西藏班公湖-怒江结合带中段去申拉组火山岩年代学及勘查找矿方向

邓世林; 林彬; 张海潮; 阿旺仁增; 王腾; 胡志中; 邹兵; 张忠坤; 杨征坤; 刘振宇

doi:10.3799/dqkx.2019.039

西藏班公湖-怒江结合带中段去申拉组火山岩年代学及勘查找矿方向

doi: 10.3799/dqkx.2019.039

邓世林^1, ,,
林彬^2, , ,,
张海潮³,
阿旺仁增³,
王腾³,
胡志中⁴,
邹兵⁵,
张忠坤⁶,
杨征坤⁶,
刘振宇⁷

1.
四川省冶金地质勘查局六○五大队, 四川眉山 620860
2.
中国地质科学院矿产资源研究所自然资源部成矿作用与资源评价重点实验室, 北京 100037
3.
西藏自治区地质矿产勘查开发局第五地质大队, 青海格尔木 810600
4.
自然资源部沉积盆地与油气重点实验室, 四川成都 610081
5.
中国地质大学地球科学与资源学院, 北京 100083
6.
西藏华泰龙矿业开发有限公司, 西藏拉萨 850000
7.
吉林省地质调查院, 吉林长春 130102

基金项目:

中国地质调查局二级项目 DD20160026

国家重点研发-深地专项 2018YFC064101

中国地质科学院基本科研业务费 SYSCR2019-02

西藏自治区科技计划项目 XZ201901-GB-24

国家自然科学基金项目 41902097

详细信息

作者简介:
邓世林(1985-), 男, 高级工程师, 主要从事青藏高原矿产地质调查研究

通讯作者:
林彬

中图分类号: P597
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- 被引次数: 0
出版历程
- 收稿日期: 2018-11-19
- 刊出日期: 2020-03-15

Geochronology and Ore Prospecting Potential of Qushenla Formation in Middle Segment of Bangong Co-Nujiang Suture Zone, Tibet

1.
No. 605 Party of Sichuan Metallurgical Geology Bureau, Meishan 620860, China
2.
MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources of Chinese Academy of Geological Sciences, Beijing 100037, China
3.
No.5 Geological Party of Tibet Bureau of Geology and Mineral Exploration and Development, Golmud 810600, China
4.
MNR Key Laboratory for Sedimentary Basin and Oil and Gas Resources, Chengdu 610081, China
5.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
6.
Tibet Huatailong Mining Development Co. Ltd., Lhasa 850000, China
7.
Geological Survey Institute of Jilin Province, Changchun 130102, China

摘要

摘要: 作为班公湖-怒江结合带最为重要的火山岩沉积地层之一，去申拉组一直缺乏精细的年代学研究和找矿潜力的分析.基于班-怒结合带中段尼玛县北部长期的矿产地质调查工作，对热过勒、饿蒙勒、阿俄作登等地区的去申拉组进行了详细解剖，并利用锆石U-Pb定年精细厘定区内去申拉组中英安岩、安山岩的结晶时限分别为106.2±1.3 Ma、107.7±1.4 Ma，属于早白垩世火山活动的产物.同时，区内1：5万水系沉积物异常以及实地调查揭示，阿俄作登和饿蒙勒地区存在良好铜、金、银组合异常，初步揭露1条高品位的矿化体.结合区域成矿作用背景分析，认为该区存在良好的斑岩-浅成低温热液型铜多金属成矿系统的找矿潜力.班公湖-怒江结合带去申拉火山沉积地层的形成时限的精确厘定，为区域基础地质格架的构建提供了直接证据；而其矿化信息的首次揭露，为该带早白垩世大面积覆盖的火山岩地区的勘查找矿工作指明了新方向.
- 去申拉组 /
- 地质年代学 /
- 斑岩-浅成低温热液 /
- 班公湖-怒江结合带 /
- 西藏
Abstract: The Qushenla Formation is one of the most important volcanic strata in Bangong Co-Nujiang suture zone, however, there is no detailed geochronology and prospecting potential study. Based on long-term ore geological survey in Nima County, we do a detailed study on the Qushenla Formation in Reguole, Emengle, Aezuodeng areas, and date the dacite and andesite in Qushenla Formation with U-Pb age of zircons. They are 106.2±1.3 Ma and 107.7±1.4 Ma, respectively, as the result of Early Cretaceous magmatism. At the same time, good Cu, Au, Ag anomalies and one high-grade copper-bearing mineralized body were found in Aezuodeng and Emengle areas, according to the 1:50 000 stream sedimentary analysis. Given the regional metallogenic background, we suggest this area is a good prospecting target for porphyry-epithermal copper system exploration. The precise geochronology of Qeshenla Formation gives the direct evidence for the framework building of regional strata. The first discovery of the mineralization in Qushenla Formation reveals a new direction for the further exploration and prospecting in the large area of the Bangong Co-Nujiang suture zone covered volcanic rocks.
- Qushenla Formation /
- geochronology /
- porphyry-epithermal /
- Bangong Co-Nujiang suture zone /
- Tibet

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图 1 班-怒结合带去申拉组分布情况（a）和尼玛地区去申拉组地质简图（b、c、d）

年龄数据引自西藏自治区地质调查院, 2002, 中华人民共和国1︰25万区域地质调查报告班戈县幅；四川省地质调查院, 2006, 中华人民共和国1︰25万区域地质调查报告物玛幅；河南省地质调查院, 2002, 中华人民共和国1︰25万区域地质调查报告尼玛幅；四川省地质调查院, 2003, 中华人民共和国1︰25万区域地质调查报告革吉县幅；吉林省地质调查院, 2006, 中华人民共和国1︰25万区域地质调查报告帕度错幅；李伟（2012）；吴浩等（2013）.1.第四系；2.新近纪康托组；3.晚白垩世竟柱山组；4.早白垩世去申拉组；5.晚侏罗世沙木罗组；6.早中侏罗世木嘎岗日岩群；7.石英闪长岩；8.铜矿化体；9.采样位置；10.地层界线；11.角度不整合界线；12.逆断层；13.剖面位置

Fig. 1. Distribution of Qushenla Formation in Ban-Nu suture zone(a) and geological map of Nima area(b, c, d)

下载: 全尺寸图片幻灯片

图 2 去申拉组剖面测量及分层岩性

图中1~9层的岩性见文中描述

Fig. 2. Section of Qushenla Formation and its lithology

下载: 全尺寸图片幻灯片

图 3 去申拉组火山岩露头及镜下（正交）照片

a.英安岩；b.安山岩；c.玄武岩. Aug.辉石；Pl.斜长石；Q.石英

Fig. 3. The outcrops and microscopic pictures (crossed) of Qushenla Formation

下载: 全尺寸图片幻灯片

图 4 部分锆石阴极发光图像及测年结果

a.阿俄作登英安岩；b.饿蒙勒安山岩

Fig. 4. CL images and U-Pb ages of partial zircons

下载: 全尺寸图片幻灯片

图 5 锆石LA-ICP-MS U-Pb谐和图与²⁰⁶Pb/²³⁸U加权平均值

Fig. 5. U-Pb concordia diagrams and ²⁰⁶Pb/²³⁸U weight average ages of zircons

下载: 全尺寸图片幻灯片

图 6 班-怒结合带去申拉组年代学测试结果

Fig. 6. Chronological results of Qushenla Formation in Ban-Nu suture zone

下载: 全尺寸图片幻灯片

图 7 饿蒙勒-阿俄作登地区水系沉积物异常

Fig. 7. Anomaly of stream sedimentary deposits from Emengle-Aezuodeng area

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图 8 饿蒙勒-阿俄作登地区矿化露头

Fig. 8. Outcrops of mineralization from Emengle-Aezuodeng area

下载: 全尺寸图片幻灯片

表 1 去申拉组火山岩中锆石U-Pb测年结果

Table 1. U-Pb dating results of zircons from Qushenla Formation

测点号	含量(10^-6)		Th/ U	比值				年龄（Ma）				谐和度 (%)
测点号	Th	U	Th/ U	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ	²⁰⁷Pb/²³⁵U	1σ	²⁰⁶Pb/²³⁸U	1σ	谐和度 (%)
AE-b1-2	349	366	1.0	0.110 7	0.010 1	0.016 9	0.000 5	106.6	9.2	108.1	3.1	98
AE-b1-3	190	236	0.8	0.111 0	0.016 2	0.016 1	0.000 6	106.9	14.8	103.0	3.6	96
AE-b1-4	243	282	0.9	0.120 4	0.014 2	0.017 4	0.000 5	115.4	12.8	111.0	3.4	96
AE-b1-5	228	259	0.9	0.124 3	0.015 5	0.017 1	0.000 6	118.9	14.0	109.2	3.7	91
AE-b1-6	300	332	0.9	0.114 2	0.013 2	0.016 3	0.000 5	109.8	12.0	104.5	3.3	95
AE-b1-7	207	250	0.8	0.108 5	0.014 1	0.016 4	0.000 6	104.6	13.0	104.8	3.5	99
AE-b1-8	222	266	0.8	0.110 8	0.013 6	0.015 9	0.000 5	106.7	12.4	101.8	3.1	95
AE-b1-10	219	271	0.8	0.108 8	0.013 9	0.016 3	0.000 6	104.9	12.7	104.4	3.5	99
AE-b1-11	220	255	0.9	0.119 1	0.014 2	0.016 9	0.000 6	114.2	12.9	108.0	3.7	94
AE-b1-12	231	245	0.9	0.107 2	0.010 1	0.016 6	0.000 6	103.4	9.3	106.0	3.6	97
AE-b1-14	341	337	1.0	0.109 0	0.015 3	0.017 1	0.000 5	105.1	14.1	109.1	2.9	96
AE-b1-15	377	389	1.0	0.112 9	0.011 5	0.016 7	0.000 4	108.6	10.5	106.7	2.7	98
AE-b1-16	142	196	0.7	0.104 2	0.018 5	0.016 5	0.000 6	100.7	17.0	105.5	3.7	95
AE-b1-18	229	260	0.9	0.094 6	0.011 1	0.015 3	0.000 5	91.8	10.3	97.9	3.0	93
AE-b1-19	330	350	0.9	0.109 9	0.012 0	0.016 1	0.000 4	105.9	10.9	102.8	2.6	97
AE-b1-20	301	304	1.0	0.106 4	0.012 2	0.017 2	0.000 5	102.7	11.2	110.2	3.3	92
AE-b1-22	170	205	0.8	0.122 3	0.011 5	0.016 6	0.000 6	117.2	10.4	106.4	3.7	90
AE-b1-23	239	271	0.9	0.113 0	0.011 2	0.017 1	0.000 5	108.7	10.2	109.1	3.4	99
AE-b1-24	193	210	0.9	0.114 7	0.013 3	0.017 4	0.000 6	110.3	12.1	111.4	3.9	99
AE-b1-26	232	262	0.9	0.118 4	0.013 2	0.016 3	0.000 5	113.6	12.0	104.0	3.2	91
AE-b1-27	166	203	0.8	0.120 2	0.012 3	0.016 8	0.000 7	115.2	11.1	107.6	4.3	93
AE-b1-29	303	333	0.9	0.122 3	0.010 3	0.016 6	0.000 5	117.2	9.3	106.4	3.4	90
AE-b1-30	180	197	0.9	0.126 8	0.020 5	0.017 4	0.000 6	121.2	18.4	111.2	4.1	91
AE-b1-31	236	278	0.9	0.112 3	0.010 8	0.016 3	0.000 5	108.1	9.8	104.5	3.1	96
AE-b1-32	293	281	1.0	0.110 2	0.012 0	0.017 1	0.000 5	106.2	11.0	109.1	3.1	97
EM-b3-1	281	398	0.7	0.113 3	0.012 0	0.016 8	0.000 4	109.0	10.9	107.5	2.5	98
EM-b3-5	456	528	0.9	0.104 9	0.012 3	0.016 3	0.000 4	101.3	11.3	104.0	2.5	97
EM-b3-8	333	474	0.7	0.104 9	0.010 6	0.016 9	0.000 4	101.3	9.8	107.7	2.7	93
EM-b3-9	314	417	0.8	0.107 8	0.012 5	0.017 2	0.000 5	103.9	11.5	110.1	3.2	94
EM-b3-10	358	451	0.8	0.119 3	0.010 7	0.016 4	0.000 4	114.4	9.7	104.8	2.8	91
EM-b3-12	239	375	0.6	0.109 9	0.012 2	0.017 1	0.000 5	105.9	11.1	109.5	3.0	96
EM-b3-14	176	251	0.7	0.116 6	0.016 1	0.016 5	0.000 5	112.0	14.6	105.7	3.0	94
EM-b3-15	276	437	0.6	0.122 8	0.011 7	0.017 4	0.000 5	117.6	10.6	111.1	2.9	94
EM-b3-16	490	555	0.9	0.111 9	0.011 4	0.016 8	0.000 5	107.7	10.4	107.7	3.0	99
EM-b3-17	176	238	0.7	0.108 6	0.017 2	0.017 1	0.000 7	104.7	15.7	109.5	4.6	95
EM-b3-18	247	359	0.7	0.114 2	0.011 8	0.017 0	0.000 5	109.8	10.7	108.7	3.1	98
EM-b3-19	410	502	0.8	0.109 7	0.011 7	0.016 8	0.000 4	105.7	10.7	107.5	2.8	98
EM-b3-20	209	267	0.8	0.116 5	0.013 0	0.017 1	0.000 6	111.9	11.9	109.3	4.0	97
EM-b3-25	241	341	0.7	0.108 0	0.014 7	0.016 8	0.000 5	104.2	13.5	107.2	3.1	97
EM-b3-26	259	245	1.1	0.106 4	0.015 4	0.016 6	0.000 5	102.7	14.1	106.1	3.4	96
EM-b3-27	234	314	0.7	0.111 3	0.010 8	0.017 0	0.000 5	107.2	9.9	108.8	3.4	98
EM-b3-31	318	413	0.8	0.116 0	0.009 9	0.017 2	0.000 5	111.4	9.0	110.2	3.1	98
注：AE-b1编号为阿俄作登地区英安岩，EM-b3编号为饿蒙勒地区安山岩.

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