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• W1752809513 abstract "AbstractFluid dynamical and numerical modelling predicts a large-scale regional domal uplift prior to basalt eruptions in large igneous provinces, which can be readily measured when a plume head rises below a shallow marine sedimentary basin. Research on the sedimentology, biostratigraphy, and isotopic chronology of the Emeishan large igneous province demonstrates that the sedimentary environment in the Maokou stage is not uniform carbonate platform facies, but rather sedimentary facies with a north–south linear alignment and west–east different distribution controlled by the syn-depositional normal faulting of the Changhai and Xiaojiang faults, which are the result of underwater dynamic uplift induced by deep mantle activity. The dynamic uplift started in the Maokou stage. Thus, thinning of the Maokou limestone was the product of the difference in the initial depositional thickness caused by the underwater uplift and post-depositional surface uplift and erosion, but post-depositional uplift was much less..." @default.
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• W1752809513 date "2015-07-20" @default.
• W1752809513 modified "2023-10-17" @default.
• W1752809513 title "Stratigraphic records of the dynamic uplift of the Emeishan large igneous province" @default.
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• W1752809513 doi "https://doi.org/10.1080/00206814.2015.1065515" @default.
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