TY - JOUR
T1 - Understanding rare earth elements in heavy mineral sand systems
AU - Morin-Ka, Sidy
AU - Gonzalez-Alvarez, Ignacio
AU - Duuring, Paul
AU - Gonzalez, Christopher M.
PY - 2025/3/12
Y1 - 2025/3/12
N2 - Heavy mineral sands (HMS) represent an alternative major resource of Rare Earth Elements (REE) deposits with over 90 % of these formed within the past 66 Myr. These deposits exhibit a diverse range of mineral compositions (i.e. ilmenite, rutile, zircon, monazite, xenotime, and garnet) and can be formed from a wide range of geological and surficial processes. However, few studies examined the in-depth geological characteristics and exploration strategies to specifically target HMS mineralisation, and particularly none have specifically focussed on the REE component of these deposits. Here we show a total of 1173 REE-HMS deposits that exhibit diverse heavy mineral compositions. The largest REE-HMS deposits show an average heavy mineral grade of 7 % (SD = 12) and an average resource size of 1337 Mt. (SD = 1932). REE-HMS deposits commonly concentrate along Quaternary coastlines that cluster within a 100 km radius and predominate in tropical humid areas within 25 degrees north and south of the Equator. Yet, 40 % of large REE-HMS deposits formed during the Neogene, Paleogene, and Cretaceous situated inland from modern coastlines. Another feature of REE-HMS clusters shows that coastal areas that are protected from major global oceanic currents show a higher prevalence than regions that remain unprotected. REE-HMS deposits originate from rocks found in high-grade metamorphic belts, orogenic belts, and cratons, transported by wind and well-developed river systems, particularly in tropical and humid climates. This study highlights the importance of geological, climatic, and surface process factors in shaping the distribution of REE-HMS deposits. Furthermore, we also consider socioeconomic factors, such as land accessibility, politics, exploration maturity, and market demand playing crucial roles. A mineral exploration approach is proposed that emphasises the use of specific datasets and exploration methodologies tailored to the footprints of REE-HMS deposits. Overall, this study's findings contribute to a better understanding of REE-HMS deposits, providing insights for future exploration and resource management.
AB - Heavy mineral sands (HMS) represent an alternative major resource of Rare Earth Elements (REE) deposits with over 90 % of these formed within the past 66 Myr. These deposits exhibit a diverse range of mineral compositions (i.e. ilmenite, rutile, zircon, monazite, xenotime, and garnet) and can be formed from a wide range of geological and surficial processes. However, few studies examined the in-depth geological characteristics and exploration strategies to specifically target HMS mineralisation, and particularly none have specifically focussed on the REE component of these deposits. Here we show a total of 1173 REE-HMS deposits that exhibit diverse heavy mineral compositions. The largest REE-HMS deposits show an average heavy mineral grade of 7 % (SD = 12) and an average resource size of 1337 Mt. (SD = 1932). REE-HMS deposits commonly concentrate along Quaternary coastlines that cluster within a 100 km radius and predominate in tropical humid areas within 25 degrees north and south of the Equator. Yet, 40 % of large REE-HMS deposits formed during the Neogene, Paleogene, and Cretaceous situated inland from modern coastlines. Another feature of REE-HMS clusters shows that coastal areas that are protected from major global oceanic currents show a higher prevalence than regions that remain unprotected. REE-HMS deposits originate from rocks found in high-grade metamorphic belts, orogenic belts, and cratons, transported by wind and well-developed river systems, particularly in tropical and humid climates. This study highlights the importance of geological, climatic, and surface process factors in shaping the distribution of REE-HMS deposits. Furthermore, we also consider socioeconomic factors, such as land accessibility, politics, exploration maturity, and market demand playing crucial roles. A mineral exploration approach is proposed that emphasises the use of specific datasets and exploration methodologies tailored to the footprints of REE-HMS deposits. Overall, this study's findings contribute to a better understanding of REE-HMS deposits, providing insights for future exploration and resource management.
KW - Heavy mineral sands
KW - Mineral exploration
KW - Mineral systems
KW - REE targeting
KW - Rare earth elements
KW - Surface processes
UR - https://www.webofscience.com/api/gateway?GWVersion=2&SrcApp=uwapure5-25&SrcAuth=WosAPI&KeyUT=WOS:001446482700001&DestLinkType=FullRecord&DestApp=WOS_CPL
U2 - 10.1016/j.gexplo.2025.107705
DO - 10.1016/j.gexplo.2025.107705
M3 - Article
SN - 0375-6742
VL - 274
JO - Journal of Geochemical Exploration
JF - Journal of Geochemical Exploration
M1 - 107705
ER -