DOCSLIB.ORG
Explore
Sign Up
Log In
Upload
Search
Home
» Tags
» Sajsi
Sajsi
Vegetation and Fire at the Last Glacial Maximum in Tropical South America
Bildnachweis
Prospecting Glacial Ages and Paleoclimatic Reconstructions Northeastward of Nevado Coropuna (16◦ S, 73◦ W, 6377 M), Arid Tropical Andes
Antarctic-Like Temperature Variations in the Tropical Andes Recorded by Glaciers and Lakes During the Last Deglaciation L
Baker-Fritzqsr2015.Pdf
Palaeogeographic Reconstruction of Minchin Palaeolake System, South America: the Influence of Astronomical Forcing
Paper Accepted. Pre-Print Version
Last Local Glacial Maximum and Deglaciation of the Andean Central Volcanic Zone: the Case of Hualcahualca Volcano and Patapampa Altiplano (Southern Peru)
1 La Evolución Glaciovolcánica Del
Isotopic Tracers of Paleohydrologic Change in Large Lakes of the Bolivian Altiplano
Forzamiento Astronómico En El Neógeno De La Tierra Y
Stratigraphy, Geochronology, and Geochemistry Of
Geochronology and Stratigraphy of Late Pleistocene Lake Cycles on the Southern Bolivian Altiplano: Implications for Causes of Tropical Climate Change
Applied Ocean Science and Engineering
The Deglaciation of the Americas During the Last Glacial Termination', Earth-Science Reviews, Vol
Prospección De Edades 36Cl De La Última Máxima Expansión De Los
Download File
Landscape Response to Pleistoceneholocene Precipitation
Top View
Pfeiffer-Etal-2018-Qsr-1.Pdf
Late Quaternary Stratigraphy, Sedimentology and Geochemistry of an Underfilled Lake Basin in the Puna Plateau (Northwest Argentina) Michael M
The Deglaciation of the Americas During the Last Glacial Termination
36Cl Chronologies and ELA Reconstructions from the Northern Boundary of the South American Arid Diagonal
Redalyc.Palynological Evidence of the Geoecological Belts Dynamics from Eastern Cordillera of NW Argentina (23° S) During the P
Cuadernos De Investigación Geográfica / Geographical
Palynological Evidence of the Geoecological Belts Dynamics from Eastern Cordillera of NW Argentina (23° S) During the Pre-Last Glacial Maximum
Late Local Glacial Maximum in the Central Altiplano Triggered by Cold and Locally-Wet Conditions During the Paleolake Tauca Episode (17–15 Ka, Heinrich 1)