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1.- Evolution of the landforms across which the Atacama Desert is draped, 20 degrees -24 degrees S latitude
Geological Society of America (GSA); Boulder, CO; USA; United States, 2006
Geological Society of America, 2006 annual meeting
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2.- Late Pleistocene organic remains in Pampa del Tamarugal, northern Chile (21 degrees S); implications for past precipitation changes in the western Precordillera
Geological Society of America (GSA); Boulder, CO; USA; United States, 2006
Geological Society of America, 2006 annual meeting
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3.- Structural, topographic and climatic control on sedimentation and facies distribution in a hyper-arid, nonmarine forearc basin, Atacama Desert, northern Chile
American Association of Petroleum Geologists and Society for Sedimentary Geology; Tulsa, OK; USA; Un, 2005
AAPG 2005 annual convention; abstracts volume
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