Citation: | 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, 2024. Geology and mineralization of the Hongqiling large magmatic nickel-copper-cobalt deposit (22×104 t) in Jilin Province, China: A review, China Geology, 7, 762-796. doi: 10.31035/cg2023106 |
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.
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Maps of the geotectonic location (a) and major deposit distribution of the study area (b; base maps modified from Wu FY et al., 2007; Xu ZG et al., 2008; Chen C, 2017).
Geolgical sketch map of the Hongqiling area (a; after Wu FY et al., 2004) and geological structure map of Hongqiling and its adjacent areas (b; after Ma JX et al., 1998).
Map showing the geochemical characteristics of Ni and the distributions of nickel deposits in the Jizhong-Yanbian metallogenic belt.
Geological map of the Hongqiling deposit in Panshi City, Jilin Province (after Sun YH et al., 2016).
Altered hornblende peridotites (a) and hornblende olivine pyroxenites (b) of the No.1 pluton and serpentinized peridotites (c) of the No. 33 pluton in rock belt I of the Hongqiling area. Cpx–Clinopyroxene; Hbl–Hornblende; Ol–Olivine; Srp–Serpentine; Tr–Tremolite.
Geological map and section of the No. 7 pluton in the Hongqiling deposit in Panshi City (modified from Qin K, 1995).
Geological map and cross section of the No. 1 pluton of the Hongqiling deposit in Panshi City (a after Team 607 of Jilin Nonferrous Metal Geological Exploration Bureau, 2008; b after Hao LB et al., 2014).
Geological map of the No. 2 pluton in the Hongqiling deposit (after Team 607 of Jilin Nonferrous Metal Geological Exploration Bureau, 2008).
Geological map (a) and cross section (b) of the No. 3 pluton in the Hongqiling deposit (modified from Li A, 2019).
Drilling verification results of Cu and Ni ores at the bottom of the No. 3 pluton in the Hongqiling deposit (after Xu ZH et al., 2022).
Microscopic images of primary ore minerals in the No. 1 pluton of the Hongqiling deposit. Ccp–Chalcopyrite; Sp–Cphalerite; Po-pyrrhotite; Pn–Pentlandite.
Histogram showing the diagenetic and metallogenic ages of major copper-nickel deposits on the northern margin of the North China Plate (data shown in Table 6).
Primitive mantle-normalized diagram of trace elements (a) and chondrite-normalized diagram of rare earth elements (b) for mafic-ultramafic rocks from the Nos. 1, 2, 3, and 7 plutons of the Hongqiling deposit (sample data from Li A, 2019).
Si/Ti vs. (Mg+Fe)/Ti and Nb/Yb vs. Th/Yb diagrams of predominant ore-bearing rocks in the Hongqiling deposit (after Li A, 2019).
Ba/La vs. Th/Yb (a) and Th/Zr vs. Nb/Zr (b) diagrams of mafic-ultramafic plutons in the Hongqiling deposit (base maps after Hanyu T et al., 2013 and Woodhead JD et al., 2001, respectively; sample data from Li A, 2019).
Diagram showing the metallogenic model of the Hongqiling copper-nickel deposit in Panshi City, Jilin Province (modified from Tang ZL et al., 1998; Xing SW et al. 2014).