T176 Science and Technology Advancement in Responsible Mining of Critical Minerals from Primary and Secondary Resources (Posters)
Tuesday, 24 September 2024
8:00 AM - 5:30 PM
Hall D
POTENTIAL CRITICAL MINERAL AND BASE METAL RESOURCES IN NON-FUEL MINE WASTE FEATURES IN THE FOUR CORNERS REGION, USA
Paper number: T176-7
Program: Technical Sessions
Time: 8:00 AM – 5:30 PM
Authors
-
Nicholas A. KarlGeology, Geophysics, and Geochemistry Science Center, Denver, CO
-
Autumn HelfrichGeology, Geophysics, and Geochemistry Science Center, Denver, CO
-
Andrew SmithGeology, Geophysics, and Geochemistry Science Center, Denver, CO
-
Jeffrey MaukGeology, Geophysics, and Geochemistry Science Center, Denver, CO
Abstract
We use approximate values to estimate the endowment of commodities in these combined porphyry Cu waste features. Assuming an average waste density of 1.8 t/m3 yields approximately 31 Gt of porphyry Cu mine waste, approximately 60% of which are stockpiles and tailings. Compiling grades in the region suggests that ore may have initially contained approximately 0.56 ± 0.16% Cu, 0.02 ± 0.01% Mo, 0.1 ± 0.05 g/t In and 1.01 ± 0.62 g/t Re, based on variations in available assay data. We estimate initial extraction efficiencies of 85 ± 10% for Cu and 30 ± 5% for other metals of interest for the materials from stockpiles and tailings and estimate the remaining waste rock nominally contains 5% of these materials. Therefore, we estimate the combined porphyry Cu waste features may contain approximately 19 ± 5.9 Mt Cu, 2.7 ± 1.4 Mt Mo, 1.3 ± 0.66 kt In and 13 ± 8.1 kt Re. This endowment is hypothetical, underscoring the need for detailed characterization of mine waste. However, the Cu endowment is approximately equivalent to the endowment of a giant to supergiant Cu deposit, which are the largest 1-10% of Cu deposits on Earth. These data suggest that reprocessing mine waste may help provide base and critical minerals to support the renewable energy transition.
Geological Society of America Abstracts with Programs. Vol. 56, No. 5
doi: 10.1130/abs/2024AM-404148
© Copyright 2024 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.