念扎金矿床热历史:锆石U-Pb、(U-Th)/He及磷灰石裂变径迹年代学的制约

张雄; 赵晓燕; 杨竹森

doi:10.3799/dqkx.2018.379

念扎金矿床热历史:锆石U-Pb、(U-Th)/He及磷灰石裂变径迹年代学的制约

doi: 10.3799/dqkx.2018.379

张雄^1, ,,
赵晓燕^2, ,,
杨竹森²

1.
北京矿产地质研究院, 北京 100012
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

基金项目:

深地资源勘查开采专项 2016YFC0600307

深地资源勘查开采专项 2016YFC0600306

国家自然科学基金项目 4170020919

中国地质科学院基本科研业务费项目 KK1709

详细信息

作者简介:
张雄(1988-), 男, 工程师, 主要从事矿床学的研究

通讯作者:
赵晓燕

中图分类号: P611
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出版历程
- 收稿日期: 2018-08-19
- 刊出日期: 2019-06-15

Thermal History of Nianzha Gold Deposit: Constraints from Zircon U-Pb, (U-Th)/He and Apatite Fission Track Geochronology

Zhang Xiong^{1
,
,},
Zhao Xiaoyan^{2
, ,},
Yang Zhusen²

1.
Beijing Institute of Geology for Mineral Resources, Beijing 100012, China
2.
Key Laboratory of Earth Probe and Geodynamics, Ministry of Natural Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

摘要

摘要: 念扎金矿床是近年来最新发现的位于雅鲁藏布江缝合带南侧仁布构造混杂岩带与蚀变闪长岩接触带的大型造山型金矿床.为约束念扎矿床的冷却及剥露历史，利用锆石的U-Pb、（U-Th）/He及磷灰石裂变径迹定年对新鲜及矿化闪长岩年龄进行测定.结果表明，新鲜闪长岩锆石U-Pb年龄为（46.32±0.53）Ma，（U-Th）/He年龄介于（7.14±0.24）Ma到（9.80±0.27）Ma，矿化闪长岩锆石（U-Th）/He年龄介于（8.38±0.24）Ma到（11.19±0.31）Ma之间，两件矿化闪长岩磷灰石裂变径迹年龄分别为（5.9±0.5）Ma和（5.3±1.0）Ma.念扎金矿床自闪长岩固结以来经历了两次快速冷却过程：第一次是从46.3 Ma开始持续到43.6 Ma，温度从750℃降至350℃，冷却速率高达约148℃/Ma；第二次为8.5~2.0 Ma，温度从约200℃降至30℃，冷却速率为26℃/Ma.念扎矿床成矿深度为9.7 km；在8.5 Ma时，矿床被抬升至4.6 km处；从8.5~5.6 Ma，矿床抬升至2.8 km；从5.6~2.0 Ma，念扎矿床被剥露至地表.
- U-Pb定年 /
- (U-Th)/He定年 /
- 裂变径迹年龄 /
- 热演化历史 /
- 念扎金矿床 /
- 岩石学
Abstract: The Nianzha gold deposit, located in the central section of the Yurlung-Zangbo suture zone is a large orogenic gold deposit which occurred in a fracture zone bordered by altered diorite in the hanging wall to the north and the Renbu tectonic mélange in the footwall to the south. In this paper, it combines zircon U-Pb, (U-Th)/He and apatite fission track dating of the fresh and mineralized diorite in order to restrict the cooling and denudation history of the Nianzha deposit. The results show that the zircon U-Pb age of the fresh diorite is (46.32±0.53) Ma and zircon (U-Th)/He ages of fresh diorite is between (7.14 ±0.24) Ma and (9.80 ±0.27) Ma, and the zircon (U-Th)/He ages of the mineralized diorite are between (8.38±0.24) Ma and (11.19±0.31) Ma. The apatite fission track ages of two mineralization diorite are (5.9±0.5) Ma and (5.3±1.0) Ma respectively. Since the consolidation of the diorite, the Nianzha gold deposit has experienced two rapid cooling processes:the first process started from 46.3 Ma to 43.6 Ma, and the temperature dropped from 750℃ to 350℃ with the cooling rate of about 148℃/Ma, while the second process happened between 8.5~2.0 Ma with the temperature dropped from 200℃ to 30℃ with cooling rate of about 26℃/Ma. The mineralization depth of the Nianzha deposit is about 9.7 km; at 8.5 Ma, the deposit was uplifted to 4.6 km; from 8.5 to 5.6 Ma, the deposit are uplifted to 2.8 km; and from 5.6 to 2.0 Ma, the Nianzha deposit was exfoliated to the surface.
- U-Pb dating /
- (U-Th)/He dating /
- fission track age /
- thermal history /
- Nianzha gold deposit /
- petrology

HTML全文

图 1 青藏高原造山型金成矿带(a)及日喀则-仁布区域地质简图(b)

a据侯增谦和王二七（2008）改编

Fig. 1. Geological maps of orogenic gold metallogenic belts in the Tibetan orogenic belt (a) and Xigaze-Renbu area, southern Tibet (b)

下载: 全尺寸图片幻灯片

图 2 念扎金矿矿区地质简图(a)、念扎金矿矿体分布图(b)和勘探线剖面图(c)

Fig. 2. (a) Geological map of Nianzha deposit; (b) map of orebody distribution of Nianzha deposit; (c) cross-section along the prospecting line

下载: 全尺寸图片幻灯片

图 3 念扎矿床岩石特征

a~c.砂板岩野外露头手标本及镜下照片；d~f.闪长岩野外露头、手标本及镜下照片，由角闪石和斜长石组成；g~i.强蛇纹石化超基性岩野外露头、手标本及镜下照片；j~l.脉状煌斑岩野外露头、手标本及镜下照片

Fig. 3. Petrologic characteristics of rocks from the Nianzha deposit

下载: 全尺寸图片幻灯片

图 4 念扎矿区闪长岩锆石CL图像(a)及U-Pb定年结果(b)

Fig. 4. Zircon CL images (a) and U-Pb dating results (b) of diorite at Nianzha deposit

下载: 全尺寸图片幻灯片

图 5 念扎矿区中闪长岩(U-Th)/He定年锆石显微照片

Fig. 5. Microscopy images of zircons for (U-Th)/He dating in diorite at Nianzha deposit

下载: 全尺寸图片幻灯片

图 6 念扎闪长岩ZHe年龄和U含量关系

Fig. 6. Relationship between ZHe age and U contents in diorite at Nianzha deposit

下载: 全尺寸图片幻灯片

图 7 磷灰石单颗粒年龄分布雷达图和直方图

Fig. 7. Radical plots and histograms of apatite samples

下载: 全尺寸图片幻灯片

图 8 念扎矿区中闪长岩热历史模拟结果(a)及He扩散曲线(b)

Fig. 8. Modeling results for thermal history of diorite at Nianzha deposit (a) and diffusion curve (b)

下载: 全尺寸图片幻灯片

图 9 念扎金矿床热演化模拟

Fig. 9. Hydrothermal evolution diagram of Nianzha gold deposit

下载: 全尺寸图片幻灯片

表 1 磷灰石裂变径迹分析结果

Table 1. The apatite fission track analysis results

实验号	原样号	颗粒数 (n)	ρ_s(10⁵/cm²) (Ns)	ρ_i(10⁵/cm²) (Ni)	ρ_d(10⁵/cm²) (N)	P(χ²) (%)	中值 t(Ma) (±1σ)	组合 t(Ma) (±1σ)	L(μm) (N)
1	ZK1206-31 硅化黄铁矿化闪长岩	35	0.309 (64)	8.476 (1 758)	7.428 (5 949)	98.2	5.3±1	5.3±1	13.1±1.8 (63)
2	NZ15-3-2 褐铁矿化闪长岩	35	1.042 (295)	26.66 (7 545)	7.672 (5 949)	19.5	5.9±0.5	5.9±0.4	13.5±2.2 (82)

下载: 导出CSV

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