| Citation: | LIN Zihan，XIA Yuan，ZHANG Hangchuan，et al. Structural features of south Hubei Province along the northern of the Mufushan pluton structural ore-controlling of polymetallic deposits[J]. Bulletin of Geological Science and Technology，2025，44（2）：1-13 doi: 10.19509/j.cnki.dzkq.tb20230525
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An intensive Early Cretaceous magmatic-hydrothermal metallogenic system developed in the Mufushan area of the central Jingnan Orogen. This orogenic belt in the South China Block formed through the accretion and subsequent collision of the Yangtze and Cathaysia blocks during the early Neoproterozoic, resulting in the formation of rare metal deposits (Li-Be-Cs-Nb-Ta) and nonferrous metal deposits (Pb-Zn-Cu-Au-Sb).
This study investigates the structural control of polymetallic deposits in southern Hubei Province utilizing structural analysis, paleostress inversions of fault-slip data, and the spatial distribution of polymetallic ore deposits.
Structural analysis revealed that the Jiangnan fault, striking E-W and originating in the Neoproterozoic, exhibits Triassic top-to-the-north thrusting, Late Cretaceous oblique normal faulting, and Paleogene left-lateral strike-slip motion. The NE-striking Changping fault, formed during the Middle Jurassic Yanshanian orogeny, shows evidence of late Early Cretaceous left-lateral strike-slip motion, late Cretaceous normal faulting, and late Paleogene right-lateral strike-slip motion. Paleostress inversions indicate that southern Hubei Province experienced a series of paleostress fields, including a strike-slip stress field (with maximum principal stress oriented N-S and minimum principal stress oriented N-S) during the late Early Cretaceous, an NW-SE extensional stress field during the late Cretaceous, another strike-slip stress field (with maximum principal stress oriented NE-SW and minimum principal stress oriented N-S) during the early Paleogene, and a NE-SW extensional stress field during the late Paleogene.
Based on the polymetallic deposits in the study area, we conclude that secondary faults subparallel to the primary NE-SW trending fault, along with NW-SE and E-W trending faults intersecting with the primary NE-SW fault, present substantial potential for polymetallic mineral exploration.
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