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Deciphering the origin of low-grade W mineralization and hydrothermal fluids in the oxidized Fujiashan W skarn deposit using garnet geochemistry
Lithium: critical, or not so critical?
The New Century for Nickel Resources, Reserves, and Mining: Reassessing the Sustainability of the Devil’s Metal
THE IMPORTANCE OF GEOLOGY IN ASSESSING BY- AND COPRODUCT METAL SUPPLY POTENTIAL; A CASE STUDY OF ANTIMONY, BISMUTH, SELENIUM, AND TELLURIUM WITHIN THE COPPER PRODUCTION STREAM
Battery and Energy Metals: Future Drivers of the Minerals Industry?
Geology and Mining: Mineral Resources and Reserves: Their Estimation, Use, and Abuse
3D Numerical Simulation-Based Targeting of Skarn Type Mineralization within the Xuancheng-Magushan Orefield, Middle-Lower Yangtze Metallogenic Belt, China
COVID-19 and the Global Mining Industry
Minerals and Allied Natural Resources and Their Sustainable Development: Principles, Perspectives with Emphasis on the Indian Scenario (M. Deb and S.C. Sarkar)
Growing Global Copper Resources, Reserves and Production: Discovery Is Not the Only Control on Supply
Abstract The critical metals are vital to modern life due to their use in a variety of domestic, green, and military high technology applications but have supplies that are inherently insecure. This study provides an overview of the concept of criticality as applied to the critical metals and outlines key issues around the resources and future supply of these metals. The methods used to quantify the criticality of critical metals have advanced over time, demonstrating that some metals are more strategically important than others, depending on the viewpoint of the organization considering criticality. However, global resources and reserves of a number of critical metals as well as their production statistics remain unclear. Methods exist to quantify the resources of critical metals with reasonable accuracy but these methods rely on information provided by the mining industry, indicating that better reporting practices would improve our knowledge of the global resources and cycling of these key commodities. Criticality can also be addressed in numerous ways, including the analysis of known mine supply chains to enable the economic extraction of critical metal by-products, the determination of the critical metal prospectivity of mining/mineral processing wastes (given a significant amount of critical metals currently deport to waste), increased amounts of recycling intermediates or end-use products containing critical metals, and the discovery of new and economic deposits of the critical metals. However, all of these approaches and the associated policy around them require more information in terms of mineral resource accounting, mineral economics, material flow analysis, mineral processing, as well as increased economic geology knowledge that would enable the making of future discoveries and increase the likelihood of critical metals being extracted as either primary or by-products. Without this information, significant parts of our knowledge base on the supply (and the security of this supply) of the critical metals will remain opaque.
Singularity mapping of fracture fills and its relationship to deep concealed orebodies – a case study of the Shaxi porphyry Cu-Au deposit, China
West Africa: The World’s Premier Paleoproterozoic Gold Province
Acceptance of the SEG Waldemar Lindgren Award for 2014
A Detailed Assessment of Global Rare Earth Element Resources: Opportunities and Challenges
A Detailed Assessment of Global Nickel Resource Trends and Endowments
Geochemistry of the 130 to 80 Ma Canadian High Arctic Large Igneous Province (HALIP) Event and Implications for Ni-Cu-PGE Prospectivity
A Detailed Assessment of Global Cu Resource Trends and Endowments
HIDDEN MINERAL DEPOSITS IN Cu-DOMINATED PORPHYRY-SKARN SYSTEMS: HOW RESOURCE REPORTING CAN OCCLUDE IMPORTANT MINERALIZATION TYPES WITHIN MINING CAMPS
Large Igneous Provinces (LIPs) and Metallogeny
Abstract Large igneous provinces (LIPs) represent significant reservoirs of energy and metals that can either drive or contribute to a variety of metallogenic systems. The relationships between LIPs and these various systems can be divided into four distinct although partially overlapping classifications: (1) LIPs form the primary source of commodities within mineral deposits (e.g., orthomagmatic Ni-Cu-PGE sulfides, or Nb-Ta-REE and diamonds for often LIP-related carbonatites and kimberlites, respectively); (2) LIPs either provide the energy to drive hydrothermal systems or can act as source rocks for hydrothermal ore deposits (e.g., volcanogenic massive sulfide (VMS) deposits)—in some cases LIP rocks can also act as barriers to fluid flow and/or reaction zones causing mineralization (e.g., orogenic Au); (3) weathering can concentrate elements such as Al and Ni-Co within laterites that develop from exposed LIP mafic-ultramafic rocks in tropical climates, and for Nb, Ta, and REE in laterites from associated carbonatites; and (4) indirect links exist between LIPs and ore deposits; here we consider two of these types of links, the first of which involves LIP events that are linked to attempted or successful continental breakup where the LIP barcode record can be used as a correlation tool for reconstructing Precambrian supercontinents and therefore enable the tracing of metallogenic belts between presently separated, but formerly contiguous crustal blocks. A second, more speculative, indirect link is provided by the fact that major continental breakup (linked to LIPs) is associated with distal compression and transpression in the plate tectonic circuit (and the formation of orogenic deposits, such as Au). We discuss the role of LIPs (be it major or contributory) in each of these classifications for the generation of this wide variety of differing mineral deposit types and potential implications of this link between LIPs and metallogenesis for exploration strategies. This review shows how our understanding of LIPs, and the processes that affect LIP magmas and rocks, have direct consequences for mineral exploration and economic geology.