| Registros del 1 al 10 de 19 encontrados |
1.- ACTIVE LATE CENOZOIC FLEXURES IN THE PRECORDILLERA IN NORTHERN CHILE; CORRELATIONS WITH THE SHALLOW SEISMIC ACTIVITY, AND IMPLICATIONS FOR THE UPLIFT OF THE ALTIPLANO
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2002
AGU 2002 FALL MEETING
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2.- Crack formation on top of propagating reverse faults of the Chuculay Fault System, northern Chile; insights from field data and numerical modelling
Elsevier; Oxford; III; International, 2008
Ver registro
3.- Crustal scale structural architecture in central Chile based on seismicity and surface geology; implications for Andean mountain building
American Geophysical Union; Washington, DC; USA; United States, 2010
Ver registro
4.- Dynamic topography and Neogene uplift of Patagonia
[International Geological Congress]; [location varies]; III; International, 2008
33rd international geological congress; abstracts
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5.- Dynamic topography control on Patagonian relief evolution as inferred from low temperature thermochronology
Elsevier; Amsterdam; NLD; Netherlands, 2013
Ver registro
6.- Effect of aseismic ridge subduction on slab geometry and overriding plate deformation; insights from analogue modeling
Elsevier; Amsterdam; NLD; Netherlands, 2013
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7.- Flat subduction dynamics and deformation of the South American Plate; insights from analog modeling
American Geophysical Union; Washington, DC; USA; United States, 2008
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8.- GEOMORPHOLOGICAL MARKERS OF FAULTING AND NEOTECTONIC ACTIVITY ALONG THE WESTERN ANDEAN MARGIN, NORTHERN CHILE
JOHN WILEY AND SONS FOR THE QUATERNARY RESEARCH ASSOCIATION; CHICHESTER; GBR; UNITED KINGDOM, 2003
Ver registro
9.- LATE CENOZOIC DEFORMATION AND UPLIFT OF THE WESTERN FLANK OF THE ALTIPLANO; EVIDENCE FROM THE DEPOSITIONAL, TECTONIC, AND GEOMORPHOLOGIC EVOLUTION AND SHALLOW SEISMIC ACTIVITY (NORTHERN CHILE AT 19 DEGREES 30'S)
AMERICAN GEOPHYSICAL UNION; WASHINGTON, DC; USA; UNITED STATES, 2005
Ver registro
10.- Late Cenozoic geomorphologic signal of Andean forearc deformation and tilting associated with the uplift and climate changes of the southern Atacama Desert (26 degrees S-28 degrees S)
Elsevier; Amsterdam; NLD; Netherlands, 2007
Ver registro
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