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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...

पूर्ण विवरण

में बचाया:
ग्रंथसूची विवरण
मुख्य लेखकों: Lin-Lin Li, Chao-Dong Wu, Chang-Fu Fan, Ji-Jun Li, Chang-Hao Zhang
स्वरूप: Artigo
भाषा:Inglês
प्रकाशित: Elsevier 2017-09-01
श्रृंखला:Geoscience Frontiers
विषय:
ऑनलाइन पहुंच:http://www.sciencedirect.com/science/article/pii/S1674987116302134
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