首页|Geology and mineralization of the Hongqiling large magmatic nickel-copper-cobalt deposit(22× 104t)in Jilin Province,China:A review

Geology and mineralization of the Hongqiling large magmatic nickel-copper-cobalt deposit(22× 104t)in Jilin Province,China:A review

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The Hongqiling large nickel-copper-cobalt deposit(hereafter referred to as the Hongqiling deposit),a typical mafic-ultramafic copper-nickel deposit in China,boasts proven Ni(Ni)resources of approximately 22× 104 t,associated copper resources of 2× 104 t,and associated cobalt(Co)resources of 0.5× 104 t,with Ni reserves ranking 10th among China's magmatic nickel deposits.Geotectonically,the Hongqiling deposit is situated in the superimposed zone between the Xing'an-Mongolian orogenic belt and the circum-Western Pacific's active continental margin belt.Its ore-bearing plutons occur within the metamorphic rocks of the Ordovician Hulan Group,with the emplacement of plutons and the locations of orebodies governed by the deep-seated Huifahe fault and its secondary NW-trending Fujia-Hejiagou-Beixinglong-Changsheng fault zone.In the deposit,the rock assemblages of ore-bearing plutons predominantly encompass gabbro-pyroxenite-olivine pyroxenite-pyroxene peridotite(pluton No.1)and norite-orthopyroxenite-harzburgite(pluton No.7),with ore-bearing lithofacies consisting primarily of olivine pyroxenite and pyroxenite facies.The Hongqiling deposit hosts stratoid,overhanging lentoid,veined,and pure-sulfide veined orebodies.Its ores principally contain metallic minerals including pyrrhotite,pentlandite,chalcopyrite,violarite,and pyrite.Despite unidentified magma sources of ore-bearing mafic-ultramafic rocks,it is roughly accepted that the magmatic evolution in the Hongqiling deposit primarily involved fractional crystallization and crustal contamination.The ore-forming materials were primarily derived from the upper mantle,mixed with minor crustal materials.The ore-bearing mafic-ultramafic rocks in the deposit,primarily emplaced during the Indosinian(208-239 Ma),were formed in an intense extension setting followed by the collisional orogeny between the North China Plate and the Songnen-Zhangguangcai Range Block during the Middle-Late Triassic.From the perspective of the metallogenic geological setting,surrounding rocks,ore-controlling structures,and rock assemblages,this study identified one favorable condition and seven significant indicators for prospecting for Hongqiling-type nickel deposits and developed a prospecting model of the Hongqiling deposit.These serve as valuable references for exploring similar nickel deposits in the region,as well as the deep parts and margins of the Hongqiling deposit.

Nickel-copper-cobalt depositFractional crystallizationCrustal contaminationMagmaticMineralizationRe-Os isotopic ageSulfur isotopicMetallogenic modeProspecting modelWestern Pacific's active continental marginMineral exploration engineeringHongqil

Cong Chen、Yu-chao Gu、Di Zhang、Tao-tao Wu、Ai Li、Yun-sheng Ren、Qing-qing Shang、Jian Zhang、Xiong-fei Bian、Fei Su、Jia-lin Yang、Qiu-shi Sun、Xiao-hai Li、Wan-zhen Liu、Zhen-ming Sun、Sen Zhang、Yu-hui Feng

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Shenyang Center of China Geological Survey,Shenyang 110034,China

School of Earth Sciences and Resources,China University of Geosciences(Beijing),Beijing 100083,China

College of Computer Science & Technology,Qingdao University,Qingdao 266071,China

Institute of Disaster Prevention,Langfang 065200,China

College of Earth Sciences,Jilin university,Changchun 130000,China

Geological Survey Institute of Jilin Province,Changchun 130000,China

School of Surveying and Mapping Engineering,Changchun Institute of Technology,Changchun 130000,China

Physical Geological Materials Center of Natural Resources,China Geological Survey,Langfang 065200,China

Shenyang Normal University,Shenyang 110034,China

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2024

10.31035/cg2023106

中国地质(英文)
中国地质调查局,中国地质科学院

中国地质(英文)

CSTPCD
ISSN：2096-5192
年,卷(期)：2024.7(4)