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Pablo Diego González

Researcher at National Scientific and Technical Research Council

Publications -  72
Citations -  955

Pablo Diego González is an academic researcher from National Scientific and Technical Research Council. The author has contributed to research in topics: Basement (geology) & Gondwana. The author has an hindex of 16, co-authored 72 publications receiving 809 citations. Previous affiliations of Pablo Diego González include National University of Río Negro & National University of La Plata.

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Evolución del orógeno Famatiniano en la Sierra de San Luis: magmatismo de arco, deformación y metamorfismo de bajo a alto grado

TL;DR: In this article, a review of the igneous-metamorphic basement of the Sierra de San Luis is presented, where the authors recognize the following three-stage evolution: (1) Pre-Famatinian processes: Initial siliciclastic sedimentation, with interbedded mafic to ultramafic lavas and banded iron formations.
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Accretion of Grenvillian terranes to the southwestern border of the Río de la Plata craton, western Argentina

TL;DR: A comprehensive review of the geological, geochronological, and isotopic features of the Mesoproterozoic Grenvillian terranes attached to the southwest of the Rio de la Plata craton in Early Paleozoic times is presented in this article.
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Early Cambrian archaeocyathan limestone blocks in low-grade meta-conglomerate from El Jagüelito Formation (Sierra Grande, Río Negro, Argentina)

TL;DR: In the El Jaguelito Formation (Sierra Grande area, Eastern North Patagonian Massif, Rio Negro, Argentina) as discussed by the authors, seven different taxa were identified, preliminary described and figured.
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Patagonia-Antarctica Early Paleozoic conjugate margins: Cambrian synsedimentary silicic magmatism, U-Pb dating of K-bentonites, and related volcanogenic rocks

TL;DR: In this article, the authors describe the stratigraphic features, petrology and geochemistry and geochronology constraints of K-bentonites, ignimbrites and related volcanogenic rocks interbedded in the marine sedimentary sequence of the El Jaguelito Formation from northern Patagonia basement, southwestern Gondwana margin (41°33′S-65°15′W, South America).
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Constraints on the Origin and Evolution of Magmas in the Payún Matrú Volcanic Field, Quaternary Andean Back-arc of Western Argentina

TL;DR: Hernando et al. as mentioned in this paper presented the Centro de Investigaciones Geologicas (CIGG) at the Consejo Nacional de Investigación Cientifica y Tecnologia (Conicet) in La Plata.