Sha, J., State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Paleontology, Nanjing, 210008, China; Olsen, P.E., Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10968, United States; Pan, Y., State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Paleontology, Nanjing, 210008, China; Xu, D., Institute of Geology, China Earthquake Administration, Beijing, 100029, China; Wang, Y., State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Paleontology, Nanjing, 210008, China; Zhang, X., Chinese Academy of Sciences Key Laboratory of Crust-Mantle Materials and Environments, School of Earth and Space Sciences, University of Science and Technology of China, Heifei, 230026, China; Yao, X., State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Paleontology, Nanjing, 210008, China; Vajda, V., Department of Geology, Lund University, Lund, 223 62, Sweden, Department of Palaeobiology, Swedish Museum of Natural History, Stockholm, 104 05, Sweden
Recommended Citation:
Sha J.,Olsen P.E.,Pan Y.,et al. Triassic-Jurassic climate in continental high-latitude Asia was dominated by obliquity-paced variations (Junggar Basin; Ürümqi; China)[J]. Proceedings of the National Academy of Sciences of the United States of America,2015-01-01,112(12)