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| Citation: | Zeng Guoping, Hu Xinlu, Yao Shuzhen, Dong Ziliang, Zhou Ming, Yang Jian, 2022. Two Epochs of Mo Mineralization in Cuihongshan Fe-Mo-Polymetallic Ore field, Heilongjiang Province. Earth Science, 47(1): 309-324. doi: 10.3799/dqkx.2021.089
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Cuihongshan Fe-Mo-polymetallic ore field in Heilongjiang Province belongs to the Lesser Xing'an Range-Zhangguangcailing Fe-polymetallic metallogenic belt, and is characterized by the large-scale mineralization of Fe, Pb, Zn, Mo and W. Among them, Mo mineralization is the most noticeable, with three mineralization styles, including skarn-porphyry Mo-W, porphyry Mo-only, and cryptoexplosion breccias Mo, coexisting in a single ore field. However, the mineralization characteristics and spatio-temporal relationship of the three Mo mineralization types have not been systematically analyzed, and the Mo mineralization events have not been clearly defined. In this paper, the Cuihongshan, Huojihe and Hongtieshan Mo (polymetallic) deposits were selected for the geological characteristics analyses. Combining the geological characteristics with molybdenite Re-Os dating, two Mo mineralization events in Cuihongshan ore field were defined, including the Late Triassic skarn-porphyry Mo-Wand cryptoexplosion Mo mineralization and the Early Jurassic porphyry Mo-only mineralization. The Re content of molybdenite and petrogenesis of ore-forming magma reveal that Mo in Cuihongshan ore field were derived from a mixed source containing mantle-derived juvenile materials and ancient crustal components. And compared with the Late Triassic mineralization, more mantle-derived juvenile materials were involved during the Early Jurassic mineralization. Based on the mineralization characteristics and ore-forming material source analysis, the Mo mineralization is suggested to be related to the collision process between Songnen block and Jiamusi block during Late Triassic to Early Jurassic.
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