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Reconstruction of the Yangtze Ramp during Floian to Darriwilian (Ordovician) in South China: Its Morphology, Controlling Factors and Significances
Institution:1 State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, and Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, Nanjing 210008, China 2 Department of Geological Science, University of Saskatchewan, Saskatoon, Saskatchewan S7N 5E2, Canada;3 Department of Earth and Environmental Sciences, University of Ottawa, Ottawa, Ontario K1N 6N5, Canada;4 Paleontology and Stratigraphy, School of Earth and Space Sciences, Peking University, Beijing 100871, China; 1 State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, and Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, Nanjing 210008, China 5 University of Chinese Academy of Sciences, Beijing 100049, China
Abstract:
Keywords:mixed siliciclastic-carbonate sedimentation  ramp  Stage Slice  lithofacies  major elements  Great Ordovician Biodiversification Event (GOBE)
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