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Tian'e Platform

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Stratigraphic cross section of Permian–Triassic boundary sections in the Gr...
in > PALAIOS
Published: 01 July 2015
Fig. 3.— Stratigraphic cross section of Permian–Triassic boundary sections in the Great Bank of Guizhou, Tian’e platform, and Chongzuo‐Pingguo platform. Section locations are shown in Figure 2 . Isotope data are found in online Supplementary Data file.
Image
Late Permian–Early Triassic paleogeography of the Nanpanjiang Basin and Yan...
in > PALAIOS
Published: 01 July 2015
Fig. 1.— Late Permian–Early Triassic paleogeography of the Nanpanjiang Basin and Yangtze Platform. Drowned upper Permian platforms in center of the basin are shown with light‐gray outline (Xilin, Leye, Lingyun, and Tian’e platforms). Field localities are as follows: HP = Heping, HC = Hochang, TW
Journal Article
Journal: PALAIOS
Published: 01 July 2015
PALAIOS (2015) 30 (7): 529–552.
...Fig. 3.— Stratigraphic cross section of Permian–Triassic boundary sections in the Great Bank of Guizhou, Tian’e platform, and Chongzuo‐Pingguo platform. Section locations are shown in Figure 2 . Isotope data are found in online Supplementary Data file. ...
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Journal Article
Published: 25 November 2013
Journal of the Geological Society (2014) 171 (2): 269–280.
... changes from abyssal dark green to black, thin-bedded chert intercalated with mudstone at Jiuxu ( Fig. 3 , sections E–G) to medium-bedded mudstone and siltstone with chert interlayers at Tian’e ( Fig. 3 , sections E–G) and to turbiditic sandstones and mudstones and calcirudites with mudstone and chert...
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Journal Article
Journal: GSA Bulletin
Published: 18 July 2017
GSA Bulletin (2018) 130 (1-2): 24–34.
... arc along the Cathaysian margin of southeastern China. Development of the Nanpanjiang basin was manifested by two contrasting depositional environments: isolated carbonate platforms and intervening deep-water turbidite depocenters ( Enos et al., 2006 ). Condensation dominated deep-water...
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Journal Article
Published: 01 September 2007
Journal of Paleontology (2007) 81 (5): 858–872.
..., 1959 , p. 75, pl. 15, figs. 3–5, text-fig. 23c) differ from the Guiding specimens by their thicker shell and subquadrate whorls. Proptychites kwangsiensis ( Chao, 1959 , p. 72, pl. 19, figs. 6, 7, text-fig. 23d) from the Flemingitan Bed at Tian'e, Guangxi, is readily distinguished from the Guiding...
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