Published December 14, 2018
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FIG. 7 in Biostratigraphy and Diversity of Paleogene Perissodactyls from the Erlian Basin of Inner Mongolia, China
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FIG. 7. Paleogene outcrops in the Shara Murun region: A, the outcrops at Ula Usu, where the Shara Murun Formation was named, showing an upper member dominated by white sandstones and a lower member dominated by sandy clays with varied colors; B, the outcrops at Xilin Nor North (= 4 mi north of Baron Sog Lamasery), showing the red clays of the Ulan Gochu Formation overlying the grayish white sandstones of the upper part of the Shara Murun Formation.
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Published as part of Bai, Bin, Wang, Yuan-Qing, Li, Qian, Wang, Hai-Bing, Mao, Fang-Yuan, Gong, Yan-Xin & Meng, Jin, 2018, Biostratigraphy and Diversity of Paleogene Perissodactyls from the Erlian Basin of Inner Mongolia, China, pp. 1-60 in American Museum Novitates 2018 (3914) on page 28, DOI: 10.1206/3914.1, http://zenodo.org/record/10110870Files
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- Journal article: 10.1206/3914.1 (DOI)
- Journal article: urn:lsid:plazi.org:pub:FFFAFFF3FFB7504CFFA5FFEE8045FFA0 (LSID)
- Journal article: http://publication.plazi.org/id/FFFAFFF3FFB7504CFFA5FFEE8045FFA0 (URL)
- Journal article: https://zenodo.org/record/10110870 (URL)