Rapid recharge of fresh water to the halite-hosted brine aquifer of Salar de Atacama, Chile

Author:

Boutt David F.1,Hynek Scott A.2,Munk Lee Ann3,Corenthal Lilly G.1

Affiliation:

1. Department of Geosciences; University of Massachusetts-Amherst; Amherst MA USA

2. Earth and Environmental Systems Institute; Pennsylvania State University; University Park PA USA

3. Department of Geological Sciences; University of Alaska-Anchorage; Anchorage AK USA

Publisher

Wiley

Subject

Water Science and Technology

Reference41 articles.

1. Sustainable groundwater development in arid, high Andean basins;Anderson;Geological Society London Special Publications,2002

2. Architecture and style of compressive Neogene deformation in the eastern-southeastern border of the Salar de Atacama Basin (22°30'-24°15'S): A structural setting for the active volcanic arc of the Central Andes;Aron;International Symposium on Andean Geodynamics,2008

3. Orographic barriers, high-resolution TRMM rainfall, and relief variations along the eastern Andes;Bookhagen;Geophysical Research Letters,2008

4. Determination of tritium by mass spectrometric measurement of 3He;Clarke;International Journal of Applied Radiation and Isotopes,1976

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