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From arc magmas to ores (FAMOS): A mineral systems approach

从弧岩浆到矿石 (FAMOS)：矿物系统方法

基本信息

批准号：
NE/P017371/1
负责人：
Jonathan Blundy
金额：
$ 114.38万
依托单位：
University of Bristol
依托单位国家：
英国
项目类别：
Research Grant
财政年份：
2017
资助国家：
英国
起止时间：
2017 至无数据
项目状态：
已结题

来源：
https://gtr.ukri.org/projects?ref=NE%2FP017371%2F1
关键词：
arc magmas ores FAMOS mineral

项目摘要

Society is dependent on a reliable supply of metals and minerals for economic growth, improved standards of living, and development of infrastructure. Population growth means that even with increased recycling and resource efficiency, new mineral deposits still need to be discovered. The efficient exploration for, and discovery of, new resources requires new concepts and new tools. The Mineral Systems approach to exploration considers ore deposits on a lithospheric scale, in terms of the "ingredients", processes and environments that favour their formation. This approach amounts to a "source-pathway-trap" model, with an increased emphasis on predictive capacity, rather than just feature recognition. Historically, much research has focused on the trap, and characterisation of the ore deposits themselves; here we aim to focus deeper in the system by integrating ore deposit formation with concepts of magmatism that arise from igneous petrology and volcanology. Therein lies a challenge because extant models for porphyry systems are increasingly at odds with magmatic models for crustal construction and arc volcanism. Rather than seeing magmatic systems in terms of large, liquid-rich magma chambers, emerging petrological models for crustal magmatism are turning instead to crystal-dominated, volatile-bearing "mushy" systems that traverse most or all of the crust. The dynamics of such systems have important consequences not just for arc magmatism, but also for the chemistry of the volatiles that are exsolved. These same volatiles fuel mineralisation and this is the synergy that we aim to exploit by assembling a multidisciplinary team of researchers from economic geology, igneous and metamorphic petrology, volcanology, geochemistry, numerical modelling and fluid dynamics. Our team embraces almost everyone currently engaged in porphyry mineralisation research in the UK and capitalises on strong existing links between UK ROs and the mining industry, many of who are Project Partners. The research will involve analysis of minerals from a wide variety of mineralised and barren settings using a wealth of modern analytical tools that enable determination of an extensive suite of trace elements and isotope tracers. As each trace element responds to magmatic processes in subtly different ways due to the affinity of different elements for different phases (minerals, melts and fluids), so the multi-element approach affords many advantages over conventional proxies in which the full potential of the Periodic Table is not exploited. The analysis of natural systems will be underpinned by high pressure and temperature experiments to establish the phase relationships of ascending arc magmas and the partition coefficients that capture the affinities of elements for certain phases. As fluid accumulation and migration is an essential, but poorly understood, final step in ore deposit formation, we will develop, in tandem with the geochemistry, numerical models for fluid-bearing mushy systems. Finally, consideration will be given to critical metals that are passengers through the main ore-forming processes, but constitute important, often under-explored, by-products of porphyry mineralisation. The research proposed has a strong element of blue skies investigation, but a particular focus on outcomes that will benefit industry through improved exploration tools. Thus the project bridges the divide between academic and applied research in a way that is not normally possible through industry-funded projects. This bridging activity lies at the heart of the Highlight Topic call, specifically through the integration of new advances in the study of mineral systems, igneous petrology and geochemistry, with a view to identifying conditions that can act as pathfinders for new targets. A key outcome will be a range of trace element proxies that will enable the mining industry to establish the potential fertility of a magmatic arc on local to regional scales.

社会依赖于金属和矿物的可靠供应来促进经济增长、提高生活水平和发展基础设施。人口增长意味着，即使提高了回收利用和资源效率，仍需要发现新的矿藏。有效地勘探和发现新资源需要新的概念和新的工具。矿物系统勘探方法从有利于矿床形成的“成分”、过程和环境的角度考虑岩石圈范围内的矿床。这种方法相当于一个“来源-途径-陷阱”模型，更加强调预测能力，而不仅仅是特征识别。从历史上看，许多研究都集中在圈闭和矿床本身的特征上;在这里，我们的目标是通过整合矿石存款形成与岩浆作用的概念，从火成岩岩石学和火山学，更深入地关注系统。这是一个挑战，因为现存的斑岩系统模型与地壳构造和弧火山作用的岩浆模型越来越不一致。新兴的地壳岩浆作用岩石学模型不再把岩浆系统看作是大型的、富含液体的岩浆房，而是转向了以晶体为主的、含有挥发物的“糊状”系统，这些系统贯穿了大部分或全部地壳。这种系统的动力学不仅对弧岩浆作用有重要影响，而且对出溶的挥发物的化学性质也有重要影响。这些相同的挥发物燃料矿化，这是我们的目标是通过组装一个多学科的研究人员团队，从经济地质学，火成岩和变质岩石学，火山学，地球化学，数值模拟和流体动力学利用协同作用。我们的团队包括目前在英国从事斑岩矿化研究的几乎所有人，并利用英国RO与采矿业之间的强大联系，其中许多人是项目合作伙伴。该研究将涉及使用丰富的现代分析工具对各种矿化和贫瘠环境中的矿物进行分析，这些工具可以确定广泛的微量元素和同位素示踪剂。由于不同元素对不同相（矿物、熔体和流体）的亲和力，每种微量元素对岩浆过程的反应方式略有不同，因此多元素方法比传统的替代方法具有许多优势，因为传统的替代方法没有充分利用元素周期表的潜力。对自然系统的分析将以高压和高温实验为基础，以确定上升弧岩浆的相关系和反映元素对某些相的亲和性的分配系数。由于流体的聚集和迁移是矿石存款形成的一个基本的，但知之甚少，最后一步，我们将开发，与地球化学，含流体糊状系统的数值模型。最后，将考虑关键金属，这些金属是主要成矿过程的乘客，但构成了斑岩矿化的重要副产品，往往未被充分勘探。这项研究有很强的蓝天调查元素，但特别关注通过改进勘探工具使工业受益的结果。因此，该项目弥合了学术和应用研究之间的鸿沟，这种方式通常不可能通过工业资助的项目来实现。这种桥接活动是重点主题的核心，特别是通过整合矿物系统，火成岩学和地球化学研究的新进展，以确定可以作为新目标的探路者的条件。一个关键成果将是一系列微量元素替代物，使采矿业能够在地方到区域范围内确定岩浆弧的潜在肥力。