Carbon and oxygen isotopic constraints on paleoclimate and paleoelevation of the southwestern Qaidam basin, northern Tibetan Plateau

We investigate the growth of the northern Tibetan Plateau and associated climate change by applying oxygen and carbon isotopic compositions in Cenozoic strata in the southwestern Qaidam basin. The X-ray diffraction and isotopic studies reveal that the carbonate minerals are mainly authigenic and the...

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Main Authors: Lin-Lin Li, Chao-Dong Wu, Chang-Fu Fan, Ji-Jun Li, Chang-Hao Zhang
Formato: Artigo
Idioma:Inglês
Publicado: Elsevier 2017-09-01
Series:Geoscience Frontiers
Assuntos:
Carbon and oxygen isotopes
Northern Tibetan Plateau
Qaidam basin
Paleoelevation
Acceso en liña:http://www.sciencedirect.com/science/article/pii/S1674987116302134
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