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作 者:Xinfa Li Guobiao Li
机构地区:[1]State Key Laboratory of Environmental Geology and Biogeology, China University of Geosciences, Beijing, China [2]School of Earth Sciences and Resources, China University of Geosciences, Beijing, China
出 处:《Open Journal of Geology》2019年第10期566-568,共3页地质学期刊(英文)
摘 要:Cretaceous radiolarians were firstly reported from the Eocene Sand-Shale Member of Zhepure Formation in the Gulupu section, Tüna, Yadong, Tibet. In spite of poor preservation, 24 species of 14 radiolarian genera have still been identified, clearly indicating an age, ranging from early Aptian–Maastrichtian, and therefore should have occurred in the Eocene as a result of redeposition. The study of the stratigraphic origin of these radiolarians will shed light on the paleoenvironment and late evolutionary history of the Tibet-Tethys.Cretaceous radiolarians were firstly reported from the Eocene Sand-Shale Member of Zhepure Formation in the Gulupu section, Tüna, Yadong, Tibet. In spite of poor preservation, 24 species of 14 radiolarian genera have still been identified, clearly indicating an age, ranging from early Aptian–Maastrichtian, and therefore should have occurred in the Eocene as a result of redeposition. The study of the stratigraphic origin of these radiolarians will shed light on the paleoenvironment and late evolutionary history of the Tibet-Tethys.
关 键 词:CRETACEOUS Redeposited RADIOLARIANS EOCENE Zhepure Formation PALEOENVIRONMENT Yadong
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