西藏查个勒铜铅锌矿成岩成矿时代及意义

高顺宝; 郑有业; 田立明; 张众; 屈文俊; 刘敏院; 郑海涛; 郑磊; 朱继华

doi:10.3799/dqkx.2012.057

西藏查个勒铜铅锌矿成岩成矿时代及意义

doi: 10.3799/dqkx.2012.057

高顺宝^{1, 2},
郑有业^{3, 4, ,},
田立明²,
张众²,
屈文俊⁵,
刘敏院⁶,
郑海涛²,
郑磊²,
朱继华²

1.
中国地质大学地质调查研究院, 湖北武汉 430074
2.
中国地质大学资源学院, 湖北武汉 430074
3.
中国地质大学地球科学与资源学院, 北京 100083
4.
中国地质大学地质过程与矿产资源国家重点实验室, 湖北武汉 430074
5.
国家地质实验测试中心, 北京 100037
6.
西藏华钰矿业有限公司, 西藏拉萨 850000

基金项目:

青藏专项项目 1212010918033

长江学者和创新团队发展计划 IRT1083

详细信息

作者简介:
高顺宝(1980-), 男, 博士研究生, 矿产普查与勘探专业

通讯作者:
郑有业, E-mail: zhyouye@163.com

中图分类号: P613
计量
- 文章访问数: 200
- HTML全文浏览量: 45
- PDF下载量: 2
- 被引次数: 0
出版历程
- 收稿日期: 2011-11-15
- 网络出版日期: 2021-11-09
- 刊出日期: 2012-05-01

Geochronology of Magmatic Intrusions and Mineralization of Chagele Copper-Lead-Zinc Deposit in Tibet and Its Implications

1.
Geological Survey, China University of Geosciences, Wuhan 430074, China
2.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
3.
Faculty of Earth Science and Mineral Resources, China University of Geosciences, Beijing 100083, China
4.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China
5.
National Research Center of Geoanalysis, Beijing 100037, China
6.
Tibet Huayu Mining Industry Company Limited, Lhasa 850000, China

摘要

摘要: 西藏查个勒铜铅锌矿在念青唐古拉铜铅锌银成矿带已发现的铜多金属矿床中处于最西端, 矿区同时存在接触交代-充填型铜铅锌矿化和斑岩型铜钼矿化.锆石LA-ICP-MS U-Pb和辉钼矿Re-Os测试表明, 矿区两种类型矿化近乎同时形成, 北部与铜铅锌矿化相关的花岗斑岩成岩时代为62.1±1.1 Ma(MSWD=2.7), 南部与铜钼矿化相关的花岗斑岩成岩时代为63.28±0.86 Ma(MSWD=3.2), 南部辉钼矿Re-Os等时线年龄为61.49±0.60 Ma(MSWD=1.5), 是在雅鲁藏布江洋盆北向俯冲后的同碰撞期形成的.该成果完善和充实了念青唐古拉铜铅锌银成矿带碰撞期成矿的时间演化序列, 且使该带规模在原有基础之上向西延伸了200 km(谢通门县青都-昂仁县查个勒), 显示该带为一条贯穿东西、以碰撞期成矿为主、长大于800 km的巨型铜铅锌银成矿带, 并为继续在此带向西寻找该类型矿床提供了重要依据.
- 念青唐古拉 /
- 查个勒矿床 /
- 碰撞期 /
- 成岩成矿 /
- 地质年代学
Abstract: Tibet chagele Copper-lead-zinc deposit is in the west end of those copper-polymetallic deposits found in Nyainqentanglha copper-lead-zinc-silver metallogenic belt, and there are two types of mineralization in the mining area, namely, copper-lead-zinc mineralization of the contact metasomatic filling and copper-molybdenum mineralization of porphyry. The zircon LA-ICP-MS U-Pb age and molybdenite Re-Os age show that two types of mineralization almost formed at the same time. The petrogenic age of the northern granite-porphyry related to copper-lead-zinc-silver mineralization is 62.1±1.1 Ma (MSWD=2.7), the southern granite-porphyry which is related to copper-molybdenum mineralization is 63.28±0.86 Ma (MSWD=3.2), and the molybdenite Re-Os age of the south is 61.49±0.60 Ma (MSWD=1.5), which formed at syn-collision stage after northward subduction of the Yarlung Zangbo oceanic basin. This study improves and enriches the time evolvement sequence and genesis of the collision metallogenic stage in Nyainqentanglha copper-lead-zinc-silver mineralization belt, and it also extends westwards its length by 200 km (Qingdu in Xietongmen-Chagele in Angren). As a result, it is found to be a huge copper-lead-zinc-silver metallogenic belt, extending in the direction of east-west more than 800 km, with deposits mainly formed in collection stage. In addition, this study provides important basis to the prospecting of the same deposits in the west of the belt.
- Nyainqentanglha /
- Chagele deposit /
- collision period /
- magmatism and mineralization /
- geochronology

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图 1 查个勒矿区地质简图

1.冰碛、冲洪积、残破积；2.始新统帕那组流纹质含火山角砾凝灰质熔岩；3.中二叠统下拉组三段灰岩、钙质板岩；4.中二叠统下拉组二段石英(杂)砂岩、板岩；5.中二叠统下拉组一段千枚岩；6.花岗斑岩；7.铜铅锌矿体；8.断层破碎带及铜钼矿体；9.断层；10.脆-韧性剪切带；11.采样位置

Fig. 1. Geological map of Chagele deposit

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图 2 查个勒矿区花岗斑岩锆石阴极发光照片

Fig. 2. CL images of zircons for porphyry granite in Chagele deposit

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图 3 查个勒矿区花岗斑岩锆石U-Pb谐和图

Fig. 3. U-Pb Concordia diagrams of zircons for porphyry granite in Chagele deposit

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图 4 查个勒矿区辉钼矿Re-Os等值线年龄(a)和加权平均年龄(b)

Fig. 4. Re-Os isotopic isochron diagram (a) and weighted meanmodelage diagram (b) of molybdenite in Chagele deposit

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表 1 查个勒矿区锆石LA-ICPMS同位素分析结果

Table 1. U-Pb LA-ICPMS analyses of zircon from Chagele deposit

点号	组成(10^-6)			Th/U	同位素比值						年龄(Ma)
点号	Pb	Th	U	Th/U	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ	²⁰⁷Pb/²⁰⁶Pb	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ
CGLD1-B4-1	5.74	259	433	0.60	0.059 0	0.003 0	0.083 9	0.004 2	0.010 4	0.000 1	565	109	81.8	3.9	66.8	0.8
CGLD1-B4-2	2.31	108	190	0.57	0.068 4	0.008 1	0.091 3	0.011 0	0.010 1	0.000 2	883	246	88.7	10.3	64.7	1.3
CGLD1-B4-3	3.09	176	223	0.79	0.078 3	0.006 2	0.107 1	0.008 3	0.010 1	0.000 2	1 154	158	103	7.6	64.8	1.2
CGLD1-B4-5	4.17	176	360	0.49	0.051 6	0.003 0	0.067 7	0.003 8	0.009 7	0.000 1	333	135	66.5	3.6	62.2	0.9
CGLD1-B4-6	5.85	277	497	0.56	0.048 0	0.002 9	0.064 1	0.003 7	0.009 8	0.000 1	102	137	63.1	3.5	63.0	0.9
CGLD1-B4-8	4.17	197	365	0.54	0.048 1	0.003 2	0.060 3	0.003 6	0.009 4	0.000 1	101.9	151.8	59.4	3.5	60.6	0.9
CGLD1-B4-9	7.61	303	575	0.53	0.052 3	0.005 3	0.077 2	0.007 4	0.010 8	0.000 1	298	233	75.5	7.0	69.4	0.9
CGLD1-B4-10	3.47	187	289	0.65	0.055 5	0.003 9	0.069 7	0.004 7	0.009 3	0.000 2	435	125	68.4	4.5	59.9	1.0
CGLD1-B4-11	4.66	198	320	0.62	0.081 0	0.004 2	0.120 4	0.006 4	0.010 8	0.000 2	1 233	101	115	5.8	69.1	1.0
CGLD1-B4-12	4.21	267	333	0.80	0.054 6	0.002 9	0.070 5	0.003 6	0.009 5	0.000 1	394	117	69.2	3.4	60.7	0.9
CGLD1-B4-14	3.92	176	310	0.57	0.053 8	0.003 1	0.074 8	0.004 3	0.010 1	0.000 2	361	127	73.2	4.0	64.8	1.1
CGLD1-B4-15	11.45	385	887	0.43	0.052 5	0.002 0	0.078 9	0.003 1	0.010 8	0.000 1	309	89	77.1	2.9	69.6	0.9
CGLD1-B4-16	8.89	341	691	0.49	0.048 8	0.002 1	0.072 0	0.003 0	0.010 7	0.000 1	139	102	70.6	2.8	68.8	0.9
CGLD1-B4-17	4.30	218	355	0.61	0.051 8	0.003 2	0.067 7	0.004 1	0.009 6	0.000 1	276	143	66.5	3.9	61.5	0.9
CGLD1-B4-18	5.72	273	467	0.58	0.048 9	0.002 5	0.065 3	0.003 5	0.009 7	0.000 1	143	120	64.2	3.3	62.5	0.8
CGLD1-B4-19	87.8	3 893	6 372	0.61	0.052 5	0.001 1	0.078 9	0.001 7	0.010 8	0.000 1	309	46	77.1	1.6	69.4	0.6
CGLD1-B4-20	3.28	204	261	0.78	0.059 4	0.003 9	0.077 9	0.005 0	0.009 7	0.000 1	583	141	76.2	4.7	62.0	0.9
CGLD3-B4-1	24.1	434	463	0.94	0.051 9	0.003 4	0.075 4	0.004 5	0.010 9	0.000 2	280	148	73.8	4.3	69.8	1.0
CGLD3-B4-2	13.7	246	348	0.71	0.055 8	0.003 3	0.074 2	0.004 2	0.009 8	0.000 1	443	130	72.7	3.9	62.7	0.9
CGLD3-B4-3	4.59	74.4	101	0.73	0.087 5	0.007 4	0.111 7	0.008 0	0.009 8	0.000 3	1 372	164	108	7	63.2	1.6
CGLD3-B4-4	17.5	279	351	0.79	0.068 0	0.008 7	0.094 0	0.011 7	0.010 2	0.000 2	878	262	91.2	10.9	65.3	1.0
CGLD3-B4-5	15.1	266	389	0.68	0.048 8	0.002 9	0.062 6	0.003 5	0.009 4	0.000 1	200	133	61.6	3.3	60.6	0.9
CGLD3-B4-6	17.9	293	392	0.75	0.050 0	0.002 8	0.069 7	0.003 8	0.010 2	0.000 2	195	130	68.4	3.6	65.7	1.0
CGLD3-B4-7	32.3	629	666	0.94	0.050 1	0.002 4	0.068 4	0.003 1	0.010 0	0.000 1	211	109	67.1	2.9	63.9	0.9
CGLD3-B4-8	8.9	163	191	0.85	0.067 7	0.008 4	0.085 5	0.010 6	0.009 6	0.000 2	861	255	83.3	9.9	61.7	1.1
CGLD3-B4-9	19.8	369	433	0.85	0.050 9	0.002 9	0.067 2	0.003 8	0.009 6	0.000 1	235	131	66.0	3.6	61.6	0.8
CGLD3-B4-10	25.1	450	582	0.77	0.047 4	0.002 7	0.064 0	0.003 5	0.009 9	0.000 1	77.9	120.4	63.0	3.3	63.2	0.8
CGLD3-B4-11	23.1	409	436	0.94	0.053 3	0.002 5	0.071 4	0.003 3	0.009 8	0.000 1	339	107	70.0	3.2	62.6	0.9
CGLD3-B4-12	11.2	182	205	0.89	0.054 8	0.004 9	0.069 1	0.005 7	0.009 5	0.000 2	467	200	67.8	5.4	60.6	1.2
CGLD3-B4-13	50.4	855	938	0.91	0.046 8	0.002 0	0.071 0	0.002 9	0.011 1	0.000 1	39.0	161.1	69.7	2.7	71.1	0.8
CGLD3-B4-14	13.9	229	261	0.88	0.050 8	0.003 2	0.074 5	0.004 6	0.010 7	0.000 2	232	146	73.0	4.4	68.4	1.0
CGLD3-B4-15	14.8	233	443	0.53	0.053 6	0.002 9	0.074 1	0.003 9	0.010 2	0.000 1	354	119	72.6	3.7	65.4	0.9
CGLD3-B4-16	29.6	515	668	0.77	0.051 7	0.002 3	0.071 2	0.003 0	0.010 1	0.000 1	333	106	69.8	2.9	64.9	0.7
CGLD3-B4-17	24.9	439	632	0.70	0.054 6	0.003 7	0.072 5	0.004 1	0.009 8	0.000 1	394	152	71.1	3.9	62.9	0.8
CGLD3-B4-18	15.6	287	280	1.02	0.055 3	0.003 9	0.075 9	0.005 0	0.010 2	0.000 2	433	157	74.3	4.8	65.6	1.1
CGLD3-B4-19	73	1 139	1 752	0.65	0.048 2	0.001 5	0.072 8	0.002 2	0.010 9	0.000 1	109	77	71.4	2.1	70.1	0.7
CGLD3-B4-20	23.6	424	527	0.80	0.051 0	0.002 6	0.067 6	0.003 4	0.009 7	0.000 1	239	119	66.4	3.2	62.5	0.7

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表 2 查个勒矿床辉钼矿Re-Os同位素分析数据

Table 2. Results of Re-Os sisotopic dating of molybdenite from Chagele deposit

样名	样重(g)	Re(10^-6)		普Os(10^-9)		¹⁸⁷Re(10^-6)		¹⁸⁷Os(10^-9)		模式年龄(Ma)
样名	样重(g)	测定值	不确定度	测定值	不确定度	测定值	不确定度	测定值	不确定度	测定值	不确定度
CGLMo1	0.102 16	3.366	0.027	0.010 3	0.005 2	2.116	0.017	2.164	0.020	61.37	0.90
CGLMo2	0.101 18	5.213	0.038	0.001 3	0.004 5	3.277	0.024	3.395	0.031	62.15	0.88
CGLMo3	0.100 11	1.391	0.012	0.001 3	0.003 0	0.874 3	0.007 6	0.901 2	0.007 6	61.84	0.90
CGLMo4	0.100 56	0.791 9	0.006 9	0.007 3	0.001 5	0.497 7	0.004 3	0.519 6	0.004 4	62.63	0.91
CGLMo5	0.101 88	1.636	0.016	0.008 7	0.004 4	1.028	0.010	1.054	0.009	61.54	0.95

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