A5007399257- Geological and Geochemical Analysis
- Geochemistry and Geologic Mapping
- Geological and Geophysical Studies Worldwide
- Paleontology and Stratigraphy of Fossils
- Geochemistry and Elemental Analysis
- Geological and Tectonic Studies in Latin America
- Geological formations and processes
- earthquake and tectonic studies
- Geology and Paleoclimatology Research
- High-pressure geophysics and materials
- Evolution and Paleontology Studies
- Environmental and Ecological Studies
- Archaeological and Geological Studies
- Plant Diversity and Evolution
- Fish biology, ecology, and behavior
- Paleontology and Evolutionary Biology
- Clay minerals and soil interactions
- Geomagnetism and Paleomagnetism Studies
- Botanical Research and Applications
- Pleistocene-Era Hominins and Archaeology
- Historical and socio-economic studies of Spain and related regions
- Hydrocarbon exploration and reservoir analysis
- Botany and Geology in Latin America and Caribbean
- Health and Medical Education
- Historical Studies in Science
Universidad Nacional de La Plata
2010-2024
Consejo Nacional de Investigaciones Científicas y Técnicas
2008-2023
Centro Científico Tecnológico - La Plata
1999-2012
Instituto de Geociencias
2010
Universidade de São Paulo
2010
Centro Científico Tecnológico - San Juan
2010
Centro Científico Tecnológico - Tucumán
2005
National Meteorological Service
1982
University of Chile
1982
Instituto de Geocronología y Geología Isotópica
1982
Research Article| July 01, 1992 Early Paleozoic orogenic belt of the Andes in southwestern South America: Result Laurentia-Gondwana collision? Luis Dalla Salda; Salda 1Universidad Nacional de La Plata, Calle 1 N 644, 1900 Argentina Search for other works by this author on: GSW Google Scholar Carlos Cingolani; Cingolani Ricardo Varela Author and Article Information Publisher: Geological Society America First Online: 02 Jun 2017 Online ISSN: 1943-2682 Print 0091-7613 Geology (1992) 20 (7):...
Research Article| December 01, 1992 Did the Taconic Appalachians continue into southern South America? Luis H. Dalla Salda; Salda 1Centro de Investigaciones Geologicas, Universidad Nacional La Plata, Calle 1, no. 644, 1900 Argentina Search for other works by this author on: GSW Google Scholar Ian W. D. Dalziel; Dalziel 2Institute Geophysics, University of Texas, 8701 Mopac Boulevard, Austin, Texas 79759 Carlos A. Cingolani; Cingolani Ricardo Varela Author and Article Information Publisher:...
Se presentan los resultados obtenidos en el estudio isotopico de rocas del basamento igneo-metamorfico Andes expuesto Argentina, aproximadamente a 40°S, las provincias Neuquen y Rio Negro. Fueron utilizadas metodologias isotopicas, para obtener informacion sobre la edad emplazamiento cuerpos igneos deformados ductilmente (U-Pb circones), tiempo enfriamiento luego procesos metamorficos que modelaron este (K-Ar micas; U-Pb titanita) historia cortical involucrada (Sm-Nd roca total). No se...
The superposition of two orogenies during the evolution Paleoproterozoic Tandilia Belt, Argentina, produced complex geological structures in granitic-gneissic-migmatitic Buenos Aires Complex. Ion microprobe (SHRIMP II) dating 61 spots 56 zircon crystals from 10 rock samples shows tectonic activity related to accretionary Encantadas orogeny 2.25-2.12 Ga, although a major overprint collisional Camboriú 2.10-2.08 Ga is also recognized. Only one age Neoarchean. Two peaks for Belt are ~2.16 and...
Abstract Ordovician K-bentonites have now been recorded from >20 localities in the vicinity of Argentine Precordillera. Most occur eastern thrust belts, San Juan Limestone and overlying Gualcamayo Formation, but a few ash beds are known also central belts. The oldest middle Arenig I. victoriae lunatus graptolite ( Oe. evae conodont) Zone, youngest Llanvirn P. elegans suecicus ) Zone. Mineralogical characteristics, typical other K-bentonites, include matrix illite/smectite mixed-layer clay...
Bed-by-bed collecting of the La Chilca Formation at Talacasto, San Juan, Argentina has revealed a sequence spanning Ordovician–Silurian boundary, and recognition following graptolite zones: Glyptograptus persculptus , probable Parakidograptus acuminatus possible Atavograptus. The Talacasto section thus allows closest definition boundary in South America. shales are 3.65 m thick, rich graptolites, have allowed us to recognize for first time America several stratigraphically important forms:...