Abstract The Middle to Late Miocene uplift of the northern Tibetan Plateau had been
revealed in a large amount of studies, however, its effects on hydrological and climatic …

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 …

To investigate climate evolution during the Miocene, especially during the Middle Miocene
climate transition on the northeastern Tibetan Plateau, stable oxygen and carbon isotopes of …

The topographic history of mountain belts reflects changes in lithospheric structure and
rheology and exerts an influence on climate. Although substantial progress has been made …

Carbon and oxygen stable isotopic composition of Cenozoic lacustrine carbonates from the
intramontane Qaidam Basin yields cycles of variable length and shows several distinct …

Lithologic, magnetostratigraphic, and stable isotope records from the Neogene Xunhua and
Linxia basins along the Tibetan Plateau's northeastern margin suggest that topography in …

There is much debate regarding the temporal and spatial pattern of hydroclimate variations
on the Tibetan Plateau during the Holocene, focusing especially on the dipolar pattern of …

Debates persist about the interpretations of stable isotope based proxies for the surface
uplift of the central–northern Tibetan Plateau. These disputes arise from the uncertain …

Post-middle Miocene changes in climate and ecology in the northern Tibetan Plateau have
been attributed to tectonic uplift and global climate change. However, the relative roles of …

Palaeoelevation reconstructions of mountain belts have become a focus of modern science
since surface elevation provides crucial information for understanding both geodynamic …