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. 2020 Jun 8;117(25):14005–14014. doi: 10.1073/pnas.1916673117

Fig. 3.

Fig. 3.

Model of thermal history of the Doushantuo Formation from 635 Ma to present based on its regional tectonic history outlined in this study. See text for details. C, Carboniferous; Cz, Cenozoic; D, Devonian; ϵ, Cambrian; J, Jurassic; K, Cretaceous; O, Ordovician; P, Permian; S, Silurian; Tr, Triassic; Z, Ediacaran.