Porphyry Cu-Au-Mo Deposits: Exploration, Resource Assessment, and Critical Mineral Potential of Ore and Waste

A special issue of Minerals (ISSN 2075-163X). This special issue belongs to the section "Mineral Deposits".

Deadline for manuscript submissions: closed (22 April 2022) | Viewed by 9032

Special Issue Editors


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Guest Editor
US Geology Survey, Natl Ctr 954, Reston, VA 20192, USA
Interests: mineral resource assessment; porphyry Cu-Au-Mo deposits; critical minerals

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Guest Editor
W.H.Bryan Mining and Geology Research Centre, Sustainable Minerals Institute, University of Queensland, 40 Isles Road, Indooroopilly, Brisbane, QLD 4068, Australia
Interests: geometallurgical and geoenvironmental characterisation; tailings characterisation and reprocessing; acid mine drainage; mine waste characterisation and repurposing
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W.H.Bryan Mining & Geology Research Centre, Sustainable Minerals Institute, University of Queensland, 40 Isles Road, Indooroopilly, Brisbane, QLD 4068, Australia
Interests: mineral deposit systems and exploration; total/ore deposit knowledge, geometallurgical and geoenvironmental characterisation
Special Issues, Collections and Topics in MDPI journals

Special Issue Information

Dear Colleagues,

Porphyry deposits represent significant resources of copper, gold, and molybdenum, and are viewed as critical exploration targets for low-grade, high-tonnage mining operations. Advanced exploration tools including remote sensing and geophysical techniques for exploring under cover provide key information for prospect targeting and mineral resource assessment. Mineral prospectivity mapping requires identification, compilation, and application of mappable criteria as evidence for porphyry system components. Although some porphyry deposits have produced by-product critical minerals such as Re, Te, and PGMs, these are typically not reported or recovered. Available data on the nature and distribution of critical minerals in porphyry ores and tailings are scarce. The high tonnages of porphyry deposits generate huge volumes of waste rock and tailings. Consequently, characterisation and reprocessing of existing surface waste materials at active and inactive mines have the potential to transform waste into a resource by providing new sources of critical metals and facilitating rehabilitation. Future metal supply will require advanced strategies for discovery along with sampling, characterisation and ore sorting technologies for surface wastes. For this Special Issue, we welcome studies that contribute to all these aspects of porphyry deposits, including reviews of critical mineral potential of porphyry ore and waste and processing technologies.  

Mrs. Jane M. Hammarstrom
Dr. Anita Parbhakar-Fox
Dr. Nathan Fox
Guest Editors

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Keywords

  • porphyry Cu-Au-Mo deposits
  • mineral exploration
  • mineral resource assessment
  • critical mineral
  • critical metals
  • waste as a resource
  • environmental characterisation
  • ore sorting

Published Papers (2 papers)

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Research

16 pages, 23374 KiB  
Article
Porphyry Copper: Revisiting Mineral Resource Assessment Predictions for the Andes
by Jane Marie Hammarstrom
Minerals 2022, 12(7), 856; https://0-doi-org.brum.beds.ac.uk/10.3390/min12070856 - 04 Jul 2022
Cited by 3 | Viewed by 4905
Abstract
A mineral resource assessment of porphyry copper deposits in the Andes Mountains of South America was done in 2005 in cooperation with geological surveys in South America. The study identified 590 million metric tons (Mt) of copper in identified resources. Continued exploration and [...] Read more.
A mineral resource assessment of porphyry copper deposits in the Andes Mountains of South America was done in 2005 in cooperation with geological surveys in South America. The study identified 590 million metric tons (Mt) of copper in identified resources. Continued exploration and development in the region over a 15-year period provide an opportunity to compare the predicted assessment results with new discoveries and resource growth in previously known deposits. The 2005 assessment estimated that 145 undiscovered deposits could contain a mean of 750 Mt of copper. The actual number of deposits increased (2005 to 2020) from 69 to 120 and the amount of identified copper resources increased from 590 Mt to 1600 Mt. Although most of the new deposits and copper resources are concentrated in Miocene-Pliocene and Eocene-Oligocene mineral belts, new deposits have been discovered in Jurassic and Cretaceous mineral belts. Resource growth in porphyry copper deposits known in the Andes in 2005 (1100 Mt copper) exceeds copper resources in new discoveries since 2005 (490 Mt copper) by a factor of 2. Full article
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22 pages, 5920 KiB  
Article
Rock-Forming (Biotite and Plagioclase) and Accessory (Zircon) Minerals Geochemistry as an Indicator of the Metal Fertility of Magmas by the Example of Au-Cu-Fe-Skarn Deposits in Eastern Transbaikalia
by Yury O. Redin, Anna A. Redina, Viktor P. Mokrushnikov, Alexandra V. Malyutina and Vladislav F. Dultsev
Minerals 2022, 12(1), 50; https://0-doi-org.brum.beds.ac.uk/10.3390/min12010050 - 30 Dec 2021
Cited by 2 | Viewed by 2098
Abstract
Many gold and gold-bearing complex deposits related to the Late Jurassic and Early Cretaceous magmatism are known in Eastern Transbaikalia. The largest deposits are the Lugokan, the Kultuma and the Bystrinsky. These deposits are in a paragenetic relationship with the Late Jurassic magmatic [...] Read more.
Many gold and gold-bearing complex deposits related to the Late Jurassic and Early Cretaceous magmatism are known in Eastern Transbaikalia. The largest deposits are the Lugokan, the Kultuma and the Bystrinsky. These deposits are in a paragenetic relationship with the Late Jurassic magmatic rocks of the Shakhtama complex. According to the available data, the total resources of gold in these three deposits are estimated to be approximately 443 tons: the Lugokan, Au~53 tons, Cu~302 thousand tons; the Kultuma, Au~121 tons, Cu~587 thousand tons, Fe~33 mln t; the Bystrinsky, Au~269 tons, Cu~2070 thousand tons, Fe~67 mln t. One of the main aims of this work was to reveal the criteria of fertility for the classical porphyry type, based on the specific geochemical features of rock-forming and accessory minerals. A comparison of the obtained results with other data on the large porphyry and skarn deposits of the world showed that the magmatic rocks of the Bystrinsky massif, specifically porphyry species dated 159.6–158.6 Ma, are potentially ore-bearing for the porphyry type mineralization. The magmatic rocks that widely occur at the Lugokan and Kultuma deposits are most close to the Fe-skarn deposits. The best indicators of the magma fertility for the porphyry rocks are Ce/Ce*, Eu/Eu*, Yb/Dy, (Ce/Nd)/Y in zircons. Thus, magmatic rocks characterized by Ce/Ce* > 100, Eu/Eu* > 0.4, Yb/Dy > 5.0 and (Ce/Nd)/Y > 0.01 may be classified as high fertile for the classical porphyry mineralization in Eastern Transbaikalia. The plagioclase and biotite chemistry data also showed that the magmatic rocks that occurred at the Bystrinsky deposit are the most fertile for the porphyry type mineralization. The magmatic rocks classified as ore-bearing porphyry type have Al* > 1 in plagioclase, high values of IV(F) and IV(F/Cl) and low ratios of X(F)/X(OH) in biotites. The assessment of the metal fertility of magmatic rocks is most effective in combination with data on both the composition of rock-forming and accessory minerals. The obtained data may be used to develop the methods of prediction and search for gold, copper and iron mineralization. Full article
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