Collaborative Research on Fluid Pathways, and Metal Transport and Deposition in Carlin-Type Gold Deposits: Insights From the Getchell System

卡林型金矿中流体路径、金属迁移和沉积的合作研究：来自 Getchell 系统的见解

• 批准号: 0635658
• 负责人: Jean Cline
• 金额: $ 29.59万
• 依托单位: University of Nevada Las Vegas
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2007
• 资助国家: 美国
• 起止时间: 2007-02-15 至 2011-01-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0635658&HistoricalAwards=false
• 关键词: Collaborative; Research; Fluid; Pathways; Metal

This collaborative study by researchers at the University of Nevada Las Vegas and the University of Nevada Reno aims to develop a time-space geological and geochemical framework of the classic Carlin-type gold deposits of the Getchell district in northern Nevada by utilizing data from more than 12,000 holes drilled by mining companies and sophisticated 3D modeling software to identify samples for state-of-the art in situ micro analytical techniques. With the drill holes and modeling software we will build a comprehensive 3-dimensional model from which we will interpret fluid pathways taken by the gold-bearing hydrothermal fluids. We will then add the fourth dimension, time, to the model by integrating detailed micro analytical studies of various stages of quartz, pyrite, and other sulfide minerals at locations along interpreted fluid pathways. Specifically, the investigators will document how the textures and isotopic and trace element compositions of quartz and pyrite vary with time and at any given point in space, using cathodoluminescence, electron microprobe chemical analyses, laser ablation ICP-MS chemical analyses, and in situ ion probe isotope analyses. The isotopic and trace element composition of the quartz and pyrite are essentially fingerprints of the hydrothermal fluid and analyses of various minerals will allow better tracking of the passage and evolution of the ore fluid. By comparing these "fingerprints" in different samples from different locations along fluid pathways it will be possible to deduce how the composition of the hydrothermal fluid, which formed the gold-bearing pyrite and quartz, varied both in time and space. It is also planned to study samples of the hydrothermal fluid trapped as fluid inclusions in the quartz to deduce how temperatures and compositions of the ore-forming fluid varied in time and space along fluid pathways. From these data the investigators will be able to constrain depositional mechanisms in high-grade portions of the ore bodies by identifying how fluids physically and chemically evolved as they traveled into, through, and out of high-grade ore zones. Carlin-type gold deposits in Nevada account for about 8% of the annual worldwide gold production, making the United States the second largest gold producer in the world. Despite their importance, several aspects of their origin remain enigmatic. The results of this research will not only lead to better understanding of the origin of Carlin-type deposits, but will also lend insights into broader earth processes. This project will advance our understanding of hydrology and mass transfer involved with hydrothermal circulation in upper crustal rocks that were being heated and extended. Important new knowledge will be generated through a research partnership between the mining industry, Nevada's second most important industry, and the researchers, including a post doctoral fellow and graduate and undergraduate students. This knowledge will improve exploration for similar gold deposits in Nevada and other parts of the world. Project results will also contribute to mineral potential assessment by government agencies and mining companies, and improved land use decisions by government agencies.

内华达大学拉斯维加斯分校和内华达大学里诺分校的研究人员进行了这项合作研究，旨在利用采矿公司钻探的12,000多个孔的数据和复杂的3D建模软件，为最先进的原位微分析技术识别样品，开发内华达州北部盖切尔地区经典卡林型金矿的时空地质和地球化学框架。利用钻孔和建模软件，我们将建立一个全面的三维模型，从中我们将解释含金热液流体的流体路径。然后，我们将通过整合沿解释流体路径位置的石英、黄铁矿和其他硫化物矿物的不同阶段的详细微观分析研究，将第四个维度（时间）添加到模型中。具体来说，研究人员将利用阴极发光、电子微探针化学分析、激光烧蚀ICP-MS化学分析和原位离子探针同位素分析，记录石英和黄铁矿的结构、同位素和微量元素组成如何随时间和在任何给定的空间点变化。石英和黄铁矿的同位素和微量元素组成是热液流体的指纹，对各种矿物的分析可以更好地跟踪矿液的通道和演化。通过比较这些“指纹”在流体路径上不同地点的不同样品，将有可能推断出形成含金黄铁矿和石英的热液流体的成分是如何在时间和空间上变化的。还计划研究作为流体包裹体的热液流体在石英中的样品，以推断成矿流体的温度和成分如何沿着流体路径随时间和空间变化。根据这些数据，研究人员将能够通过确定流体在进入、穿过和离开高品位矿体带时的物理和化学演化过程，来限制矿体高品位部分的沉积机制。内华达州卡林型金矿约占世界黄金年产量的8%，使美国成为世界第二大黄金生产国。尽管它们很重要，但它们起源的几个方面仍然是个谜。这项研究的结果不仅将有助于更好地了解卡林型矿床的起源，而且还将为更广泛的地球过程提供见解。该项目将促进我们对上地壳岩石热液循环的水文和传质过程的理解。重要的新知识将通过内华达州第二大产业采矿业与研究人员（包括博士后研究员、研究生和本科生）之间的研究伙伴关系产生。这一发现将改善内华达州和世界其他地区类似金矿的勘探工作。项目结果也将有助于政府机构和矿业公司评估矿物潜力，并有助于政府机构改进土地使用决定。