Mineral Prospectivity Mapping of the Kalatag Cu–Polymetallic District, Eastern Tianshan, NW China, Using a Maximum Entropy Model

The Kalatag Cu–polymetallic district in the Eastern Tianshan Orogen, NW China, is characterized by complex tectono-magmatic evolution and diverse mineralization styles, including porphyry-skarn, hydrothermal-vein, and volcanogenic massive sulfide (VMS) systems. However, only nine verified mineral occurrences were available for calibration of the present regional prospectivity model. This small occurrence dataset, together with the heterogeneous spatial distribution of geological and geochemical indicators, poses a challenge for regional prospectivity mapping. In this study, a Maximum Entropy (MaxEnt) model was developed to evaluate Cu–polymetallic prospectivity using presence-only mineral occurrence data. Seven rock-debris geochemical predictors, including Cu, Zn, Au, Mo, Ag, Ni, and Sb, were selected based on statistical characteristics and metallogenic relevance, while two geological predictors representing proximity to faults and intrusions were derived from regional geological maps. Nine-fold leave-one-out cross-validation (LOOCV) was used to evaluate out-of-sample discrimination and model sensitivity to regularization. The interpretation-oriented RM = 0.5 configuration yielded a mean LOOCV test AUC of 0.665, whereas the final model fitted using all nine verified occurrences achieved a training AUC of 0.850. High-prospectivity zones occupied 12.20% of the study area and contained 88.89% of known mineral occurrences. Jackknife analysis and response curves indicate that distance to intrusions, distance to faults, and Au anomalies provide the strongest independent spatial information within the predictor system. Prospectivity is generally enhanced near fault zones and intrusive contacts, highlighting the importance of tectono-magmatic architecture in controlling the spatial distribution of Cu–polymetallic mineralization. The resulting prospectivity map identifies regional high-prospectivity zones where favorable geological and geochemical conditions coincide, providing a quantitative basis for exploration prioritization. The study indicates that MaxEnt is an effective approach for integrating multisource geoscientific data under small-sample and presence-only conditions, while emphasizing that model outputs require further validation through geological, geochemical, geophysical, and drilling investigations.

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Journal
Minerals
Published
2026-09-28
DOI
https://doi.org/10.3390/min16100999
Primary Topic
Geochemistry and Geologic Mapping
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article
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article

Mineral Prospectivity Mapping of the Kalatag Cu–Polymetallic District, Eastern Tianshan, NW China, Using a Maximum Entropy Model

Haiyang He, Xiaoqiang Zhu, Zhiyuan Sun, Cai Jia et al.
Minerals
Geochemistry and Geologic Mapping
article

Mineral Prospectivity Mapping of the Kalatag Cu–Polymetallic District, Eastern Tianshan, NW China, Using a Maximum Entropy Model

Haiyang He, Xiaoqiang Zhu, Zhiyuan Sun, Cai Jia, Xiaole Qiu, Huicong Mou, Yongjian Gu, Wenru Hao
article en

Abstract

The Kalatag Cu–polymetallic district in the Eastern Tianshan Orogen, NW China, is characterized by complex tectono-magmatic evolution and diverse mineralization styles, including porphyry-skarn, hydrothermal-vein, and volcanogenic massive sulfide (VMS) systems. However, only nine verified mineral occurrences were available for calibration of the present regional prospectivity model. This small occurrence dataset, together with the heterogeneous spatial distribution of geological and geochemical indicators, poses a challenge for regional prospectivity mapping. In this study, a Maximum Entropy (MaxEnt) model was developed to evaluate Cu–polymetallic prospectivity using presence-only mineral occurrence data. Seven rock-debris geochemical predictors, including Cu, Zn, Au, Mo, Ag, Ni, and Sb, were selected based on statistical characteristics and metallogenic relevance, while two geological predictors representing proximity to faults and intrusions were derived from regional geological maps. Nine-fold leave-one-out cross-validation (LOOCV) was used to evaluate out-of-sample discrimination and model sensitivity to regularization. The interpretation-oriented RM = 0.5 configuration yielded a mean LOOCV test AUC of 0.665, whereas the final model fitted using all nine verified occurrences achieved a training AUC of 0.850. High-prospectivity zones occupied 12.20% of the study area and contained 88.89% of known mineral occurrences. Jackknife analysis and response curves indicate that distance to intrusions, distance to faults, and Au anomalies provide the strongest independent spatial information within the predictor system. Prospectivity is generally enhanced near fault zones and intrusive contacts, highlighting the importance of tectono-magmatic architecture in controlling the spatial distribution of Cu–polymetallic mineralization. The resulting prospectivity map identifies regional high-prospectivity zones where favorable geological and geochemical conditions coincide, providing a quantitative basis for exploration prioritization. The study indicates that MaxEnt is an effective approach for integrating multisource geoscientific data under small-sample and presence-only conditions, while emphasizing that model outputs require further validation through geological, geochemical, geophysical, and drilling investigations.

MineralsVol. 16(10)
Hefei University of Technology (CN), Anhui Conch Design and Research Institute of Building Materials (China) (CN), Anhui Institute of Robotics Industrial Technology Research Institute (CN), Suzhou University (CN), Anhui Normal University (CN), University of South China (CN)
Peace, Justice and strong institutions, Reduced inequalities
Openalex Percentile: Top 9%
Geochemistry and Geologic Mapping
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