[HTML][HTML] Coupled tectonic evolution of Andean orogeny and global climate

R Armijo, R Lacassin, A Coudurier-Curveur… - Earth-Science …, 2015 - Elsevier
The largest tectonic relief breaking the Earth's surface (13 km vertically) is at the subduction
margin of the Andes, which generates routinely megathrust earthquakes (Mw> 8.5) and …

River terraces and alluvial fans: The case for an integrated Quaternary fluvial archive

AE Mather, M Stokes, E Whitfield - Quaternary Science Reviews, 2017 - Elsevier
The fluvial archive literature is dominated by research on river terraces with appropriate
mention of adjacent environments such as lakes. Despite modern sedimentary basins …

Atmospheric origins of perchlorate on Mars and in the Atacama

DC Catling, MW Claire, KJ Zahnle… - Journal of …, 2010 - Wiley Online Library
Isotopic studies indicate that natural perchlorate is produced on Earth in arid environments
by the oxidation of chlorine species through pathways involving ozone or its photochemical …

Landscape modification in response to repeated onset of hyperarid paleoclimate states since 14 Ma, Atacama Desert, Chile

TE Jordan, NE Kirk-Lawlor, NP Blanco, JA Rech… - …, 2014 - pubs.geoscienceworld.org
The landscape of the hyperarid Atacama Desert in northern Chile records extremely slow
change on Earth's surface. Disputed ages for the onset of hyperaridity range from the late …

Climatic fluctuations in the hyperarid core of the Atacama Desert during the past 215 ka

B Ritter, V Wennrich, A Medialdea, D Brill, G King… - Scientific Reports, 2019 - nature.com
Paleoclimate records from the Atacama Desert are rare and mostly discontinuous, mainly
recording runoff from the Precordillera to the east, rather than local precipitation. Until now …

Uplift of the Altiplano‐Puna plateau: A view from the west

TE Jordan, PL Nester, N Blanco, GD Hoke, F Dávila… - …, 2010 - Wiley Online Library
The western flank of the Central Andean Plateau is a crustal‐scale monoclinal fold,
expressed in the geomorphology and in the westward tilt of fore‐arc basin strata. Data from …

The spatial distribution of soluble salts in the surface soil of the Atacama Desert and their relationship to hyperaridity

C Voigt, S Klipsch, D Herwartz, G Chong… - Global and Planetary …, 2020 - Elsevier
We systematically investigated the spatial distribution of sulfates, chlorides, and nitrates in
Atacama Desert soils in order to identify their relationship to long-term aridity gradients and …

The relationships between tectonics, climate and exhumation in the Central Andes (18–36 S): Evidence from low-temperature thermochronology

NF Stalder, F Herman, MG Fellin, I Coutand… - Earth-Science …, 2020 - Elsevier
Abstract The Central Andes between 18° S and 36° S latitude strike north-south for 2000 km
along the Chilean subduction margin, cross several climate zones from hyperarid to humid …

Review of erosion dynamics along the major NS climatic gradient in Chile and perspectives

S Carretier, V Tolorza, V Regard, G Aguilar… - Geomorphology, 2018 - Elsevier
Chile is an elongated country, running in a north-south direction for more than 30° along a
subduction zone. Its climate is progressively wetter and colder from north to south. This …

Geomorphology on geologic timescales: Evolution of the late Cenozoic Pacific paleosurface in Northern Chile and Southern Peru

LA Evenstar, AE Mather, AJ Hartley, FM Stuart… - Earth-Science …, 2017 - Elsevier
Abstract The Atacama Desert on the western margin of the Central Andes is one of the driest
and oldest deserts in the world. It is defined by a distinct and ancient surface, known as the …