西藏拿若斑岩型铜(金)矿含矿岩体年代学、地球化学及地质意义

丁帅; 唐菊兴; 郑文宝; 杨超; 张志; 王勤; 王艺云

doi:10.3799/dqkx.2017.001

西藏拿若斑岩型铜(金)矿含矿岩体年代学、地球化学及地质意义

doi: 10.3799/dqkx.2017.001

丁帅^1,,
唐菊兴^2, ,,
郑文宝²,
杨超²,
张志³,
王勤¹,
王艺云¹

1.
成都理工大学地球科学学院，四川成都 610059
2.
中国地质科学院矿产资源研究所，北京 100037
3.
成都地质矿产研究所，四川成都 610081

基金项目:

国土资源部公益性行业科研专项项目 201511017

详细信息

作者简介:
丁帅(1987-)，男，博士研究生，主要从事矿物学、岩石学、矿床学研究专业.ORCID:0000-0002-9837-9498.E-mail: 782628728@qq.com

通讯作者:
唐菊兴，ORCID:0000-0002-9162-6986.E-mail:tangjuxing@126.com

中图分类号: P597
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出版历程
- 收稿日期: 2016-07-15
- 刊出日期: 2017-01-15

Geochronology and Geochemistry of Naruo Porphyry Cu (Au) Deposit in Duolong Ore-Concentrated Area, Tibet, and Their Geological Significance

1.
College of Earth Science, Chengdu University of Technology, Chengdu 610059, China
2.
Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China
3.
Chengdu Center of China Geological Survey, Chengdu 610081, China

摘要

摘要: 多龙矿集区是班公湖-怒江成矿带最重要的组成部分，其成矿规模巨大、时间跨度较长、成矿过程复杂，因而人们对该区成岩成矿地质背景及岩石成因等问题一直争议不断，值得进一步明确.通过研究矿集区中部拿若斑岩型铜(金)矿与成矿相关的花岗闪长斑岩LA-ICP-MS锆石U-Pb年龄、全岩地球化学特征及Hf同位素组成，并与区域邻近矿床进行详细地对比研究，查明了多龙地区与成矿相关的岩浆岩形成构造背景、岩石成因及深部动力学过程.测试结果表明拿若铜(金)矿形成时代为早白垩世120Ma左右，与多龙地区其他矿床形成时代一致.这些岩浆岩均相对富集轻稀土(LREE)与大离子亲石元素(LILE: Rb, Ba, K等)；亏损重稀土(HREE )与高场强元素(HFSE: Nb, Ta, Zr, Hf等).原位锆石ε_Hf(t)均为正值，为1.38～7.37，Hf同位素两阶段模式年龄t_DM2为707～1086Ma，表明多龙矿集区斑岩-浅成低温热液型铜(金)矿形成与早白垩世班公湖-怒江特提斯洋北向俯冲有关.当俯冲洋壳到达地壳50～70km深度时发生不同程度相变，从而导致角闪石等矿物脱水产生的熔体交代楔形地幔，进而诱发幔源物质部分熔融产生弧岩浆，其形成环境类似于南美安第斯成矿带洋陆俯冲背景之下的陆缘弧环境.
- 拿若铜(金)矿 /
- 年代学 /
- 地球化学 /
- 锆石Hf同位素 /
- 陆缘弧 /
- 亏损地幔
Abstract: As the most important part of Bangong Lake-Nujiang River metallogenic belt, the Duolong ore-concentrated area is characterized by the occurrence of huge mineralization scale, extended time span and complex forming process, resulting in controversial understanding of its petrogenesis and tectonics and those of related deposits. To address this problem, this study firstly presents new data of LA-ICP-MS zircon U-Pb age, whole-rock geochemistry, and in situ zircon Hf isotopes for the mineralization-associated granite porphyry in Naruo porphyry copper (gold) deposit, and secondly we make a detailed comparison with research results of other porphyry deposits in Duolong area to find out the tectonic setting, petrogenesis and geodynamic processes of the mineralization-associated porphyry in Duolong area. The test results show that the age of the Naruo Cu (Au) deposit formation is consistent with that of other deposits in Duolong area formed at Early Cretaceous about 120Ma. All the main intrusive rocks have similar lithogeochemical characteristics, for they all show the relative enrichment in light rare earth elements (LREE) and large-ion lithophile elements (LILE: Rb, Ba, K, etc.), relatively depleted in heavy rare earth elements (HREE ) and high field strength elements (HFSE: Nb, Ta, Zr, Hf, etc.). Moreover, the granite porphyry shows positive ε_Hf(t) values between 1.38-7.37, and two-stage model ages of zircons are 707-1086Ma. The results suggest that the formation of porphyry-epithermal copper (gold) deposit in Duolong ore-concentrated area is dominated by northward subduction of the Bangongcuo Tethys plate beneath Qiangtang block at Early Cretaceous. When the subducted oceanic crust reached 50-70km underground and generated different degrees of phase transformation, which leads to melt produced by dehydration of amphibole minerals metasomatized mantle wedge and induced mantle partial melting produced magmatic arc. Those deposits occurred in a continental arc tectonic setting which is similar to the continental margin arc environment of the ocean-continent subduction setting of the Andes metallogenic belt in South America.
- Naruo copper (gold) deposit /
- geochronology /
- geochemistry /
- Hf zircon isotope /
- continental arc /
- depleted mantle

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图 1 研究区位置(a),西藏地区构造分区(b),班公湖-怒江结合带及邻区构造单元(c)

图b根据Hou et al.(2004)修改;图c根据耿全如等(2011)修改

Fig. 1. Geographic location(a),tectonic sketch in Tibet(b),tectonic units of the Bangong-Nujiang suture zone and its neighboring areas(c)

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图 2 多龙地区地质图(a),拿若铜(金)矿地质图(b),拿若矿区A-A＇剖面(c)

锆石U-Pb数据据Li et al.(2011a,2011b,2013)、方向等(2015)以及祝向平等(2015)

Fig. 2. Geological sketch of Duolong area(a)and Naruo porphyry Cu(Au)deposit(b),Section A-A＇ of the Naruo deposit(c)

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图 3 拿若斑岩型铜(金)矿岩石、矿石脉体及蚀变照片

a.斑岩型矿体;b.花岗闪长斑岩中浸染状金属矿物;c.长石石英砂岩中脉-网脉状矿体;d.含硫化物石英脉;e.角砾岩型矿体;f.角砾之间填充的金属矿物;g.含矿花岗闪长斑岩;h.含矿花岗闪长斑岩,发育弱钾化(样品用于LA-ICP-MS锆石测年及Hf同位素测试);i.含矿花岗闪长岩斑岩镜下照片;j.含矿花岗闪长岩斑岩镜下照片;k.不含矿花岗闪长斑岩,发育弱青磐岩化(样品用于LA-ICP-MS锆石测年及Hf同位素测试).Py.黄铁矿;Mt.磁铁矿;Cp.黄铜矿;Bn.斑铜矿;Cov.铜蓝;Sup.硫化物;Q.石英;Kfs.钾长石;Pl.斜长石;Bi.黑云母;Ep.绿帘石;Rut.金红石

Fig. 3. Photographs of rocks,ore minerals,veins and alterations in Naruo porphyry Cu(Au)deposit

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图 4 拿若斑岩型铜(金)矿区锆石CL图像、测点、U-Pb年龄及Hf同位素测试结果

Fig. 4. Zircon(CL)images with analysis spots,U-Pb ages and ε_Hf(t)values from the Naruo porphyry Cu(Au)deposit

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图 5 拿若矿区花岗闪长斑岩锆石U-Pb谐和图及²⁰⁶Pb/²³⁸U加权平均年龄

Fig. 5. Zircon U-Pb concordia diagrams and weighted mean ²⁰⁶Pb/²³⁸U ages of the granodiorite porphyry from the Naruo deposit

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图 6 拿若斑岩型铜(金)矿花岗闪长斑岩地球化学图解

a.A/CNK(摩尔)-A/NK(摩尔),底图据Peccerillo and Taylor(1976);b.稀土元素Cl球粒陨石标准化配分曲线;c.微量元素原始地幔标准化蛛网图;Cl球粒陨石及原始地幔值分别采用Boynton(1984)和Sun and McDonough(1989);多龙地区含矿与不含矿花岗闪长斑岩数据李金祥等(2008)、Li et al.(2013)以及陈华安等(2013);拿若矿区花岗闪长斑岩数据祝向平等(2015)

Fig. 6. Geochemical diagram of granodiorite porphyry from the Naruo porphyry Cu(Au)deposit

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图 7 拿若斑岩型铜(金)矿区锆石ε_Hf(t)值频率分布

以往研究数据祝向平等(2015)

Fig. 7. Frequency histogram of zircons ε_Hf(t)value from Naruo porphyry Cu(Au)deposit

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图 8 多龙地区主要岩浆活动

图中包括多不杂、波龙、拿若、拿顿、荣那5个矿床共计35个数据;数据佘宏全等(2009)、李金祥等(2008)、Li et al.(2011a,2011b,2013)、方向等(2015)、陈华安等(2013)、祝向平等(2015)以及王勤等(2015)

Fig. 8. Age of main magmatic event in Duolong area

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图 9 拿若斑岩型铜(金)矿区花岗闪长斑岩地球化学图解

a.Th/Ta-Yb,底图据Gorton and Schandl(2000);b.Th/Yb-Nb/Yb;底图据Pearce(1983);c.Th-Co-Zr/10;d.Th-Sc-Zr/10,底图据Bhatia and Crook(1986).A.洋岛弧;B.陆缘弧;C.活动大陆边缘;D.被动大陆边缘.图中符号同图 6a

Fig. 9. Geochemical discrimination diagrams of granodiorite porphyry from the Naruo porphyry Cu(Au)deposit

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图 10 拿若矿区花岗闪长斑岩岩石性质及源区判别

a.Y-Sr/Y,底图据Defant and Drummond(1990);b.Yb_N-(La/Yb)_N图解,底图据Martin(1999);c.Th/Ce-Th/Sm图解,底图据Boztuet al.(2007);d.Al₂O₃+FeO^T+MgO+TiO₂-Al₂O₃/(FeO^T+MgO+TiO₂)图解,底图据PatioDouce(1999);图中符号同图 6a

Fig. 10. Discriminant diagrams of rock properties and source region discrimination of Naruo granodiorite porphyry

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图 11 拿若矿区花岗闪长斑岩ε_Hf(t)与U-Pb年龄关系

部分数据祝向平等(2015);多龙地区数据李金祥等(2008)、Li et al.(2013)以及陈华安等(2013)

Fig. 11. Plot of ε_Hf(t)versus U-Pb ages of granodiorite porphyry from Naruo deposit

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图 12 多龙地区岩浆活动及矿床形成动力学模型

据Manning(2004)

Fig. 12. Geodynamic model for the generation of the magma and the formation of the deposit in Duolong area

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表 1 拿若矿区花岗闪长斑岩LA-ICP-MS锆石U-Pb同位素分析结果

Table 1. LA-ICP-MS zircon U-Pb isotopes analyzed data of the granodiorite porphyry from the Naruo deposite

样品点	Pb(10^-6)	Th(10^-6)	U(10^-6)	Th/U	同位素比值						年龄(Ma)
样品点	Pb(10^-6)	Th(10^-6)	U(10^-6)	Th/U	²⁰⁶Pb/²³⁸U	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁶Pb/²³⁸U	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁷Pb/²⁰⁶Pb	1σ
Z01-01	5	162	255	0.63	0.0187	0.0002	0.1443	0.0123	0.0560	0.0048	119.34	1.05	137	12	453	189
Z01-02	9	265	469	0.57	0.0186	0.0001	0.1553	0.0076	0.0606	0.0030	118.79	0.80	147	7	623	105
Z01-03	10	293	505	0.58	0.0189	0.0001	0.1252	0.0063	0.0479	0.0024	120.96	0.77	120	6	95	118
Z01-04	7	227	321	0.71	0.0188	0.0001	0.1350	0.0098	0.0520	0.0038	120.30	0.87	129	9	285	165
Z01-05	3	82	164	0.50	0.0187	0.0002	0.1395	0.0204	0.0540	0.0081	119.59	1.47	133	19	372	336
Z01-06	6	186	304	0.61	0.0188	0.0001	0.1413	0.0077	0.0544	0.0029	120.36	0.89	134	7	387	121
Z01-07	5	123	233	0.53	0.0189	0.0001	0.1605	0.0131	0.0615	0.0050	120.92	0.93	151	12	656	174
Z01-08	9	308	413	0.75	0.0190	0.0001	0.1752	0.0081	0.0669	0.0029	121.24	0.94	164	8	836	90
Z01-09	4	113	205	0.55	0.0190	0.0003	0.1300	0.0307	0.0496	0.0119	121.35	1.73	124	29	176	558
Z01-10	5	124	229	0.54	0.0191	0.0002	0.1293	0.0176	0.0492	0.0068	121.69	1.08	123	17	157	323
Z01-11	8	193	391	0.49	0.0191	0.0001	0.1267	0.0106	0.0482	0.0038	121.82	0.89	121	10	108	188
Z01-12	3	98	159	0.62	0.0191	0.0002	0.1380	0.0185	0.0523	0.0072	122.10	1.18	131	18	300	313
Z15-01	10	387	503	0.77	0.0185	0.0001	0.1412	0.0058	0.0555	0.0022	117.96	0.79	134	5	431	88
Z15-02	6	219	297	0.74	0.0185	0.0001	0.1467	0.0106	0.0575	0.0042	118.14	0.88	139	10	512	160
Z15-03	8	301	429	0.70	0.0185	0.0001	0.1304	0.0059	0.0510	0.0023	118.33	0.78	124	6	243	104
Z15-04	6	170	286	0.60	0.0188	0.0002	0.1400	0.0103	0.0540	0.0038	120.02	0.97	133	10	372	159
Z15-05	10	145	521	0.28	0.0187	0.0003	0.2119	0.0193	0.0824	0.0064	119.13	1.84	195	18	1255	152
Z15-06	11	450	528	0.85	0.0188	0.0001	0.1408	0.0063	0.0542	0.0024	120.31	0.79	134	6	380	99
Z15-07	5	150	251	0.60	0.0190	0.0001	0.1270	0.0105	0.0485	0.0040	121.21	0.92	121	10	126	193
Z15-08	4	109	214	0.51	0.0188	0.0002	0.1260	0.0186	0.0486	0.0074	120.02	1.07	121	18	130	357
Z15-09	3	80	159	0.50	0.0188	0.0002	0.1322	0.0174	0.0510	0.0070	120.00	1.12	126	17	242	316
Z15-10	8	179	441	0.41	0.0186	0.0001	0.1342	0.0084	0.0523	0.0032	118.87	0.79	128	8	299	140
Z15-11	14	565	689	0.82	0.0187	0.0001	0.1146	0.0043	0.0444	0.0016	119.63	0.90	110	4	-90	90
注：因测得年龄＜1000Ma，故采用²⁰⁶Pb/²³⁸U年龄.

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表 2 拿若斑岩型铜(金)矿区花岗闪长斑岩的主量元素(%)和微量元素(10^-6)分析结果

Table 2. Major elements(%)and trace elements(10^-6)analytic data of the granodiorite porphyry from the Naruo porphyry Cu(Au)deposit

岩性样品编号	含矿花岗闪长斑岩					不含矿花岗闪长斑岩
岩性样品编号	Z01-125	Z01-278	Z07-263	Z07-301	Z08-239	Z15-179	Z15-255
SiO₂	65.01	65.13	64.53	65.54	64.85	63.91	64.71
Al₂O₃	15.19	14.16	15.98	15.87	15.45	15.50	14.96
Fe₂O₃	1.66	2.75	2.89	2.83	2.19	2.33	2.22
FeO	4.29	3.17	3.02	2.44	3.82	4.19	3.84
MgO	1.57	1.65	1.71	1.62	1.66	1.74	1.73
CaO	3.00	2.00	2.82	1.48	3.05	3.86	3.60
K₂O	3.01	4.60	2.64	3.44	2.80	2.61	2.25
TiO₂	0.37	0.36	0.37	0.32	0.38	0.39	0.38
MnO	0.14	0.19	0.07	0.07	0.09	0.08	0.09
P₂O₅	0.13	0.12	0.14	0.10	0.12	0.15	0.13
LOSS	2.55	4.34	2.57	3.46	2.67	2.17	2.73
Total	99.45	98.57	99.44	99.17	99.37	99.64	99.34
FeO^T	5.79	5.64	5.62	4.98	5.79	6.28	5.84
Mg^#	32.6	34.27	35.15	36.68	33.84	33.06	34.56
ANK	2.05	2.74	2.19	2.26	2.27	2.18	2.13
ACNK	1.18	1.61	1.29	1.63	1.25	1.12	1.08
Bi	0.70	2.21	0.22	0.52	0.48	0.22	0.10
Li	28.30	25.05	30.46	23.76	21.51	24.58	27.53
Be	1.46	1.09	1.36	1.25	1.30	1.17	1.33
Sc	8.97	7.07	8.25	7.81	8.03	7.16	7.71
V	81.62	59.88	76.13	87.61	82.01	74.19	83.80
Cr	7.34	4.78	5.77	5.05	6.03	6.18	7.23
Co	9.33	7.53	6.22	6.05	8.09	8.35	8.80
Ni	5.96	4.62	3.83	2.69	6.54	7.33	13.19
Cu	602.00	5 733.00	399.30	357.30	1 422.00	2 528.50	356.30
Pb	12.57	10.44	9.44	6.07	10.67	10.75	8.76
Zn	110.05	77.25	60.87	50.05	64.84	67.41	38.05
Ga	18.04	15.62	18.27	18.09	17.56	17.99	18.16
Rb	72.32	193.70	75.71	133.10	90.12	63.51	90.49
Sr	421.40	421.70	402.70	208.20	379.30	453.85	480.90
Y	12.07	7.99	12.57	12.84	8.93	9.35	9.59
Zr	95.18	76.82	91.61	84.08	97.41	97.92	89.95
Nb	8.81	6.59	5.26	5.27	7.29	6.78	7.88
Cs	18.32	17.71	16.62	15.98	10.99	10.92	28.79
Ba	615.70	791.20	515.70	591.30	425.90	414.60	482.50
La	12.60	9.33	10.60	15.44	8.74	10.60	10.72
Ce	18.72	15.42	16.19	25.60	12.59	15.30	15.64
Pr	2.84	2.35	2.60	3.89	1.89	2.26	2.29
Nd	11.28	9.27	10.86	15.56	7.61	9.03	9.07
Sm	2.19	1.88	2.20	2.96	1.47	1.74	1.73
Eu	0.60	0.69	0.63	0.81	0.51	0.57	0.58
Gd	1.88	1.86	1.96	2.71	1.40	1.59	1.59
Tb	0.35	0.35	0.37	0.50	0.26	0.28	0.28
Dy	1.90	1.98	2.08	2.71	1.41	1.55	1.52
Ho	0.35	0.32	0.38	0.47	0.26	0.29	0.28
Er	1.18	1.09	1.26	1.56	0.84	0.92	0.90
Tm	0.19	0.17	0.20	0.27	0.13	0.14	0.14
Yb	1.31	1.11	1.38	1.62	0.86	0.90	0.90
Lu	0.21	0.17	0.22	0.26	0.14	0.15	0.14
Hf	12.07	7.99	12.57	12.84	8.93	9.35	9.59
Ta	0.76	0.57	0.48	1.00	0.52	0.53	0.71
Tl	0.84	1.65	0.88	1.08	1.09	0.85	1.31
Th	9.93	9.06	8.07	6.76	6.59	7.07	7.36
U	1.12	0.88	0.87	0.75	0.37	0.49	0.64
ΣREE	55.57	45.99	50.93	74.38	38.10	45.32	45.79
LREE	48.22	38.93	43.07	64.28	32.81	39.50	40.03
HREE	7.35	7.06	7.86	10.10	5.29	5.82	5.76
LREE/HREE	6.56	5.52	5.48	6.37	6.20	6.79	6.95
δEu	0.91	1.14	0.93	0.88	1.09	1.05	1.07
δCe	0.77	0.81	0.76	0.81	0.76	0.77	0.77
La_N/Yb_N	6.91	6.04	5.53	6.84	7.28	8.41	8.54
注:A/CNK=(Al₂O₃)/(CaO+K₂O+Na₂O)摩尔比值;A/NK=(Al₂O₃)/(K₂O+Na₂O)摩尔比值;δEu=Eu_N/[(Sm_N)×(Gd_N)]^1/2;δCe=Ce_N/[(La_N)×(Pr_N)]^1/2.

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表 3 拿若斑岩型铜(金)矿区锆石Hf同位素分析结果

Table 3. Hf isotopes analyzed data of the zircons from the Naruo porphyry Cu(Au)deposit

岩性	样品编号	年龄(Ma)	¹⁷⁶Yb/¹⁷⁷Hf	¹⁷⁶Lu/¹⁷⁷Hf	¹⁷⁶Hf/¹⁷⁷Hf	2σ	(¹⁷⁶Hf/¹⁷⁷Hf)_i	ε_Hf(0)	ε_Hf(t)	2σ	t_DM1(Ma)	t_DM2(Ma)	f_Lu/Hf
含矿花岗闪长斑岩	Z01-01	119.59	0.062560	0.001861	0.282868	0.000016	0.282864	3.39	5.87	0.6	558	801	-0.94
	Z01-02	121.24	0.035551	0.001092	0.282883	0.000016	0.282881	3.94	6.51	0.6	524	761	-0.97
	Z01-03	121.69	0.059476	0.001616	0.282893	0.000014	0.282890	4.29	6.83	0.5	517	741	-0.95
	Z01-04	120.92	0.047134	0.001418	0.282881	0.000015	0.282878	3.85	6.39	0.5	532	768	-0.96
	Z01-05	121.35	0.052565	0.001445	0.282889	0.000016	0.282886	4.13	6.68	0.6	521	750	-0.96
	Z01-06	120.30	0.034450	0.001024	0.282863	0.000015	0.282860	3.21	5.77	0.5	553	808	-0.97
	Z01-07	122.10	0.026299	0.000772	0.282906	0.000016	0.282905	4.75	7.37	0.6	487	707	-0.98
	Z01-08	121.82	0.031657	0.000958	0.282899	0.000013	0.282897	4.50	7.09	0.5	500	724	-0.97
	Z01-09	120.36	0.054250	0.001642	0.282876	0.000013	0.282872	3.67	6.18	0.5	543	781	-0.95
不含矿花岗闪长斑岩	Z15-01	121.21	0.029555	0.000831	0.282846	0.000017	0.282845	2.63	5.23	0.6	573	843	-0.97
	Z15-02	120.02	0.019530	0.000565	0.282853	0.000014	0.282852	2.88	5.47	0.5	559	827	-0.98
	Z15-03	120.00	0.047284	0.001260	0.282860	0.000016	0.282857	3.10	5.63	0.6	561	816	-0.96
	Z15-04	118.14	0.032316	0.000841	0.282740	0.000016	0.282738	-1.15	1.38	0.6	724	1086	-0.97
	Z15-05	120.02	0.031431	0.000879	0.282830	0.000015	0.282828	2.05	4.62	0.5	597	881	-0.97
	Z15-06	120.31	0.034790	0.000999	0.282844	0.000015	0.282842	2.54	5.10	0.5	579	851	-0.97
	Z15-07	118.33	0.033119	0.000980	0.282829	0.000016	0.282827	2.01	4.53	0.6	600	885	-0.97
	Z15-08	119.13	0.032367	0.001021	0.282835	0.000015	0.282833	2.23	4.77	0.5	592	871	-0.97

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西藏拿若斑岩型铜(金)矿含矿岩体年代学、地球化学及地质意义

doi: 10.3799/dqkx.2017.001

作者简介:
丁帅(1987-)，男，博士研究生，主要从事矿物学、岩石学、矿床学研究专业.ORCID:0000-0002-9837-9498.E-mail: 782628728@qq.com

通讯作者:
唐菊兴，ORCID:0000-0002-9162-6986.E-mail:tangjuxing@126.com

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Geochronology and Geochemistry of Naruo Porphyry Cu (Au) Deposit in Duolong Ore-Concentrated Area, Tibet, and Their Geological Significance

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留言板

西藏拿若斑岩型铜(金)矿含矿岩体年代学、地球化学及地质意义

doi: 10.3799/dqkx.2017.001

作者简介: 丁帅(1987-)，男，博士研究生，主要从事矿物学、岩石学、矿床学研究专业.ORCID:0000-0002-9837-9498.E-mail: 782628728@qq.com

通讯作者: 唐菊兴，ORCID:0000-0002-9162-6986.E-mail:tangjuxing@126.com

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出版历程

Geochronology and Geochemistry of Naruo Porphyry Cu (Au) Deposit in Duolong Ore-Concentrated Area, Tibet, and Their Geological Significance

计量

出版历程

目录

作者简介:
丁帅(1987-)，男，博士研究生，主要从事矿物学、岩石学、矿床学研究专业.ORCID:0000-0002-9837-9498.E-mail: 782628728@qq.com

通讯作者:
唐菊兴，ORCID:0000-0002-9162-6986.E-mail:tangjuxing@126.com