.西藏高原冈底斯斑岩铜矿带辉钼矿Re-Os年龄:成矿作用时限与动力学背景应用.中国科学(D辑), 33(7): 609-618. http://d.old.wanfangdata.com.cn/Periodical/zgkx-cd200307001
[70]	纪伟强, 吴福元, 锺孙霖, 等, 2009.西藏南部冈底斯岩基花岗岩时代与岩石成因.中国科学(D辑), 39(7): 849-871. http://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200907002.htm
[71]	赖绍聪, 秦江锋, 朱韧之, 等, 2015.扬子地块西缘天全新元古代过铝质花岗岩类成因机制及其构造动力学背景.岩石学报, 31(8): 2245-2258. http://d.old.wanfangdata.com.cn/Periodical/ysxb98201508009
[72]	冷秋锋, 唐菊兴, 郑文宝, 等, 2016.西藏拉抗俄斑岩Cu-Mo矿床含矿斑岩地球化学、锆石U-Pb年代学及Hf同位素组成.地球科学, 41(6): 999-1015. http://www.earth-science.net/WebPage/Article.aspx?id=3312
[73]	李光明, 段志明, 黄勇, 等, 2017.西藏冈底斯-喜马拉雅地质与成矿.武汉:中国地质大学出版社.
[74]	李光明, 芮宗瑶, 2004.西藏冈底斯成矿带斑岩铜矿的成岩成矿年龄.大地构造与成矿学, 28(2): 165-170. doi: 10.3969/j.issn.1001-1552.2004.02.008
[75]	黎有为, 魏启荣, 王程, 等, 2017.西昆仑东段宿营地晚三叠世中性脉岩的锆石U-Pb定年、岩石地球化学特征及其意义.地球科学, 42(6): 909-926. http://www.earth-science.net/WebPage/Article.aspx?id=3587
[76]	路凤香, 桑隆康, 2002.岩石学.北京:地质出版社, 93-94.
[77]	毛秀丽, 王国芝, 陈俊瑾, 等, 2013.西藏达布地区花岗斑岩与典型埃达克岩地球化学特征对比浅析.矿物学报, (S2): 341-342. http://d.old.wanfangdata.com.cn/Conference/8300988
[78]	孟祥金, 2004.西藏碰撞造山带冈底斯中新世斑岩铜矿成矿作用研究(博士学位论文).北京: 中国地质科学院. http://cdmd.cnki.com.cn/Article/CDMD-82501-2007213424.htm
[79]	孟元库, 2016.藏南冈底斯中段南缘构造演化(博士学位论文).北京: 中国地质科学院. http://cdmd.cnki.com.cn/Article/CDMD-82501-1016056636.htm
[80]	莫宣学, 潘桂棠, 2006.从特提斯到青藏高原形成:构造-岩浆事件的约束.地学前缘, 13(6): 43-51. doi: 10.3321/j.issn:1005-2321.2006.06.007
[81]	莫宣学, 赵志丹, 邓晋福, 等, 2003.印度-亚洲大陆主碰撞过程的火山作用响应.地学前缘, 10(3): 135-148. doi: 10.3321/j.issn:1005-2321.2003.03.013
[82]	潘桂棠, 2013.青藏高原及邻区大地构造图及说明书.北京:地质出版社.
[83]	潘桂棠, 莫宣学, 侯增谦, 等, 2006.冈底斯造山带的时空结构及演化.岩石学报, 22(3): 521-533. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200603001
[84]	曲晓明, 侯增谦, 黄卫, 2001.冈底斯斑岩铜矿(化)带:西藏第二条"玉龙"铜矿带?矿床地质, 20(4): 355-366. doi: 10.3969/j.issn.0258-7106.2001.04.009
[85]	曲晓明, 侯增谦, 辛洪波, 2006.西藏冈底斯碰撞造山带两套埃达克岩的锆石SHRIMPU-Pb年龄及地球化学特征.矿床地质, (S1): 419-422. http://kns.cnki.net/KCMS/detail/detail.aspx?filename=KCDZ2006S1111&dbname=CJFD&dbcode=CJFQ
[86]	芮宗瑶, 李光明, 王龙生, 2004.青藏高原的金属矿产资源.地质通报, 23(1): 20-23. doi: 10.3969/j.issn.1671-2552.2004.01.008
[87]	芮宗瑶, 张洪涛, 陈仁义, 等, 2006.斑岩铜矿研究中若干问题探讨.矿床地质, 25(4): 491-500. doi: 10.3969/j.issn.0258-7106.2006.04.014
[88]	桑隆康, 马昌前, 2012.岩石学(第二版).北京:地质出版社, 188.
[89]	唐菊兴, 多吉, 刘鸿飞, 等, 2012.冈底斯成矿带东段矿床成矿系列及找矿突破的关键问题研究.地球学报, 33(4): 393-410. doi: 10.3975/cagsb.2012.04.02
[90]	王强, 许继锋, 赵振华, 2001.一种新的火成岩——埃达克岩的研究综述.地球科学进展, 16(2): 201-208. doi: 10.3321/j.issn:1001-8166.2001.02.010
[91]	王艺云, 唐菊兴, 郑文宝, 等, 2015.西藏曲水县达布斑岩型铜钼矿床金属沉淀机制探讨.矿床地质, 34(1): 81-97. http://d.old.wanfangdata.com.cn/Periodical/kcdz201501005
[92]	吴福元, 黄宝春, 叶凯, 等, 2008.青藏高原造山带的垮塌与高原隆升.岩石学报, 24(1): 1-30. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200801001
[93]	吴元宝, 郑永飞, 2004.锆石成因矿物学研究及其U-Pb年龄解释的制约.科学通报, 49(16): 1589-1604. doi: 10.3321/j.issn:0023-074X.2004.16.002
[94]	夏抱本, 夏斌, 王保弟, 等, 2007.冈底斯中段达布埃达克质含矿斑岩:增厚下地壳熔融与斑岩铜钼矿成因.地质科技情报, 26(4): 19-26. doi: 10.3969/j.issn.1000-7849.2007.04.005
[95]	杨震, 姜华, 杨明国, 等, 2017.冈底斯中段岗讲斑岩铜钼矿床锆石U-Pb和辉钼矿Re-Os年代学及其地质意义.地球科学, 42(3): 339-356. http://www.earth-science.net/WebPage/Article.aspx?id=3545
[96]	张旗, 王焰, 钱青, 等, 2001.中国东部燕山期埃达克岩的特征及其构造-成矿意义.岩石学报, 17(2): 236-244. http://d.old.wanfangdata.com.cn/Periodical/ysxb98200102008
[97]	郑高峰, 钟康惠, 苟金, 等, 2011.西藏曲水县达布斑岩型铜钼矿床地质特征及找矿前景.四川有色金属, (3): 9-13. doi: 10.3969/j.issn.1006-4079.2011.03.003
[98]	郑有业, 薛迎喜, 程力军, 等, 2004.西藏驱龙超大型斑岩铜(钼)矿床:发现、特征及意义.地球科学, 29(1): 103-108. doi: 10.3321/j.issn:1000-2383.2004.01.018
[99]	郑有业, 张刚阳, 许荣科, 等, 2007.西藏冈底斯朱诺斑岩铜矿床成岩成矿时代约束.科学通报, 52(21): 2542-2548. doi: 10.3321/j.issn:0023-074x.2007.21.013
[100]	朱弟成, 段丽萍, 廖忠礼, 等, 2002.两类埃达克岩(Adakite)的判别.矿物岩石, 22(3): 5-9. doi: 10.3969/j.issn.1001-6872.2002.03.002