(ITPCAS OpenIR): Rock magnetic constraints for the Mid-Miocene Climatic Optimum from a high-resolution sedimentary sequence of the northwestern Qaidam Basin, NE Tibetan Plateau
(ITPCAS OpenIR): Rock magnetic constraints for the Mid-Miocene Climatic Optimum from a high-resolution sedimentary sequence of the northwestern Qaidam Basin, NE Tibetan Plateau : Forgotten Password? Stay signed in , Cancel Log In Log In Cancel Chinese | English Image search Paste the image URL Home Collections Authors DocType Subjects K-Map News ITPCAS OpenIR > Start a Submission Submissions Unclaimed Claimed Attach Fulltext Bookmarks QQ Weibo Feedback Rock magnetic constraints for the Mid-Miocene Climatic Optimum from a high-resolution sedimentary sequence of the northwestern Qaidam Basin, NE Tibetan Plateau Guan, C (Guan, Chong) 1,5 ; Chang, H (Chang, Hong) 3,4,5 ; Yan, MD (Yan, Maodu) 1,2,5 ; Li, LY (Li, Leyi) 3,5 ; Xia, MM (Xia, Mengmeng) 6 ; Zan, JB (Zan, Jinbo) 1,2,5 ; Liu, SC (Liu, Shuangchi) 7 Source Publication PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 2019 Volume 532 Issue: 0 Pages: 109263 DOI 10.1016/j.palaeo.2019.109263 Abstract The thick sequence of Cenozoic deposits