Metallogenic characteristics and mineralization of supergiant gold deposits (223 t) in the northeastern margin of the Jiaolai Basin, Shandong Province: A review

Jun-wei Bo , Zheng-jiang Ding , Jun Deng , Feng-yue Sun , Kun-feng Qiu , Ming-chun Song

China Geology ›› 2025, Vol. 8 ›› Issue (4) : 806 -842.

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China Geology ›› 2025, Vol. 8 ›› Issue (4) :806 -842. DOI: 10.31035/cg2023122
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Metallogenic characteristics and mineralization of supergiant gold deposits (223 t) in the northeastern margin of the Jiaolai Basin, Shandong Province: A review

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Abstract

Since the first discovery of gold deposits on the northeastern margin of the Jiaolai Basin in Shandong Province at the end of the 20th century, seven medium-sized to large/super-large gold deposits have been identified in this region, with cumulative proven gold resources of 223 t. This study reviewed the metallogenic and geochemical characteristics of various gold deposits in this region, examined the sources of their ore-forming fluids and materials, as well as their gold metallogenic epochs and processes, and developed a gold metallogenic model. The gold deposits in this region are governed by both dense fractures and detachment structural systems along basin margins, primarily categorized into the altered rock type and the pyrite-bearing carbonate vein type. The latter type, a recently discovered mineralization type in the Jiaodong Peninsula, enjoys high gold grade, a large scale, and high gold mineral fineness, suggesting considerable prospecting potential. Both types of gold deposits show metallogenic epochs ranging from 116 Ma to 119 Ma. Their ore-forming fluids are identified as a CO2-NaCl-H2O fluid system characterized by moderate to low temperatures, moderate to low salinity, and low density, with the pyrite-bearing carbonate vein-type gold deposits manifesting slightly higher salinity. The C-H-O, S, and Pb isotopes of hydrothermal minerals reveal that the ore-forming fluids and materials are characteristic of crust-mantle mixing. Specifically, they were derived from mantle fluids in the early stages, mixed with stratum water and meteoric water in the later stages for mineralization. The gold metallogenic process is identified as follows: During the Early Cretaceous, the subduction of the Pacific Plate and the destruction of the North China Craton led to asthenospheric upwelling. The resulting fluids, after metasomatizing the enriched mantle, differentiated and evolved into C-H-O ore-bearing fluids, which were then mixed with crustal fluids. The mixed fluids migrated to the shallow crust, where they mingled with stratum water and meteoric water. Then, the fluids underwent unloading and final mineralization in detachment fault tectonic systems on basin margins. Due to differences in mixed crustal materials or the surrounding rocks involved in water-rock interactions, altered rock- and pyrite-bearing carbonate vein-type gold deposits were formed in acidic and alkaline fluid environments, respectively.

Keywords

Supergiant gold deposit / Pyrite-bearing carbonate vein-type / Altered rock type / CO2-NaCl-H2O fluid system / C-H-O, S, and Pbisotopes / Mantle fluids / Metallogenic characteristics / Mineralization / Mineral exploration engineering / Jiaolai Basin / Shandong Province

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Jun-wei Bo, Zheng-jiang Ding, Jun Deng, Feng-yue Sun, Kun-feng Qiu, Ming-chun Song. Metallogenic characteristics and mineralization of supergiant gold deposits (223 t) in the northeastern margin of the Jiaolai Basin, Shandong Province: A review. China Geology, 2025, 8(4): 806-842 DOI:10.31035/cg2023122

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CRediT authorship contribution statement

Zheng-jiang Ding, Jun Deng and Feng-yue Sun conceived of the presented idea. Jun-wei Bo and Zheng-jiang Ding wrote the manuscript in consulation. Jun-wei Bo processed the data and drew all the figures. Jun-wei Bo, Zheng-jiang Ding, Fengyue Sun, and Kun-feng Qiu participated in field investigation. Jun Deng and Ming-chun Song reviewed the draft. All authors discussed the results and contributed to the final manuscript.

Declaration of competing interest

The authors declare no conflicts of interest.

Acknowledgment

This study was supported by the Program of the National Natural Science Foundation of China (Nos. 41973048, U2006201), the Open Project of State Key Laboratory of Geological Processes and Mineral Resources (No. GPMR202203), the Key R&D Program of Shandong Province (No. 2023CXGC011001), the Taishan Scholars. Program (tstp20240847), and the Open Project of Shandong Engineering Research Center of Application and Development of Big Data for Deep Gold Exploration (No. SDK202207). The authors would like to extend their sincere gratitude to the reviewers of this manuscript for their valuable comments.

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