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Volume 32 Issue 1
Mar 2021
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Rui Cao, Xinghua Ma, Leon Bagas, Yongbao Gao, Demin Liu, Zailai Mou. Late Jurassic Intracontinental Extension and Related Mineralisation in Southwestern Fujian Province of SE China: Insights from Deformation and Syn-Tectonic Granites. Journal of Earth Science, 2021, 32(1): 158-173. doi: 10.1007/s12583-020-1387-6
Citation: Rui Cao, Xinghua Ma, Leon Bagas, Yongbao Gao, Demin Liu, Zailai Mou. Late Jurassic Intracontinental Extension and Related Mineralisation in Southwestern Fujian Province of SE China: Insights from Deformation and Syn-Tectonic Granites. Journal of Earth Science, 2021, 32(1): 158-173. doi: 10.1007/s12583-020-1387-6

Late Jurassic Intracontinental Extension and Related Mineralisation in Southwestern Fujian Province of SE China: Insights from Deformation and Syn-Tectonic Granites

doi: 10.1007/s12583-020-1387-6
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  • Corresponding author: Xinghua Ma, maxh@pku.edu.cn
  • Received Date: 28 Apr 2020
  • Accepted Date: 06 Dec 2020
  • Publish Date: 01 Feb 2021
  • Late Mesozoic igneous intrusions and extensional structures in Carboniferous to Permian sequences in the SW Fujian region acted as important controls on the localisation of Fe-polymetallic deposits. Here we document the identification of extensional deformation at shallow crustal levels and syn-tectonic granites related to normal faults. Based on spatial distribution and structural features, the extensional deformation can be divided into cover-only and basement-intersecting styles. A series of syn-tectonic plutons were emplaced into the footwall of normal faults. Representative samples of the Tangquan Granite have high SiO2 (66.4 wt.%-73.9 wt.%) assays and Mg# values (37-59). The samples also have relatively homogenous initial 87Sr/86Sr (0.708 3-0.708 9) and εNd (-9.2--10.2) values. Geochemical and isotopic evidences indicate that the Tangquan granite originates from a hybrid source including lower crustal-derived felsic and lithospheric mantle-derived mafic magmas. Zircon U-Pb dating indicates that the granodiorite phase from the pluton crystallised at 161±4 Ma and the monzogranite phase crystallised at 159±1 Ma. Combined with the granitic rocks in a wider region of SE China, the widespread granitic magmatism and polymetallic mineralisation have been synchronous during the Late Mesozoic, probably resulting from extensional tectonics related to the lithospheric thinning.

     

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