Geochronology and Ore Genesis of the Niujuan-Yingfang Pb-Zn-Ag Deposit in Fengning, Northern North China Craton: Constraints from Fluid Inclusions, H-O-S Isotopes and Fluorite Sr-Nd Isotopes

Xiang Yan; Bin Chen; Xiaoxia Duan; Zhiqiang Wang

doi:10.1007/s12583-020-1393-8

Volume 32 Issue 1

Mar 2021

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Journal of Earth Science > 2021 > 32(1): 81-102.

Xiang Yan, Bin Chen, Xiaoxia Duan, Zhiqiang Wang. Geochronology and Ore Genesis of the Niujuan-Yingfang Pb-Zn-Ag Deposit in Fengning, Northern North China Craton: Constraints from Fluid Inclusions, H-O-S Isotopes and Fluorite Sr-Nd Isotopes. Journal of Earth Science, 2021, 32(1): 81-102. doi: 10.1007/s12583-020-1393-8

Citation:

Xiang Yan, Bin Chen, Xiaoxia Duan, Zhiqiang Wang. Geochronology and Ore Genesis of the Niujuan-Yingfang Pb-Zn-Ag Deposit in Fengning, Northern North China Craton: Constraints from Fluid Inclusions, H-O-S Isotopes and Fluorite Sr-Nd Isotopes. Journal of Earth Science, 2021, 32(1): 81-102. doi: 10.1007/s12583-020-1393-8

Citation:

Xiang Yan, Bin Chen, Xiaoxia Duan, Zhiqiang Wang. Geochronology and Ore Genesis of the Niujuan-Yingfang Pb-Zn-Ag Deposit in Fengning, Northern North China Craton: Constraints from Fluid Inclusions, H-O-S Isotopes and Fluorite Sr-Nd Isotopes. Journal of Earth Science, 2021, 32(1): 81-102. doi: 10.1007/s12583-020-1393-8

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Geochronology and Ore Genesis of the Niujuan-Yingfang Pb-Zn-Ag Deposit in Fengning, Northern North China Craton: Constraints from Fluid Inclusions, H-O-S Isotopes and Fluorite Sr-Nd Isotopes

doi: 10.1007/s12583-020-1393-8

Xiang Yan^{1, 2
,},
Bin Chen^{3
,
,
,},
Xiaoxia Duan^{1, 2},
Zhiqiang Wang^{1, 2}

1.
School of Resources and Environmental Engineering, Hefei University of Technology, Hefei 230009, China
2.
Ore Deposit and Exploration Centre(ODEC), Hefei University of Technology, Hefei 230009, China
3.
Department of Earth and Space Sciences, Southern University of Science and Technology, Shenzhen 518055, China

More Information

Corresponding author: Bin Chen, chenb6@sustech.edu.cn
Received Date: 21 Sep 2020
Accepted Date: 16 Dec 2020
Publish Date: 01 Feb 2021

Abstract

Abstract

The Niujuan-Yingfang Pb-Zn-Ag deposit in northern North China Craton (NCC) is hosted at the contact zone between Permian biotite monzogranite and Hongqiyingzi Group migmatitic gneiss. The orebodies are structurally controlled by NE-trending F₁ fault. Mineralization can be divided into three stages: (1) siliceous-chlorite-pyrite stage, (2) quartz-Ag-base metal stage, and (3) fluorite-calcite stage. Four types of fluid inclusions were identified, including: (1) liquid-rich aqueous inclusions, (2) vapor-rich inclusions, (3) liquid-rich, solid-bearing inclusions, and (4) CO₂-bearing inclusions. Microthermometric measurements reveal that from stage Ⅰ to Ⅲ, the homogenization temperatures range from 317 to 262 ℃, from 297 to 192 ℃, and from 248 to 151 ℃, respectively, and the fluid salinities are in the ranges from 1.1 wt.% to 6.5 wt.%, 1.2 wt.% to 6.0 wt.% and 0.7 wt.% to 4.0 wt.% NaCl equivalents, respectively. Fluid boiling and cooling are the two important mechanisms for ore precipitation according to microthermometric data, and fluid-rock interaction is also indispensable. Laser Raman spectroscopic analyses indicate the fluid system of the deposit is composed of CO₂-NaCl-H₂O±N₂. Metallogenic fluorites yielded a Sm-Nd isochron age of 158±35 Ma. The δ³⁴S_V-CDT values of sulfides range from -1.3‰ to 6.3‰, suggesting that the sulfur may be inherited from the basement metamorphic igneous rocks. Hydrogen and oxygen isotopic compositions of quartz indicate a metamorphic origin for the ore-forming fluid, and the proportion of meteoric water increased during the ore-forming processes. Sr-Nd isotopes of fluorites show a crustal source for the ore-forming fluid, with primary metamorphic fluid mixed with meteoric water during ascent to lower crustal levels. Combined with the geological, metallogenic epoch, fluid inclusions, H-O-S and Sr-Nd isotopes characteristics of the deposit, we suggest that the Niujuan-Yingfang deposit belongs to the medium-low temperature hydrothermal vein-type Pb-Zn-Ag polymetallic deposit, with ore-forming fluids dominantly originated from metamorphic fluids.
- fluid inclusion,
- geochronology,
- H-O-S isotopes,
- fluorite Sr-Nd isotopes,
- Niujuan-Yingfang Pb-Zn-Ag deposit,
- NCC

Electronic Supplementary Material: Supplementary material (Table S1) is available in the online version of this article at https://doi.org/10.1007/s12583-020-1393-8.

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