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

Lead Research Organisation: Imperial College London
Department Name: Earth Science and Engineering

Abstract

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.

Planned Impact

We have taken an "embedded impact" approach with FAMOS. Stakeholders and beneficiaries have been involved with the development of the project from its initiation (including the initial Highlight Topic suggestion). The scientific content of the proposal was developed in discussion with representatives from industry, and the final consortium has assembled an Advisory Board that includes industry representatives so as to maintain two-way knowledge exchange and ensure development of impact. We have also engaged an international set of project partners (PP) who will extend the reach of our impact (see letters of support). The embedded impact will be delivered through various activities to support outreach, engagement and dissemination.

The key impact goal for FAMOS is to improve discovery rates of porphyry deposits by aiding exploration under cover, influencing decision making in the exploration process, reducing exploration risk and reducing the environmental impacts of drilling and associated disruptive fieldwork through more efficient prospectivity assessment.

There are four impact objectives within FAMOS:

1) A revised Mineral Systems model of porphyry deposit formation. This will lead to improved targeting at regional and igneous complex scales and better inputs to national strategies on mineral resources. Beneficiaries include PRIVATE SECTOR COMPANIES involved in mining, exploration and consultancy (e.g. PPs Anglo American, Rio Tinto, BHPBilliton, Freeport McMoRan), and NATIONAL AGENCIES charged with encouraging exploration and developing strategic resources (e.g. BGS and PP USGS).

2) New proxies for porphyry fertility. This will provide low-cost tools and approaches that will support improved decision-making during exploration. By using multiple proxies within a single sample, more data-rich exploration is possible, and in turn less sampling is required and less environmental impact is caused. Beneficiaries will include PRIVATE SECTOR COMPANIES involved in exploration, consultancy, and the provision of data and analytical equipment to industry (i.e. service companies, e.g. see PPs Olympus, Zeiss and SRK ES letters of support).

3) E-tech elements in porphyries. We will generate vital data for better global and national e-tech resource estimation. This facilitates improved targeting for specific e-techs during exploration, and improved metallurgical characterisation of them. Beneficiaries will be GOVERNMENT AGENCIES who advise on resource strategy (e.g. BGS, PP USGS), and POLICY MAKERS IN GOVERNMENT planning future clean energy strategies. PRIVATE SECTOR COMPANIES exploring for resources (see PP Anglo American letter of support) and end-users of e-techs will benefit through improved strategic knowledge of future supplies and the WIDER PUBLIC will gain through support of sustainable environmental technologies for a low-carbon society.

4) Outreach, education and training. We have planned activities to increase public understanding of resource issues (discovery, depletion, environmental and social impacts, the 'e-tech' concept), particularly through NHM outreach, and activities to encourage the uptake of the new model and proxies with professional geoscientists through training workshops, short courses and engagement at high profile conferences. Beneficiaries include the WIDER PUBLIC, PRIVATE SECTOR COMPANIES as publicly traded bodies and employers of skilled professionals and PROFESSIONAL BODIES such as the IOM3 and Mineral Deposits Studies Group (see letter of support) who support training and professional development for their members.
 
Description The formation, storage and chemical differentiation of magma in the Earth's crust is of fundamental importance in igneous geology and volcanology. Recent data are challenging the high melt fraction 'magma chamber' paradigm that has underpinned models of crustal magmatism for over a century, suggesting instead that magma is normally stored in low melt fraction 'mush reservoirs'. A mush reservoir comprises a porous and permeable framework of closely packed crystals with melt present in the pore space. However, many common features of crustal magmatism have not yet been explained by either the 'chamber' or 'mush' reservoir concepts. We have shown that reactive melt flow is a critical, but hitherto neglected, process in crustal mush reservoirs. Reactive flow occurs because buoyant melt percolates upwards through, and reacts with, the crystals: transport of chemical components with the melt modifies the local bulk composition, and chemical reaction occurs to maintain local thermodynamic equilibrium. We have shown that reactive flow in mid- to lower crustal mush reservoirs can produce the low crystallinity, chemically differentiated (silicic) magmas which ascend to form shallower intrusions or erupt to the surface. Reactive flow can accumulate silicic magmas containing much older crystals, creating the age disparity recorded in many crustal magmatic systems. Older crystals are stored at low and even sub-solidus temperatures before being remobilized by the rapid accumulation of melt, consistent with crystal chemistry data. Reactive melt flow can also produce the observed bimodality in magma compositions sourced from many mid- to lower-crustal reservoirs. Trace element profiles generated by reactive flow are similar to those observed in a well-studied reservoir now exposed at the surface. We have shown that magma storage and differentiation primarily occurs by reactive melt flow in long-lived mush reservoirs, rather than by the commonly invoked process of fractional crystallisation in magma chambers.
Exploitation Route These results can be used to update textbooks and popular science books and articles that ubiquitously and incorrectly portray magma reservoirs as large holes in the ground filled with molten rock.
Sectors Education

URL http://www.imperial.ac.uk/earth-science/research/research-groups/norms/
 
Description Fluid dynamical controls on high-grade hypogene porphyry deposits
Amount £275,000 (GBP)
Organisation BHP 
Sector Private
Country Canada
Start 01/2022 
End 12/2023
 
Description Funding for PhD student Catherine Booth at Imperial College
Amount £96,292 (GBP)
Organisation Engineering and Physical Sciences Research Council (EPSRC) 
Sector Public
Country United Kingdom
Start 10/2018 
End 03/2022
 
Description Sustainable exploration for orthomagmatic (critical) raw materials in the EU: Charting the road to the green energy transition
Amount € 6,672,184 (EUR)
Funding ID 101057741 
Organisation European Commission 
Sector Public
Country European Union (EU)
Start 06/2022 
End 05/2025
 
Description @NORMS_IC Twitter account 
Form Of Engagement Activity Engagement focused website, blog or social media channel
Part Of Official Scheme? No
Geographic Reach International
Primary Audience Postgraduate students
Results and Impact NORMS Twitter account promotes and publicizes activities of group
Year(s) Of Engagement Activity 2018,2019,2020,2021,2022,2023
 
Description Co-edited Futurum (online outreach resource for young people) 
Form Of Engagement Activity A magazine, newsletter or online publication
Part Of Official Scheme? No
Geographic Reach International
Primary Audience Schools
Results and Impact Jamie Wilkinson, Jon Blundy, Matt Jackson and Dan Smith co-edited an article on FAMOS-related research for Futurum which produces online and print articles and outreach resources to encourage young people into STEM/STEMM/STEAM subjects.
Year(s) Of Engagement Activity 2020
URL https://futurumcareers.com/magma-detectives-studying-volcanic-arcs-to-find-valuable-minerals-in-eart...
 
Description Development of Twitter account @FAMOS_ores 
Form Of Engagement Activity Engagement focused website, blog or social media channel
Part Of Official Scheme? No
Geographic Reach International
Primary Audience Study participants or study members
Results and Impact Development of Twitter account @FAMOS_ores including information on project outputs, conference participation and project updates
Year(s) Of Engagement Activity 2018