Silver deposits, melt-inclusions, isotopes, and thermobarometry

拟议的研究计划的目的是发展如何银是形成，运输，分区，并在各种热液环境沉淀的增强理解。本文通过一系列实验来验证：（1）低温银合金熔体的存在;（2）表面增强拉曼光谱（Sers）间接测量银熔体包裹体的熔融温度;（3）银同位素作为地质温度计和流体示踪剂的可行性。 我们要检验的第一个假设是，银、铋和其他金属是否可以在相对低温的盐水中作为熔体被活化。这将通过对银、铋和其他金属进行一系列活塞缸热液实验以及捕获合成熔体和流体包裹体来研究。第二项研究将测试的前提下，使用1010倍的信号强度增加的Sers，相对于标准的拉曼分析，作为一种间接的方法来确定熔融温度的拉曼惰性贵金属，如银和金的流体和熔融包裹体。将使用一些实验运行产品，沿着天然材料，研究107 Ag和109 Ag同位素的分配，以确定银同位素作为地质温度计的适用性。这项同位素研究将包括拟订一项从若干具有重要经济意义的含银矿物中提取银同位素的议定书。地质温度计的校准将根据天然和合成矿物对相对于一个充分表征的国际银同位素标准（NIST SRM 978 a）的分馏，通过高分辨率二次离子和多收集器电感耦合等离子体质谱法进行测量。 该研究计划建立在我在矿床，矿石岩石学，流体和熔体包裹体，同位素和实验工作方面的现有专业知识基础上，并继续与澳大利亚国立大学和澳大利亚地球科学研究人员的现有研究伙伴关系。我的研究团队将开发和利用新的研究工具和技术，以更好地表征压力，温度和流体成矿事件的时间，并推进我们对流体和金属熔体在银存款形成中的作用的理解。研究结果将有助于提高我们对地壳流体演化的认识，建立其与构造和成矿事件的关系，并加强银矿床的勘探模式。该研究计划还将培养下一代HQP在地球化学，矿床，流体包裹体和矿产勘探方面的技能。该计划将整合我们现有的行业合作伙伴关系，但也创造了新的机会，与行业合作，这将加强我们的研究，并为我的学生创造就业机会。

The objective of the proposed research program is to develop an enhanced understanding of how silver is speciated, transported, partitioned, and precipitated in a variety of hydrothermal environments. A series of experiments will be undertaken to test: 1) the existence of low-temperature silver-alloy melts; 2) the indirect measurement of melting temperatures of silver melt inclusions by Surface Enhanced Raman Spectroscopy (SERS); and 3) the feasibility of a using silver isotopes as a geothermometer and a fluid tracer. The first hypothesis we will test is whether silver, bismuth, and other metals can be mobilized as melts in relatively low temperature saline brines. This will be investigated via a series of piston cylinder hydrothermal experiments on silver, bismuth and other metals, and the trapping of synthetic melt and fluid inclusions. A second study will test the premise of using the 1010-fold signal strength increase of SERS, relative to standard Raman analysis, as an indirect method of determining melting temperatures of Raman inactive precious metals such as silver and gold in fluid and melt inclusions. Some of the experimental run products will be used, along with natural materials, to investigate the partitioning of 107Ag and 109Ag isotopes to determine the applicability of silver isotopes as a geothermometer. This isotope research will include the development of a protocol for silver isotope extraction from a number of economically important silver-bearing minerals. Calibration of the geothermometer will be based on the fractionation between naturally and synthetically produced mineral pairs relative to a well-characterized international silver isotope standard (NIST SRM978a), measured by high-resolution secondary ion and multi-collector inductively coupled plasma mass spectrometry. This research program builds upon my existing expertise in ore deposits, ore petrology, fluid and melt inclusions, isotopes, and experimental work and continues existing research partnerships with researchers from Australian National University and Geoscience Australia. My research team will develop and utilize new research tools and techniques to better characterize pressure, temperature, and timing of fluid mineralizing events, and advance our understanding of the role of fluid and metal melts in silver deposit formation. The results will help to improve our understanding of the evolution of the fluids in Earth's crust, establish their relationship to tectonic and mineralizing events and enhance exploration models for silver deposits. This research program will also train next generation HQP skilled in geochemistry, ore deposits, fluid inclusions, and mineral exploration. This program will integrate our existing industry partnerships, but also create new opportunities to collaborate with industry that will enhance our research and create career opportunities for my students.