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- W2907290480 abstract "Huojihe is a representative porphyry Mo deposit in the Lesser Xing'an Range, Northeast China. The major magmatic rocks in the ore district include granodiorite, porphyritic granodiorite, and monzogranite. Most of the orebodies are hosted within the granodiorite, with minor within the monzogranite. LA-ICP-MS zircon UPb dating of the granodiorite, porphyritic granodiorite, and monzogranite yields crystallization ages of 184.8 ± 1.2 Ma, 184.9 ± 1.3 Ma, and 182.1 ± 1.9 Ma, respectively. The ReOs model ages of the molybdenite range from 182.4 to 179.2 Ma. Combined with the petrological evidences and previously published age data, we suggest that the granodiorite and porphyritic granodiorite are different lithofacies of the same pluton, and the Huojihe Mo deposit experienced two epoches of mineralization related to the granodiorite (ca. 185 Ma) and the monzogranite (ca. 182 Ma), respectively. The granodiorite and monzogranite display consistent (87Sr/86Sr)i ratios of 0.70677 to 0.70746, εNd(t) values of −2.1 to −0.5, εHf(t) values of 0.5 to 7.7, and two-stage Nd and Hf model ages from 1167 to 711 Ma, indicating that they were generated by partial melting of a mixed source containing mantle-derived juvenile materials and pre-existed lower crust. The magmatism and mineralization in the Huojihe Mo deposit were resulted from collision of the Jiamusi and Songnen Blocks in response to the subduction of the Paleo-Pacific plate. Multistage magmatism is beneficial for magmatic-related mineralizaiton because it can result in the coupling of favorable structures, heat energy, and ore-forming materials." @default.
- W2907290480 created "2019-01-11" @default.
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- W2907290480 date "2019-02-01" @default.
- W2907290480 modified "2023-10-03" @default.
- W2907290480 title "Multistage magmatism resulting in large-scale mineralizaion: A case from the Huojihe porphyry Mo deposit in NE China" @default.
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- W2907290480 doi "https://doi.org/10.1016/j.lithos.2018.12.036" @default.
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