Response of meteoric δ18O to surface uplift — Implications for Cenozoic Andean Plateau growth
- 1 February 2012
- journal article
- research article
- Published by Elsevier BV in Earth and Planetary Science Letters
- Vol. 317-318, 262-272
- https://doi.org/10.1016/j.epsl.2011.11.039
Abstract
No abstract availableKeywords
This publication has 41 references indexed in Scilit:
- Impacts of Cenozoic global cooling, surface uplift, and an inland seaway on South American paleoclimate and precipitation 18OGSA Bulletin, 2011
- Sedimentology-based reconstructions of paleoclimate changes in the Central Andes in response to the uplift of the Andes, Arica region between 19 and 21°S latitude, northern ChileInternational Journal of Earth Sciences, 2010
- Late Miocene climate variability and surface elevation in the central AndesEarth and Planetary Science Letters, 2010
- End member models for Andean Plateau upliftEarth-Science Reviews, 2009
- Response to Comment on "Rapid Uplift of the Altiplano Revealed Through 13 C- 18 O Bonds in Paleosol Carbonates"Science, 2006
- Comment on "Rapid Uplift of the Altiplano Revealed Through 13 C- 18 O Bonds in Paleosol Carbonates"Science, 2006
- Neogene and Quaternary history of vegetation, climate, and plant diversity in AmazoniaQuaternary Science Reviews, 2000
- Topographic development of the Southern Alps recorded by the isotopic composition of authigenic clay minerals, South Island, New ZealandChemical Geology, 1999
- Water isotope module of the ECHAM atmospheric general circulation model: A study on timescales from days to several yearsJournal of Geophysical Research: Atmospheres, 1998
- Origin of the high plateau in the central Andes, Bolivia, South AmericaTectonics, 1997