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首页|期刊导航|地质与勘探|胶东旧店金矿29号矿脉的成矿流体和成矿物质来源:基于流体包裹体以及H-O-S同位素的证据

胶东旧店金矿29号矿脉的成矿流体和成矿物质来源:基于流体包裹体以及H-O-S同位素的证据

刘欢 鲁浩 史猛 林大伟 尹升 张鲁涛 宋维雨

地质与勘探2025,Vol.61Issue(5):912-925,14.
地质与勘探2025,Vol.61Issue(5):912-925,14.DOI:10.12134/j.dzykt.2025.05.003

胶东旧店金矿29号矿脉的成矿流体和成矿物质来源:基于流体包裹体以及H-O-S同位素的证据

Ore-Forming Fluids and Sources of Materials in vein No.29 of the Jiudian Gold Deposit,Jiaodong Peninsula:Insights from Fluid Inclusions and H-O-S Isotope Analysis

刘欢 1鲁浩 1史猛 1林大伟 2尹升 1张鲁涛 2宋维雨3

作者信息

  • 1. 山东省第三地质矿产勘查院,山东 烟台 264004||烟台市深部金矿探测技术创新中心,山东 烟台 264004
  • 2. 山东省第三地质矿产勘查院,山东 烟台 264004
  • 3. 山东省鲁东地质工程有限公司,山东 烟台 264000
  • 折叠

摘要

Abstract

The Jiaodong Jiudian gold deposit is located in the southern of the Zhaopong fault zone and is a medium-sized gold deposit characterized by quartz vein-type mineralization.This study focused on the vein No.29 in the Jiudian gold deposit of the Jiaodong Peninsula.Fluid inclusion studies and H-O-S isotope analyses of quartz and pyrite from the ores were conducted to constrain the properties and origins of the ore-forming fluids.The results show that the fluid inclusions are predominantly two-phase aqueous(L-V),CO2-H2O three-phase,and minor pure CO2 single-phase types.The homogenization temperatures range from 193.4℃to 340.9℃,with a peak between 250℃and 290℃.The salinities(wt%Nacleqv)vary from 4.8%to 12.5%,indicative of a moderate-temperature,moderate-low salinity,and CO2-rich fluid system.The δ18OV-SMOW values of quartz range from 11.6‰ to 12.4‰,and δDV-SMOW values vary from-83.0‰ to-76.4‰.The calculated δ18OH2O values of the fluid range from 3.5‰ to 4.3‰.The δ34S values of pyrite range from 7.6‰ to 8.5‰,with an average of 8.1‰.These isotopic features suggest a magmatic-hydrothermal origin with contributions from crustal fluids and meteoric water during fluid migration.Combined with previous studies,fluid immiscibility is considered the key mechanism for gold precipitation.The mineralization was facilitated by thermal upwelling-extensional structures related to the subduction and rollback of the Pacific Plate during the Mesozoic.

关键词

旧店金矿床/29号脉/成矿流体/成矿物质/流体包裹体/H-O-S同位素/胶东地区

Key words

Jiudian gold deposit/vein No.29/ore-forming fluids/ore-forming materials/fluid inclusions/H-O-S isotopes/Jiaodong Peninsula

分类

天文与地球科学

引用本文复制引用

刘欢,鲁浩,史猛,林大伟,尹升,张鲁涛,宋维雨..胶东旧店金矿29号矿脉的成矿流体和成矿物质来源:基于流体包裹体以及H-O-S同位素的证据[J].地质与勘探,2025,61(5):912-925,14.

基金项目

山东省自然科学基金(编号:ZR2022QD060)、新一轮找矿突破战略行动科技支撑项目(编号:ZKKJ202406)、山东省省级地质勘查项目(编号:鲁勘字(2024)71号)和2024年乳山市金矿资源勘查项目(编号:SDGP371083000202402000014)联合资助. (编号:ZR2022QD060)

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