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Predictive Modeling of Reservoir Quality Associated with the Dissolution of K-Feldspar During Diagenesis: Lower Cretaceous, Scotian Basin, Canada -
Experimental Constraints on Baryte–Sulfide Ore in the Miocene Seawater-Dominated Mykonos Vein System, Cyclades -
Minor and Trace Elements in Copper Tailings: A Mineralogical and Geometallurgical Approach to Identify and Evaluate New Opportunities -
Petrophysical Characterisation and Suitability of Serpentinites from the Monteferrato Area (Tuscany, Italy) for Architectural Restoration -
Bacteria-like Ferruginous Structures in Carboniferous Limestones as Remains of Post-Variscan Hydrothermal Activity in Southern Poland
Journal Description
Minerals
Minerals
is an international, peer-reviewed, open access journal of natural mineral systems, mineral resources, mining, and mineral processing, and is published monthly online by MDPI.
- Open Access— free for readers, with article processing charges (APC) paid by authors or their institutions.
- High Visibility: indexed within Scopus, SCIE (Web of Science), GeoRef, CaPlus / SciFinder, Inspec, Astrophysics Data System, AGRIS, and other databases.
- Journal Rank: JCR - Q2 (Mining and Mineral Processing) / CiteScore - Q1 (Geology)
- Rapid Publication: manuscripts are peer-reviewed and a first decision is provided to authors approximately 17.7 days after submission; acceptance to publication is undertaken in 2.6 days (median values for papers published in this journal in the second half of 2025).
- Recognition of Reviewers: reviewers who provide timely, thorough peer-review reports receive vouchers entitling them to a discount on the APC of their next publication in any MDPI journal, in appreciation of the work done.
- Companion journal: Mining
- Journal Cluster of Geotechnical Engineering and Geology: Minerals, GeoHazards, Mining, Geotechnics, Glacies.
Impact Factor:
2.2 (2024);
5-Year Impact Factor:
2.5 (2024)
Latest Articles
A Review of Micro-Nanobubbles Applications in Fine-Grained Mineral Flotation
Minerals 2026, 16(3), 271; https://doi.org/10.3390/min16030271 (registering DOI) - 28 Feb 2026
Abstract
Micro-nanobubbles have emerged as a transformative technology in mineral flotation, offering superior performance in the recovery of fine-grained minerals. Conventional flotation processes often struggle with low recovery rates due to inefficient particle–bubble interactions and the formation of slimes, which increase pulp viscosity and
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Micro-nanobubbles have emerged as a transformative technology in mineral flotation, offering superior performance in the recovery of fine-grained minerals. Conventional flotation processes often struggle with low recovery rates due to inefficient particle–bubble interactions and the formation of slimes, which increase pulp viscosity and reduce selectivity. Micro-nanobubbles, characterized by their smaller size, larger specific surface area, and high stability, overcome these limitations by enhancing collision efficiency, promoting particle aggregation through the “bubble bridge” effect, and improving flotation recovery rates and concentrate quality. This review systematically examines the generation mechanisms of micro-nanobubbles, critically appraises their laboratory and industrial applications through specific case studies, and elucidates their fundamental roles in enhancing fine-grained mineral recovery by increasing collision-attachment efficiency and promoting hydrophobic aggregation. Additionally, the study highlights real-world application cases and discusses future directions for optimizing micro-nanobubbles flotation technology through equipment improvements, process integration, and synergies with emerging techniques. The findings underscore the potential of micro-nanobubbles to revolutionize mineral processing by increasing recovery efficiency, reducing reagent usage, and enhancing sustainability.
Full article
(This article belongs to the Special Issue Advances in Fine Particles and Bubbles Flotation, 2nd Edition)
Open AccessArticle
Effect of Sodium Carbonate on Phosphorus Reaction Behavior and Iron Mineral Transformation During Direct Reduction
by
Shichao Wu, Bo Li, Yonggang Wei, Haoyuan Xu and Tichang Sun
Minerals 2026, 16(3), 270; https://doi.org/10.3390/min16030270 (registering DOI) - 28 Feb 2026
Abstract
The coal-based direct reduction followed by magnetic separation (CDRMS) is an efficient iron extraction and dephosphorization process, which requires adding additives to improve the phosphorus removal rate. Compared with other additives, sodium carbonate has the advantages of good iron index, high phosphorus removal
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The coal-based direct reduction followed by magnetic separation (CDRMS) is an efficient iron extraction and dephosphorization process, which requires adding additives to improve the phosphorus removal rate. Compared with other additives, sodium carbonate has the advantages of good iron index, high phosphorus removal rate and less environmental pollution. Its role in phosphorus-rich oolitic iron ore (PROIO) where phosphorus exists in the form of apatite has been proved. However, the influence on the phosphorus transformation process in the lattice of iron minerals is not clear. In this paper, the effect of sodium carbonate on phosphorus removal in iron minerals and iron recovery during CDRMS was studied. Compared with not adding chemicals, the addition of sodium carbonate significantly reduced the phosphorus content of direct reduced iron (DRI) from 0.69% to 0.09%. The iron grade increased from 93.28% to 95.08%, and the iron recovery rate rose from 90.61% to 96.48%. The mechanism of sodium carbonate was revealed by using a synchronous thermal analyzer (TG–DSC), X-ray diffractometer (XRD), X-ray photoelectron spectrometer (XPS), scanning electron microscope and energy dispersive spectrometer (SEM–EDS), and vibrating sample magnetometer (VSM). The results show that sodium carbonate reacted with silicon and aluminum components to form nepheline, and the lattice substitution of phosphorus in iron minerals and silicon in nepheline prevents the reduction of phosphorus. In addition, sodium carbonate promotes the reduction of iron minerals, resulting in an increase in the magnetic properties of the reduction products.
Full article
(This article belongs to the Section Mineral Processing and Extractive Metallurgy)
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Open AccessArticle
Composition of Chlorite as a Proxy for Fluid Evolution and Gold Precipitation Mechanisms in the Jinshan Gold Deposit, Dexing District, South China
by
Danli Wang, Tao Zhang, Minjuan Zhou, Shaohao Zou, Xilian Chen, Deru Xu, Yongwen Zhang and Cui Yang
Minerals 2026, 16(3), 269; https://doi.org/10.3390/min16030269 (registering DOI) - 28 Feb 2026
Abstract
The physicochemical controls on gold precipitation in orogenic gold deposits remain poorly constrained, with traditional fluid inclusion and isotopic studies often yielding ambiguous results due to overprinting or incomplete records. This study addresses this challenge using chlorite—a sensitive mineral proxy for fluid conditions—as
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The physicochemical controls on gold precipitation in orogenic gold deposits remain poorly constrained, with traditional fluid inclusion and isotopic studies often yielding ambiguous results due to overprinting or incomplete records. This study addresses this challenge using chlorite—a sensitive mineral proxy for fluid conditions—as a quantitative sensor in the Jinshan orogenic gold deposit (>200 t Au) of the Jiangnan orogenic belt, South China. Hosted in Neoproterozoic phyllite within NE–NNE-trending ductile–brittle shear zones, Jinshan features auriferous quartz–polymetallic sulfide veins with prominent chlorite alteration. Integrating high-resolution SEM-EPMA analyses of multi-generational chlorite with thermodynamic modeling, we reconstruct the temporal evolution of temperature, oxygen fugacity (fO2), pH and sulfur fugacity (fS2) during ore formation. Four paragenetic stages are identified: Stage 1 (ankerite–quartz), Stage 2 (pyrite–arsenopyrite–quartz), Stage 3 (quartz–gold–polymetallic sulfide), and Stage 4 (chlorite–carbonate–quartz). Electron microprobe analysis reveals that the chlorite composition changes from Fe-rich chamosite (Stage 2) to Mg-rich clinochlore (Stage 3) and then to Fe-rich chamosite (Stage 4). Chlorite from Stage 2 (Chl-1) formed metasomatically at low fluid/rock ratios, while Stage 3 and 4 chlorites (Chl-2 and Chl-3) precipitated directly from higher fluid/rock ratio fluids. Chlorite compositions record a critical Stage 2–3 transition involving cooling from ~ 320 °C to ~ 260 °C, reduction (log fO2 from –33.6 to –39.7), and alkalinization, and sulfur fugacity remained stable within a narrow range (log fS2 = –13.6 to –8.0), followed in Stage 4 by minor reheating to ~280 °C, re-acidification, and a slight rebound in oxygen fugacity. Thermodynamic simulations reveal that the destabilization of Au(HS)2- complexes, primarily driven by the synergistic effects of cooling, pH increase, and decreasing oxygen fugacity, triggered gold precipitation during the main ore stage. Results demonstrate that abrupt cooling coupled with fluid alkalinization and reduction exerted the dominant control on gold precipitation in Jinshan, resolving long-standing debates on ore-forming mechanisms and highlighting chlorite as a robust quantitative sensor for fluid evolution.
Full article
(This article belongs to the Special Issue Gold Deposits: From Primary to Placers and Tailings After Mining)
Open AccessReview
High-Salinity Sedimentary Environments and Source–Reservoir System Development: Insights from Chinese Basins
by
Fei Huo, Chuan He, Yuhan Huang, Huiwen Huang, Xueyan Wu, Ruiyu Guo and Lingjie Yang
Minerals 2026, 16(3), 268; https://doi.org/10.3390/min16030268 (registering DOI) - 28 Feb 2026
Abstract
High-salinity water environments, e.g., saline lacustrine basins and lagoons, represent significant sedimentary settings on Earth. They serve not only as crucial archives of paleoclimate and paleoenvironmental evolution but also as favorable realms for the development of high-quality hydrocarbon source rocks. Although traditional views
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High-salinity water environments, e.g., saline lacustrine basins and lagoons, represent significant sedimentary settings on Earth. They serve not only as crucial archives of paleoclimate and paleoenvironmental evolution but also as favorable realms for the development of high-quality hydrocarbon source rocks. Although traditional views suggested that high salinity inhibits biological activity and is thus detrimental to source rock formation; recent hydrocarbon discoveries in formations such as the Leikoupo Formation (Sichuan Basin) and Majiagou Formation (Ordos Basin) in China have confirmed the exceptional hydrocarbon generation potential of source rocks in such settings. Focusing on major sedimentary basins in China, this review synthesizes how high-salinity settings critically control the integrated “generation-storage” sequence of hydrocarbon source rocks. Research indicates that moderate salinity can promote blooms of halophilic microorganisms, e.g., algae, cyanobacteria, resulting in high primary productivity. Concurrently, salinity-driven stable water stratification creates a strongly reducing bottom water environment, which greatly facilitates the preservation of organic matter, establishing a synergistic enrichment model of “high productivity—excellent preservation.” Products of high-salinity environments, such as evaporites, e.g., gypsum, halite, can act as catalysts, lowering the activation energy for hydrocarbon generation and enhancing hydrocarbon yield. Additionally, associated organic salts provide supplementary material for hydrocarbon generation. Regarding reservoir quality, the laminated structures formed in high-salinity settings, combined with organic–inorganic synergistic diagenesis, e.g., dolomitization, organic acid dissolution, and hydrocarbon-generation overpressure, collectively shape high-quality reservoirs with significant heterogeneity. Despite important progress, challenges remain, including the quantitative analysis of primary factors controlling organic matter enrichment, the threshold of salinity inhibiting biological communities, and the prediction of strongly heterogeneous reservoirs. Saline settings serve as critical carbon sinks in the geological carbon cycle through high primary productivity, enhanced preservation conditions, and distinctive mineral assemblages, playing a particularly important role in the formation of hydrocarbon source rocks and long-term carbon sequestration. Future research should integrate modern saline lake observations with high-resolution characterization techniques to deepen the understanding of the formation mechanisms of high-salinity source rocks, aiming to provide theoretical guidance and exploration targets for petroleum systems in similar geological settings worldwide.
Full article
(This article belongs to the Topic Formation Mechanism and Quantitative Evaluation of Deep to Ultra-Deep High-Quality Reservoirs)
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Open AccessArticle
Study on Radiometric Sorting of Uranium Ore Based on Deconvolution
by
Dongyang Wang, Xiongjie Zhang, Yang Liu, Yuantong Yan, Bao Wang, Shangwei Wu, Qi Liu, Xinqi Cai, Renbo Wang and Bin Tang
Minerals 2026, 16(3), 267; https://doi.org/10.3390/min16030267 (registering DOI) - 28 Feb 2026
Abstract
Uranium ore preconcentration is a critical step in achieving environmentally sustainable uranium mining and reducing the operational load of hydrometallurgical processing systems. Conventional radioactive sorting systems predominantly employ a “single-ore-particle intermittent measurement” mode. Under continuous ore flow and high-throughput operating conditions, however, the
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Uranium ore preconcentration is a critical step in achieving environmentally sustainable uranium mining and reducing the operational load of hydrometallurgical processing systems. Conventional radioactive sorting systems predominantly employ a “single-ore-particle intermittent measurement” mode. Under continuous ore flow and high-throughput operating conditions, however, the radiation fields of adjacent ore particles inevitably overlap, which results in gamma-counting interference and blurred ore-segment boundaries, thereby limiting sorting accuracy and system capacity. To address these challenges, this study established a convolutional model that describes the relationship between ore-grade distribution and gamma-response characteristics under continuous ore flow conditions. On this basis, a deconvolution-based method for uranium ore grade calculation was proposed, and an adaptive determination strategy for the characteristic parameter α was introduced to improve grade estimation accuracy and enable reliable identification of ore-segment boundaries. The experimental results showed that, for uranium grades ranging from 0.05% to 0.18% and ore-segment lengths of 16–40 cm, the relative errors between the inverted and true grades of individual segments were all less than 10%. Compared with conventional intermittent measurement and identification schemes, the proposed method achieves stable and accurate grade inversion under conditions of overlapping radiation fields in continuous ore segments.
Full article
(This article belongs to the Section Mineral Processing and Extractive Metallurgy)
Open AccessArticle
Performance-Based Mixture Screening for Sustainable Low-Clinker Supersulfated Cement Incorporating Ferronickel Slag, Desulfurized Gypsum, and Carbide Slag
by
Ping Chen, Liangqian Chen and Yang Sun
Minerals 2026, 16(3), 266; https://doi.org/10.3390/min16030266 (registering DOI) - 28 Feb 2026
Abstract
This study aimed to develop sustainable supersulfated cement (SSC) comprising ferronickel slag (FNS), desulfurized gypsum, carbide slag, and a small amount of Portland cement (PC). A two-stage optimization approach considering mechanical strength, volume stability, durability, and sustainability was employed to screen the mixture
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This study aimed to develop sustainable supersulfated cement (SSC) comprising ferronickel slag (FNS), desulfurized gypsum, carbide slag, and a small amount of Portland cement (PC). A two-stage optimization approach considering mechanical strength, volume stability, durability, and sustainability was employed to screen the mixture proportions of low-clinker FNS-based SSC. Orthogonal experiments were firstly conducted to investigate the effects of PC, carbide slag, and desulfurized gypsum contents on the mechanical properties of SSC mortar. Range analysis revealed that carbide slag exerted the most significant impact on early-age mechanical strength, while desulfurized gypsum plays an increasingly important role in late-age strength development. Subsequently, a single-factor test was applied to determine the optimal carbide slag content in FNS-based SSC. The results demonstrated that with the incorporation of 4% carbide slag, the SSC mortar achieved the 3-day and 28-day compressive strengths of 15.88 and 42.5 MPa, with relatively low volumetric expansion. The screened mixture proportions also satisfied the requirements for strength class 42.5 SSC according to both Chinese and British standards. A life cycle assessment further indicated that its carbon emission was approximately 46.91% lower than that of conventional PC. This research provided key technical and data support for the synergistic utilization of multi-source solid wastes in producing low-carbon cementless binder.
Full article
(This article belongs to the Section Clays and Engineered Mineral Materials)
Open AccessArticle
Genetic Mechanisms and Main Controlling Factors of Dolomite Reservoirs in Member 1 of the Lower Cambrian Canglangpu Formation, Northern–Central Sichuan Basin
by
Fei Huo, Chuan He, Xueyan Wu, Zhengdong Wang, Kezhong Li, Zhidian Xi, Yi Hu, Zhun Wang and Binxiu Li
Minerals 2026, 16(3), 265; https://doi.org/10.3390/min16030265 (registering DOI) - 28 Feb 2026
Abstract
In recent years, oil and gas exploration in the Lower Cambrian of the central–northern Sichuan Basin, China, has demonstrated enormous resource potential. As a potential interval of high-quality hydrocarbon source rocks, the Canglangpu Formation of the Lower Cambrian remains underdeveloped in exploration and
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In recent years, oil and gas exploration in the Lower Cambrian of the central–northern Sichuan Basin, China, has demonstrated enormous resource potential. As a potential interval of high-quality hydrocarbon source rocks, the Canglangpu Formation of the Lower Cambrian remains underdeveloped in exploration and lacks in-depth research. Affected by tectonics, sedimentary environment, and diagenesis, the genetic mechanisms and genetic models of carbonate reservoirs in the Canglangpu Formation within the study area need further clarification. This study utilizes petrological characteristics of dolomite and geochemical data to clarify diagenetic fluids of different reservoir rocks and identifies the main controlling factors and development models of the reservoirs. The results show that the dolomites in Member 1 of the Canglangpu Formation (Cang-1 Member) in central–northern Sichuan are mainly classified into three types: silty–fine crystalline dolomite (D1), granular dolomite (D2), and residual-texture dolomite (D3). The reservoir spaces are dominated by intercrystalline pores, intergranular pores, and structural fractures. The porosity of the Cang-1 Member in the area is relatively low, with an average porosity of 5% or lower. The reservoir porosity average is 3.63%, belonging to low-porosity reservoirs. The permeability average is 2.94 × 10−3 mD. Analysis of different geochemical indicators indicates that the diagenetic fluids of the three dolomite types are mainly syndepositional seawater. D1 is formed by penecontemporaneous dolomitization, while both D2 and D3 are formed during the shallow-to-middle burial stage. The main controlling factors of dolomite reservoirs include sedimentary facies, diagenesis, and tectonic movement. This study clarifies the genesis and development model of dolomite reservoirs in the Cang-1 Member, aiming to provide reliable and valuable references for the exploration of dolomite reservoirs in the Canglangpu Formation of the Sichuan Basin.
Full article
(This article belongs to the Topic Formation Mechanism and Quantitative Evaluation of Deep to Ultra-Deep High-Quality Reservoirs)
Open AccessArticle
Formation of Niujuan Ag-Au Deposit, North China Craton: Constraints from Pyrite Textures and In-Situ Trace Element and H-O-S Isotope Geochemistry
by
Chunlai Liu, Ruiming Cao, Wei Li, Xiaoxuan Liu, Ke Huang, Wei Pan, Wei Cui and Linan Cui
Minerals 2026, 16(3), 264; https://doi.org/10.3390/min16030264 (registering DOI) - 28 Feb 2026
Abstract
The North China Craton (NCC) hosts numerous world-class Au deposits and these Au deposits can be classified into the Au-only and Ag-Au polymetallics, respectively. The former is mostly located in the eastern NCC, such as in the giant Jiaodong Province, and the latter
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The North China Craton (NCC) hosts numerous world-class Au deposits and these Au deposits can be classified into the Au-only and Ag-Au polymetallics, respectively. The former is mostly located in the eastern NCC, such as in the giant Jiaodong Province, and the latter is mostly distributed along the northern and southern margins of the NCC. Compared with Au-only deposits, the ore genesis of the Ag-Au deposits remains controversial. This paper focuses on the Niujuan Ag-Au deposit in the Fengning ore cluster of the northern margin of the NCC. Detailed deposit geology investigation, texture analysis, and analyses of the in situ trace element and sulfur isotope compositions of pyrite, coupled with H-O isotope compositions of quartz from different stages, were conducted to elucidate the ore-forming processes and metal sources. The results showed that the formation of the Niujuan deposit can be divided into four stages, including a pre-ore siliceous breccia stage (stage 1), syn-ore quartz-pyrite stage (stage 2), syn-ore polymetallic sulfide stage (stage 3), and post-ore fluorite-calcite stage (stage 4). Among these, stage 3 represents the major Ag-Au mineralization stage. Pyrite is well developed within stage 2 and stage 3, representing the intensive sulfidation of the wall rock. Microscopic analytical techniques including gamma-enhanced reflected light and scanning electron microscopy backscattered electron (BSE) reveal that pyrite samples from stage 2 and stage 3 have distinct textures. Pyrite (Py1) from stage 2 is homogeneous but with numerous pores. In contrast, pyrite (Py2) from stage 3 has overgrowth textures, and be divided into three sub-stages from core to rim (Py2a, Py2b, and Py2c) with different BSE brightness levels. LA-ICP-MS trace elements analyses results show that these different stages of pyrite show different composition such as Au, As, Ag, Co, and Ni. Py1 has low Au and Ag concentrations ranging from < 0.1 ppm to 0.02 ppm and < 0.1 ppm to 21.8 ppm, respectively. Py2a has low Au and Ag concentrations ranging from < 0.1 ppm to 0.4 ppm and 0.4 ppm to 118.4 ppm, respectively. Py2b is characterized by high As and low Au contents, with average values of 6670.8 ppm for As and 1.4 ppm for Au. Py2c shows relatively low Co and Ni concentrations ranging from 0.02 ppm to 255.2 ppm and < 0.1 ppm to 9.9 ppm, respectively. The sulfur isotope composition of Py1 and Py2 is relatively consistent, ranging from 3.8‰ to 6.7‰. The H and O isotope compositions of quartz from stage 1, stage 2, and stage 3 have insignificant variations, ranging from −119.5‰ to −101.3‰ for δD and −6.8‰ to −3.7‰ for δ18Ofluid, respectively. The results show that sulfur and, possibly, Au and Ag were mainly derived from magmatic hydrothermal fluids, and a significant amount of meteoric water was involved. Combined with the published mineralizing ages (~140 Ma), this paper suggests that the Niujuan Ag-Au deposit formed during the Early Cretaceous under an extensional setting in response to the eastward retreating subduction of the Paleo-Pacific oceanic plate. Evidence from deposit geology and geochemistry reveals that the mixture of magmatic and meteoric water, together with intensive sulfidation, is the key factor controlling Au and Ag deposition.
Full article
(This article belongs to the Section Mineral Deposits)
Open AccessArticle
Chronology and Geochemistry of the REE-Mineralized Hatu Alkaline Rock, Mid-Eastern Kunlun
by
Shouzhi Zhan, Guangming Ren, Shukuan Wu, Tao Tian and Lizhi Zhao
Minerals 2026, 16(3), 263; https://doi.org/10.3390/min16030263 (registering DOI) - 28 Feb 2026
Abstract
The alkaline rocks located in the Hatu area of Dulan county in the middle section of the East Kunlun Orogenic Belt have a relatively high content of light rare earth elements (LREE). This study conducted scanning electron microscopy (SEM) petrographic methods, zircon U-Pb
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The alkaline rocks located in the Hatu area of Dulan county in the middle section of the East Kunlun Orogenic Belt have a relatively high content of light rare earth elements (LREE). This study conducted scanning electron microscopy (SEM) petrographic methods, zircon U-Pb dating, and geochemical work on two REE-mineralized alkaline rock outcrops, providing support for further work and study in the mining area. The REE-mineralized alkaline rocks are composed of alkali feldspar syenite, hornblende alkali feldspar syenite, and quartz alkali feldspar syenite. SEM analysis indicates that the REE are mainly hosted in REE-bearing minerals such as chevkinite, parisite, allanite, and monazite. The alkali feldspar syenite and hornblende alkali feldspar are enriched in REE, with a content of 994 × 10−6~5054 × 10−6. The zircon U-Pb dating results show that the ages of the two REE-mineralized alkaline rock are 423.6 ± 2.7 Ma and 431.2 ± 5.3 Ma, respectively. Geochemical analysis indicates that the Hatu alkaline rocks can be classify as A-type granite, and are characterized by evidence of a mixture of materials from the crust and mantle. Considering the regional tectonic history, it is primarily inferred that the Hatu REE-mineralization alkaline rocks were formed after the closure of the Proto-Tethys Ocean Basin and the Eastern Kunlun region experienced extensional tectonic stage, resulting in the upwelling of asthenospheric material and heating of crustal material. This study provides theoretical support for regional geochemical research and further exploration efforts in the Hatu area.
Full article
(This article belongs to the Special Issue Magmatic–Hydrothermal Process and the Genesis of Related Mineral Deposits)
Open AccessArticle
Geochemical Indicators of the Peraluminous W-Cu-Mo-(±Sn-Li-Ta-Nb) Granites in Dahutang Orefield in Northern Jiangxi and Their Significance for Exploration
by
Haimin Ye, Mangting Shen, Minggang Yu, Cunzhi Wang and Feipeng Fan
Minerals 2026, 16(3), 262; https://doi.org/10.3390/min16030262 (registering DOI) - 28 Feb 2026
Abstract
The origin of Mesozoic granites associated with the Dahutang W-Cu-Mo orefield in northern Jiangxi, which hosts the world’s second-largest tungsten deposit, remains a compelling subject despite extensive geochemical and geochronological studies. In this contribution, we present wolframite mineral and whole-rock geochemistry, as well
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The origin of Mesozoic granites associated with the Dahutang W-Cu-Mo orefield in northern Jiangxi, which hosts the world’s second-largest tungsten deposit, remains a compelling subject despite extensive geochemical and geochronological studies. In this contribution, we present wolframite mineral and whole-rock geochemistry, as well as monazite and zircon U-Pb ages, for the Mesozoic granites to constrain our understanding of the petrogenesis of these granites and their coupling relationship with the mineralization. The following two magmatic phases and four types of rocks in the study area are identified: the early stage (152–147 Ma) biotite (G1) granites and the late stage (144–130 Ma) two-mica (G2),muscovite (G3), and albite (G4) granite series. These two magmatic phases are temporally coincident with two mineralization stages (~150 Ma and 144–139 Ma). All the Mesozoic granites share the characteristics of high silica content, peraluminosity (A/CNK > 1.1), and low Zr + Nb + Ce + Y values (<200 ppm); they are derived from the partial melting of a Proterozoic crustal source and classified as S-type granites. Specifically, the G1 granites are characterized by relatively high MgO (~0.5%), CaO (~1%), and low P2O5 (0.13%–0.20%). They formed through a relatively high degree of partial melting at approximately 766 °C (zircon saturation temperatures), a process influenced by biotite dehydration reactions, with minor contributions from mantle-derived materials. In contrast, the G2–G4 granite series exhibits more typical peraluminous S-type granite features, such as high Al2O3, Na2O, and P2O5 (mostly > 0.2%) contents, and low Sr and Ba contents. They are products of low-degree partial melting that occurred under conditions close to muscovite breakdown at ~726 °C. Additionally, fluid–melt interaction is recorded in both granites by distinctive geochemical signatures, including enrichment in Sn (>30 ppm), Cs (>35 ppm), Li (>250 ppm), F (>0.4%), and W (10–1000 ppm), coupled with low K/Rb (<150) and Nb/Ta (<5) ratios. The near-chondritic Zr/Hf (22.6–34.1) and Y/Ho (24.5–31.5) ratios of the G1 granites imply a relatively limited role of magmatic fluid–melt interaction during its evolution. For the G2–G4 granites, however, intense crystal fractionation and late-stage fluid–melt interaction are well-documented by their highly variable and low ratios of Y/Ho (14.8–41.4), Nb/Ta (0.89–5.57), Zr/Hf (8.84–41.67), and K/Rb (13.96–128.29). In the long-lived, reduced, and volatile-rich aqueous environment of the G2–G4 magmas, fractional crystallization and albitization collectively enhanced the solubility and hydrothermal transport capacity of W, Sn, Li, Nb, and Ta by multiple orders of magnitude. In contrast, in the earlier, more oxidized G1 magmas (which incorporated mantle materials), the exsolution and hydrothermal transport of Cu and Mo were associated with localized greisenization, but their capacity diminished with fractional crystallization. Historically, mineral exploration in the Dahutang mining area has focused primarily on W, Cu, and Mo. Based on this research, we conclude that there is significant mineral potential for rare metals (particularly Sn, Li, and Ta), and future exploration should prioritize areas adjacent to the evolved G2–G4 peraluminous leucogranites to search for new concealed mineral occurrences.
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(This article belongs to the Section Mineral Exploration Methods and Applications)
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Open AccessArticle
Detrital Zircon U-Pb Geochronology and Hf Isotopic of the Taiyuan Formation, Qinshui Basin: Implications for Maximum Sedimentary Age and Provenance Shift
by
Yuehua Hou, Fenghua Zhao, Dongna Liu, Linhua Zhong, Shangqing Zhang and Qi Zhang
Minerals 2026, 16(3), 261; https://doi.org/10.3390/min16030261 (registering DOI) - 28 Feb 2026
Abstract
To constrain the Late Paleozoic tectonic evolution of Taiyuan Formation, we conducted detrital zircon U-Pb dating and Hf isotopes analysis. The U-Pb age spectra from ten sandstone samples (taken from both the top and bottom of the formation) display four major age groups
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To constrain the Late Paleozoic tectonic evolution of Taiyuan Formation, we conducted detrital zircon U-Pb dating and Hf isotopes analysis. The U-Pb age spectra from ten sandstone samples (taken from both the top and bottom of the formation) display four major age groups of 2.6–2.4 Ga, 2.2–1.8 Ga, 496–421 Ma and 350–270 Ma with highest peaks at ca. 323 Ma and 443 Ma. Moreover, on the basis of the weighted mean age of the five youngest detrital zircons (293.0 ± 4.1 Ma), combined with published results, we propose that the Taiyuan Formation formed during the Early Permian. Comparison of detrital zircon U-Pb age spectra and Hf isotopic compositions with potential source regions indicates that the early Paleozoic zircons were largely derived from the North Qinling orogenic belt, whereas the late Paleozoic zircons originated from the Inner Mongolia uplift. This shift reveals a significant provenance change recorded in the Taiyuan Formation. The uplift of the northern North China Craton (Inner Mongolia uplift) is interpreted as a response to the resubduction of the Paleo-Asian Ocean during the Late Paleozoic. The resulting paleogeographic pattern—higher in the north and lower in the south—redirected sediment supply for the uppermost sandstone and overlying strata of the Taiyuan Formation in the Qinshui Basin from the earlier North Qinling orogenic belt to the Inner Mongolia uplift.
Full article
(This article belongs to the Section Mineral Deposits)
Open AccessArticle
Evaluating Sparse Magnetotelluric Arrays for Imaging Deep Volcanic Plumbing Systems: Insights from Sensitivity and PSF Analyses
by
Yabin Li, Yu Tang, Shuai Qiao, Yunhe Liu, Weijie Guan, Chuncheng Li and Dajun Li
Minerals 2026, 16(3), 260; https://doi.org/10.3390/min16030260 (registering DOI) - 28 Feb 2026
Abstract
Volcanic magma plumbing systems is essential for understanding crustal–mantle material exchange and the dynamics of volcanic activity. The magnetotelluric method (MT) offers an effective tool for imaging conductive features from the crust to the lithospheric mantle. However, current survey strategies face a tradeoff
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Volcanic magma plumbing systems is essential for understanding crustal–mantle material exchange and the dynamics of volcanic activity. The magnetotelluric method (MT) offers an effective tool for imaging conductive features from the crust to the lithospheric mantle. However, current survey strategies face a tradeoff between imaging resolution and acquisition cost. Here, we construct a lithosphere-scale synthetic model of a magma plumbing system and use 3D MT inversion, sensitivity analysis, and point spread function evaluation to assess the resolving capability of sparse versus dense arrays. Our results show that large-scale conductive anomalies in the mid–lower crust and lithospheric mantle can be reliably imaged using a sparse regional array with targeted densification in the crustal anomaly zone. This approach reduces field costs and computational demand. Guided by these findings, we conducted MT observations across the Longgang volcanic field and identified low-resistivity anomalies extending from the lithospheric mantle into the mid–lower crust. These features are consistent with the dense array MT inversion results. Our study demonstrates that an array strategy combining wide-area sparse coverage with targeted densification offers a cost-effective approach to image deep conductive structures, which may provide practical guidance for optimizing MT survey design in volcanic regions.
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(This article belongs to the Special Issue Gravity, Magnetic, and Electromagnetic (GME) Geophysical Data Interpretation for Mineral Exploration and Crustal Structure Investigation)
Open AccessArticle
Genetic Mechanism of Calcareous Interbeds in Shoreface Reservoirs and Implications for Hydrocarbon Accumulation: A Case Study of the Donghe Sandstone Reservoir in Hade Oilfield, Tarim Basin
by
Rui Xie, Xiaoyun Lin, Shan Jiang, Kaiyu Wang, Jian Liu and Yijing Lu
Minerals 2026, 16(3), 259; https://doi.org/10.3390/min16030259 (registering DOI) - 28 Feb 2026
Abstract
Calcareous interbeds are widely developed in marine clastic sequences, where laterally continuous, tight calcareous interbeds act as critical controls on the formation of lithologic traps and the distribution of oil. However, the genetic mechanisms and development models of these interbeds, particularly under deep-burial
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Calcareous interbeds are widely developed in marine clastic sequences, where laterally continuous, tight calcareous interbeds act as critical controls on the formation of lithologic traps and the distribution of oil. However, the genetic mechanisms and development models of these interbeds, particularly under deep-burial conditions subject to complex fluid interactions, remain poorly understood. Using the Donghe Sandstone in the Hade Oilfield (Tarim Basin) as a case study, this paper investigates the genetic evolution of calcareous interbeds via an integrated approach combining core observation, thin-section petrography, scanning electron microscopy (SEM), stable isotope analysis, fluid inclusion microthermometry, and heavy fraction analysis. The results indicate that: (1) The carbonate cements within the interbeds are compositionally complex, dominated by calcite but characterized by a diagnostic assemblage of anhydrite, ferroan calcite, and ankerite. (2) During the depositional to shallow burial stages, seawater evaporation and meteoric freshwater influx led to the supersaturation of calcium-rich pore waters near the surface. This facilitated the precipitation of early cement assemblages, which are predominantly of freshwater origin and consist mainly of non-ferroan calcite nodules, dolomite, and anhydrite. (3) During the deep burial stage, the injection of high-salinity brines and organic acid decarboxylation triggered Thermochemical Sulfate Reduction (TSR). This process caused the extensive consumption of the pre-existing anhydrite and the formation of authigenic pyrite, followed by the tight occlusion of remaining porosity through the precipitation of late-stage ferroan calcite and ankerite. (4) In the broad slope setting, these tight calcareous interbeds constitute effective flow barriers, resulting in a stepped distribution of the oil–water contact. Within the reservoir compartments segmented by these interbeds, crude oil maturity exhibits a distinct inversion (i.e., higher maturity below the interbeds and lower maturity above), confirming the critical sealing capacity of the interbeds during hydrocarbon accumulation. Ultimately, this study establishes a genetic model coupling calcareous interbed development with deep-burial fluid alteration, providing new geological insights for predicting subtle traps in marine sandstone reservoirs.
Full article
(This article belongs to the Special Issue Advances in Carbonate Sedimentology: From Deposition to Diagenesis)
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Open AccessArticle
Lithofacies and Pore Structures of the Permian Qixia Dolostone Reservoirs (Central Sichuan Basin, China): Implication of Hydrothermal Dolomitization on Reservoir Quality
by
Xingyu Zhang, Haizhou Qu, Lianjin Zhang, Xiugen Fu, Ziye Lu, Dongfan Yang, Huilin Xu and Yunfeng Zhang
Minerals 2026, 16(3), 258; https://doi.org/10.3390/min16030258 (registering DOI) - 28 Feb 2026
Abstract
The Permian Qixia dolostone in the Central Sichuan Basin is a significant hydrocarbon reservoir of hydrothermal origin, linked to the Emeishan Large Igneous Province and structurally controlled by E–W strike–slip faults. However, how this process controls reservoir quality remains poorly understood. To address
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The Permian Qixia dolostone in the Central Sichuan Basin is a significant hydrocarbon reservoir of hydrothermal origin, linked to the Emeishan Large Igneous Province and structurally controlled by E–W strike–slip faults. However, how this process controls reservoir quality remains poorly understood. To address this, we integrate core observation, thin-section petrography, XRD analysis, thickness mapping, MICP, and μ-CT to characterize the lithofacies and pore structures of the Qixia Formation in the study area. Six lithofacies are recognized, including mudstone (F1), wackestone (F2), packstone (F3), grainstone (F4), rudstone (F5), and dolostone (F6), and F6 is further divided into three subtypes (F6-1, F6-2, F6-3). Dolostones exhibit superior reservoir quality relative to limestones, and among the dolostone, reservoir quality improves progressively from F6-1 to F6-3 with increasing crystal size and dolomite content. Dolostone distribution is spatially tied to E–W strike–slip faults, and its formation age coincides with documented fault activity, implicating these faults as the primary fluid conduits. Quantitative pore structure analyses further indicates that dolomitization enhanced permeability by enlarging pore–throat radii and improving macropore connectivity, with associated dissolution contributing additional secondary porosity.
Full article
(This article belongs to the Special Issue Deformation, Diagenesis, and Reservoir in Fault Damage Zone)
Open AccessArticle
REE Enrichment Process in the Maoniuping Carbonatite-Related REE Deposits, Mianning, Sichuan: Genetic and Mineralogical Evidence
by
Yanan Jin, Wei Wang, Bin He, Zhi Zhao and Ruiwei Zhao
Minerals 2026, 16(3), 257; https://doi.org/10.3390/min16030257 (registering DOI) - 28 Feb 2026
Abstract
The Maoniuping deposit, recognized as the world’s third-largest light rare earth (LREE) deposit, is characterized by exceptional ore-forming conditions and considerable exploration potential. Based on systematic mineralogical investigations of chevkinite, allanite, and bastnäsite, this paper synthesizes the trace elements and rare-earth element (REE)
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The Maoniuping deposit, recognized as the world’s third-largest light rare earth (LREE) deposit, is characterized by exceptional ore-forming conditions and considerable exploration potential. Based on systematic mineralogical investigations of chevkinite, allanite, and bastnäsite, this paper synthesizes the trace elements and rare-earth element (REE) geochemical characteristics of these minerals to elucidate their enrichment mechanisms and metallogenic processes. The results reveal a crystallization sequence of chevkinite → allanite → bastnäsite, accompanied by a progressive decrease in the content of Nb, Ta, Zr, Hf, Sr, and Ba. This trend indicates continuous magmatic–hydrothermal evolution of the ore-forming fluids. REE enrichment exhibits distinct stages: early-stage enrichment of HREE, mid-stage enrichment of Ce, Pr, and Nd, and late-stage dominance of La. For chevkinite (δCe = 0.98–1.11, avg. 1.05; δEu = 0.75–0.87, avg. 0.82) and bastnäsite (δCe = 0.81–1.15, avg. 0.88; δEu = 0.58–0.79, avg. 0.66), the evolution process of the continuous increase in oxygen fugacity within the metallogenic system is recorded. The low-temperature, high-oxygen fugacity environment facilitates the incorporation of LREEs into bastnäsite lattices, enabling the formation of large-scale REE ore bodies at structurally favorable positions. These findings provide direct mineralogical evidence for understanding REE enrichment mechanisms in alkaline magmatic–hydrothermal systems and offer crucial insights for metallogenic process inversion and exploration assessment of analogous REE deposits.
Full article
(This article belongs to the Section Mineral Deposits)
Open AccessArticle
Effect of Ball Filling Ratio on Fine Particle Production Characteristics During Ceramic Ball Grinding of Magnetite Ore
by
Li Ling, Chengfang Yuan, Liying Sun, Caibin Wu, Quan Li, Ziyu Zhou and Zongyan Zhou
Minerals 2026, 16(3), 256; https://doi.org/10.3390/min16030256 (registering DOI) - 28 Feb 2026
Abstract
To clarify the influence of the media filling ratio on fine particle production during ceramic ball grinding of magnetite, magnetite ore from the fine grinding stage of an industrial concentrator was investigated under different feed size classes and media filling ratios through grinding
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To clarify the influence of the media filling ratio on fine particle production during ceramic ball grinding of magnetite, magnetite ore from the fine grinding stage of an industrial concentrator was investigated under different feed size classes and media filling ratios through grinding kinetics experiments. The generation behavior of the fine and finest particle fractions during ceramic ball grinding was systematically analyzed. The results indicate that particle size fractions with sizes less than or equal to 0.150 mm exhibit pronounced zero-order production characteristics under different filling ratios, with cumulative yields showing a strong linear relationship with grinding time. This zero-order behavior is insensitive to variations in the media filling ratio. Conversely, the generation rate of the finest size fraction is significantly affected by the media filling ratio. For coarse feed sizes, the generation rate of the finest fraction initially increases and then decreases with increasing filling ratio, reaching a peak value of 6.23%/min at a filling ratio of 35%. When the feed falls below 1.18 mm, the generation rate of the finest fraction shows a strong positive correlation with the ceramic ball filling ratio. Furthermore, based on the functional relationship between the generation rate of the finest size fraction and the mill input power, an energy–size model for magnetite ceramic ball grinding was established, providing a quantitative description of the variation in the finest particle yield with respect to the input energy and media filling ratio. The findings provide a theoretical foundation for optimizing media filling ratios, enhancing fine grinding performance, and controlling overgrinding in industrial applications.
Full article
(This article belongs to the Collection Advances in Comminution: From Crushing to Grinding Optimization)
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Open AccessArticle
Mechanistic Analysis of the Effect of Hematite Concentrates on the Sintering Properties of Iron Ore Fines: Based on Process Mineralogy and Sintering Properties
by
Sijun Xie, Jian Pan, Deqing Zhu, Qingshi Song, Siwei Li, Congcong Yang, Zhengqi Guo and Mengjie Hu
Minerals 2026, 16(3), 255; https://doi.org/10.3390/min16030255 (registering DOI) - 28 Feb 2026
Abstract
The sintering process represents a primary source of dust, SO2, NOx, and CO2 emissions in steel mills. Utilizing high-grade concentrate with low impurity content can directly reduce slag generation at the source, thereby decreasing fuel consumption and minimizing associated emissions.
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The sintering process represents a primary source of dust, SO2, NOx, and CO2 emissions in steel mills. Utilizing high-grade concentrate with low impurity content can directly reduce slag generation at the source, thereby decreasing fuel consumption and minimizing associated emissions. This study investigated the physicochemical properties, microstructure, and elemental distribution of hematite concentrates (H2 and H3) and H1 sinter fines. Sinter pot tests were conducted to evaluate the effects of blending these two concentrates on sintering performance and key quality indices. Microstructural analysis and quantitative phase composition statistics of the sintered products were performed to elucidate the mechanisms by which these concentrates influence sintering outcomes. Results demonstrated that replacing 33% H1 sinter fines with 33% H2 or H3 concentrates reduced the tumbler index from 73.6% to 68.5% and 73.2%, respectively. The productivity coefficient decreased to 68.5% and 73.2%, while solid fuel consumption increased from 73.9 kg/t to 90.5 kg/t and 81.2 kg/t. RI declined from 80.0% to 77.9% and 78.4%, whereas RDI improved from 72.9% to 76.8% and 75.8%.
Full article
(This article belongs to the Special Issue Mineralogy of Iron Ore Sinters, 3rd Edition)
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Open AccessArticle
Numerical Simulation of Air-Water-Mineral Three-Phase Flow in a Flotation Column for Graphite
by
Zhineng Liu, Jun Wang, Dongfang Lu, Hongchang Liu, Baojun Yang, Rui Liao, Lianjun Wu and Guanzhou Qiu
Minerals 2026, 16(3), 254; https://doi.org/10.3390/min16030254 (registering DOI) - 28 Feb 2026
Abstract
This study aims to clarify the influence mechanism of air–water–mineral three-phase flow behavior on separation efficiency in a graphite flotation column, addressing the issues of over-breaking of coarse graphite flakes and low recovery of fine particles caused by mismatched flow fields and operating
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This study aims to clarify the influence mechanism of air–water–mineral three-phase flow behavior on separation efficiency in a graphite flotation column, addressing the issues of over-breaking of coarse graphite flakes and low recovery of fine particles caused by mismatched flow fields and operating parameters in traditional flotation columns. Using CFD numerical simulations based on the Eulerian multiphase flow model, the standard k-ε turbulence model, and scalable wall functions, the effects of feed velocity (0.8–2.4 m/s) and aeration velocity (1–5 m/s) on the flow field structure, gas holdup distribution, and weighted average bubble–particle collision probability inside the column were systematically analyzed. Key quantitative results show that under the synergistic condition of a feed velocity of 2 m/s and an aeration velocity of 3 m/s, an internal circulation flow field conducive to particle retention is formed. Under these conditions, the gas holdup in the collection zone reaches an optimal range (0.26–0.27), and the weighted average collision probability increases by approximately 22% compared to the baseline condition. Aeration velocity shows a significant positive correlation with gas holdup in the collection zone (~0.235 at 1 m/s, rising to ~0.285 at 5 m/s). While an increase in feed velocity reduces the overall gas volume fraction, it enhances turbulence and promotes uniform bubble dispersion through the spatial distribution of regions with high collision probability from the upper part to the upper–middle part of the column and improves the uniformity of distribution. The novelty of this study lies in being the first to quantitatively reveal, through CFD simulation, the coupled regulatory effects of feed velocity and aeration velocity on the stratified flow field structure and mineralization probability in a flotation column and to identify the key optimization threshold of “2 m/s feed velocity”. The practical significance is that it provides a clear theoretical basis and operational window for energy saving, consumption reduction, and process intensification in industrial flotation columns. It offers directly applicable parameter optimization strategies for the efficient recovery of fine-flake graphite and the protection of coarse flakes.
Full article
(This article belongs to the Special Issue Mineral Processing and Extractive Metallurgy of Sulfide Ores, 2nd Edition)
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Open AccessArticle
Insights into the Precipitation of Biocement Minerals Using Microfluidic Devices and SEM Images
by
Mariana M. Pinto, Vânia Silvério, Manuel Francisco Costa Pereira, Sofia O. D. Duarte, Gabriel A. Monteiro and Rafaela Cardoso
Minerals 2026, 16(3), 253; https://doi.org/10.3390/min16030253 (registering DOI) - 28 Feb 2026
Abstract
Microbially Induced Carbonate Precipitation (MICP) is a biochemical process that promotes the precipitation of calcium carbonate, mainly in the mineral form of calcite, using urease-producing bacteria. This method has numerous applications, particularly in the field of geotechnical engineering when it is adopted for
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Microbially Induced Carbonate Precipitation (MICP) is a biochemical process that promotes the precipitation of calcium carbonate, mainly in the mineral form of calcite, using urease-producing bacteria. This method has numerous applications, particularly in the field of geotechnical engineering when it is adopted for soil improvement or for the consolidation of porous or cracked construction materials such as stone and concrete. One microfluidic platform made of polymethylmethacrylate (PMMA) was designed with multiple channels, and the minerals precipitated were visualized using an optical microscope. The precipitated mineral observed in all channels analyzed formed spherical mineral structures with a core and multiple external rings. The same spherical mineral structures were observed in the biocement layer precipitated on plates of the same material as that of the microfluidic platform and on limestone, following the same treatment protocol. SEM images of pieces of these layers, complemented with EDS and mineral analysis by XRD, have confirmed the existence of multiple layers of minerals with spherical structures, mainly vaterite, precipitated around a nucleation point. Overlapping minerals in both the confined microfluidic channels and the unconstrained plates indicate that overlap results from repeated injections rather than physical confinement. From the tests with the microfluidic devices, these studies revealed that crystallization depends on different factors, namely the size of the channels and the number of Sporosarcina pasteurii cells. The number of injections appeared to affect the number of rings precipitated around the inner core. Substrate effects on spatial distribution or adhesion may still exist but were not detectable in this study and require further investigation. The observation of similar mineralogical structures in both the microfluidic devices and the plates, particularly the limestone, demonstrates that microfluidic systems are effective tools for small-scale visualization of geological processes.
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(This article belongs to the Section Biomineralization and Biominerals)
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Open AccessArticle
Influence of Particle Size and Micronization on the Adsorption Efficiency of Aflatoxin B1 by Bentonite in Animal Feed Applications
by
Sonja Milićević, Jovica Stojanović, Ivica Ristović, Hunor Farkaš, Vladimir Dragiša Jovanović, Nevena Stojković and Dragan Radulović
Minerals 2026, 16(3), 252; https://doi.org/10.3390/min16030252 (registering DOI) - 27 Feb 2026
Abstract
Aflatoxin B1 (AFB1) is one of the most toxic mycotoxins contaminating animal feed, and bentonite clays are widely used as adsorbents to reduce its bioavailability. This study introduces and characterizes a new, previously unexplored bentonite deposit from Bijelo Polje (Bar, Montenegro), with ~55%
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Aflatoxin B1 (AFB1) is one of the most toxic mycotoxins contaminating animal feed, and bentonite clays are widely used as adsorbents to reduce its bioavailability. This study introduces and characterizes a new, previously unexplored bentonite deposit from Bijelo Polje (Bar, Montenegro), with ~55% montmorillonite in the raw material. Size fractions (<0.200 mm, <0.037 mm, <0.005 mm) were obtained by sieving and centrifugation and characterized by laser diffraction, chemical composition, BET, CEC, and quantitative XRD (Rietveld). In vitro AFB1 adsorption (2–50 ppm, pH 3.0, 0.02% w/v adsorbent) simulated monogastric gastrointestinal conditions. Progressive size reduction increased smectite content (from ~55% to 91%), CEC (44–70 meq/100 g), purity, and BET specific surface area (26.5–50.8 m2/g), while reducing impurities and heavy metals to undetectable levels. The finest fraction (<0.005 mm) achieved the highest maximum adsorption capacity (qmax ≈ 240 mg/g), attributed to enhanced surface homogeneity and site accessibility, significantly outperforming coarser fractions and most unmodified natural bentonites. Only the <0.005 mm fraction fully complies with EU regulatory requirements (Commission Implementing Regulation (EU) No 1060/2013) for AFB1-binding feed additives (≥70% dioctahedral smectite, >90% binding, low quartz/calcite). These results demonstrate that simple mechanical fractionation can yield exceptional performance in a novel natural raw material, offering a cost-effective, sustainable alternative to chemical modification for mycotoxin mitigation.
Full article
(This article belongs to the Section Clays and Engineered Mineral Materials)
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