Timing of seawater retreat from proto-Paratethys, sedimentary provenance, and tectonic rotations in the late Eocene-early Oligocene in the Tajik Basin, Central Asia
Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China; CAS Center for Excellence in Tibetan Plateau Earth Sciences, Chinese Academy of Sciences, Beijing, 100101, China; University of Chinese Academy of Sciences, Beijing, 100049, China; Department of Geology, University of Leicester, Leicester, LEI 7RH, United Kingdom; Nanjing Institute of Geology and Paleontology, Chinese Academy of Sciences, Nanjing, 210008, China; Institute of Geology, Earthquake Engineering and Seismology of the Academy of Sciences, Tajikistan
Recommended Citation:
Sun J.,Zhang Z.,Cao M.,et al. Timing of seawater retreat from proto-Paratethys, sedimentary provenance, and tectonic rotations in the late Eocene-early Oligocene in the Tajik Basin, Central Asia[J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2020-01-01,545