Search Results - "Martino, R.D."
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Petrology and SHRIMP U–Pb zircon geochronology of Cordilleran granitoids of the Bariloche area, Argentina
Published in Journal of South American earth sciences (01-12-2011)“…A petrological and geochronological study of Cordilleran granitoid intrusions in the Bariloche area (Argentina) point to a complex time-compositional evolution…”
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A Middle Paleozoic shear zone in the Sierra de Valle Fértil, Argentina: Records of a continent-arc collision in the Famatinian margin of Gondwana
Published in Journal of South American earth sciences (01-12-2014)“…Geological, petrological and structural observations were obtained along a 30-km-long traverse across a segment of the Valle Fértil shear zone, central-western…”
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Geology and petrology of a deep crustal zone from the Famatinian paleo-arc, Sierras de Valle Fértil and La Huerta, San Juan, Argentina
Published in Journal of South American earth sciences (01-04-2009)“…The ranges of the Sierras Valle Fértil-La Huerta expose natural cross sections through a paleo-arc crust that formed in the Late Cambrian - Early Ordovician…”
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Anisotropy of magnetic susceptibility study in two classical localities of the Gastre Fault System, central Patagonia
Published in Journal of South American earth sciences (01-12-2010)“…The Central Patagonian Batholith is a suite of acid and meso-silicic rocks cropping out in central Patagonia. The emplacement of these rocks has been proposed…”
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Wavelength-dispersive spectral analysis and quantification of monazites by electron-probe microanalysis
Published in Spectrochimica acta. Part B: Atomic spectroscopy (2011)“…The problem of determining the chemical composition of monazite grains through electron probe microanalysis is studied, by using a scanning electron microscope…”
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Top-down structures of mafic enclaves within the Valle Fértil magmatic complex (Early Ordovician, San Juan, Argentina)
Published in Geologica acta (01-04-2009)“…Magmatic structures related to the mechanical interaction between mafic magmas and granitoids have been studied in the Valle Fértil calc-alkaline igneous…”
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