Mountain building results in high erosion rates and the interaction of rocks with the
atmosphere, water and life. Carbon transfers that result from increased erosion could control …

The surface uplift history of the Tibetan Plateau (TP) offers a key testing ground for
evaluating models of collisional tectonics and holds important implications for processes …

Global cooling in the Cenozoic, which led to the growth of large continental ice sheets in
both hemispheres, may have been caused by the uplift of the Tibetan plateau and the …

Weathering of uplifted continental rocks consumes carbon dioxide and transports cations to
the oceans, thereby playing a critical role in controlling both seawater chemistry and climate …

Thermochronologic, sedimentologic, oceanographic, and paleoclimatic studies suggest that
rapid uplift and unroofing of southern Tibet began about 20 million years ago and that the …

The recent proliferation of stratigraphic studies of δ13C variation in carbonates and organic
C in later Neoproterozoic and basal Cambrian successions (∼ 850-530 Ma) indicates a …

The elevation of the Tibetan plateau is a revolutionary event in the Earth history, which
resulted in change not only of Cenozoic regional and global climate but also of monsoon …

A range of ages have been proposed for the timing of India‐Asia collision; the range to some
extent reflects different definitions of collision and methods used to date it. In this paper we …

The strontium (Sr) isotope method can be a powerful tool in studies of chemical weathering
and soil genesis, cation provenance and mobility, and the chronostratigraphic correlation of …

Revision of the GEOCARB model (Berner, 1991, 1994) for paleolevels of atmospheric CO~
2~, has been made with emphasis on factors affecting CO~ 2~ uptake by continental …