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Fig. 2 | Progress in Earth and Planetary Science

Fig. 2

From: From desert to monsoon: irreversible climatic transition at ~ 36 Ma in southeastern Tibetan Plateau

Fig. 2

A Cenozoic geology map of Jianchuan Basin; B lithostratigraphy of Cenozoic successions of Jianchuan Basin, with emphasis on sedimentary facies; C Yunlong Formation showing red weathered siltstones interbedded with minor sandstones and conglomerates; D Red, thin to medium bedded sandstones interbedded with conglomerates of the Baoxiangsi Formation; E Massive think-bedded conglomerates of Baoxiangsi Formation; F Poorly sorted fanglomerate and sandstones of the Baoxiangsi Formation; G Upper Baoxiansi Formation, showing dark red, thick-bedded sandstones with large-scale, high-angle trough and planar cross-bedding; H Stacked, thick-bedded typical pale colored sandstones of the Jinsichang Formation; I Massive thick-bedded limestone of the Jiuziyan Formation, and stromatolites within the limestone (I’); J, Shuanghe Formation, showing coals with interbedded fine sandstones, siltstones, shales, and volcano-sedimentary rocks

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