Weathering profiles in granites, Sierra Norte (Córdoba, Argentina) By Alicia Matilde Kirschbaum, Estela Martínez, Gisela Roxana Pettinari and Silvana Andrea Herrero. Cite . BibTex ; Full citation; Abstract. Abstract: Two weathering profiles evolved on peneplainrelated granites in Sierra Norte, Córdoba province, were examined. Several weathering levels, of no more than 2 m thickness, were
WhatsAppArgentina, granites in China, and pegmatites in Australia, China, and Zimbabwe. An important aspect of the lithium R areelement granitic pegmatites are well recognized for the diversity and concentrations of metal ores that they host. The supply of some of these elements is of concern, and the European Commission recently designated metals such as tantalum and niobium as "critical materials
WhatsAppThree granitoid types are recognised in the Famatinian magmatic belt of NW Argentina, based on lithology and new geochemical data: (a) a minor trondhjemitetonalitegranodiorite (TTG) group, (b) a metaluminous Itype gabbromonzogranite suite, and (c) Stype granites. The latter occur as small cordieritic intrusions associated with Itype granodiorites and as abundant cordieritebearing facies
WhatsApp· Two weathering profiles evolved on peneplainrelated granites in Sierra Norte, Córdoba province, were examined. Several weathering levels, of no more than 2 m thickness, were studied in these profiles. They had developed from similar parent rock, which had been exposed to hydrothermal processes of varying intensity. Fracturing is the most notable feature produced by weathering; iron
WhatsAppGeochemical evolution of granites from the Achala batholith of the Sierras Pampeanas, Argentina Author(s) intrusion of probable Silurian age exposed in the Sierra de Cordoba in the eastern Sierras Pampeanas of central Argentina (31°6′S to 32°2′S; 64°29′W to 65°7′W). The batholith was emplaced into late Precambrian amphibolite and granulitefacies metamorphic rocks. Five
WhatsAppLower Carboniferous postorogenic granites in centraleastern Sierra de Velasco, Sierras Pampeanas, Argentina: UÐPb monazite geochronology, geochemistry and SrÐNd isotopes Pablo Grosse ® Frank
WhatsAppof the NW Argentina, in Fourth Hutton symposium on the origin of Granites and related rocks: Transactions of the Royal Society of Edinburgh Earth Sciences, p. 151163. Parkhurst,, Rapela, J. Saavedra, E. Baldo, J. Dlquist, I. Pascua, and Fanning, 1998, The Famatinian magmatic arc in the central Sierras Pampeanas; an Early to MidOrdovician continental arc on the
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WhatsAppThe student Enrico Ribacki has participated in the GRANITES II Summer school. This workshop was dedicated to magmatic differentiation and combined field studies, experimental petrology, geochemistry, petrophysics, modeling, and geochronology for a
WhatsAppAge and origin of coeval TTG, I and Stype granites in the Famatinian belt of NW Argentina Volume 91 Issue 12 R. J. Pankhurst, C. W. Rapela, C. M. Fanning
WhatsAppAbstract The geochemistry of K‐feldspar for K, P, Sr, Ba, Rb, Cs, Ga, and of muscovite for the same elements plus Nb and Ta, was used for proving the parental relationships of S‐type granites and L
WhatsAppThe centraleastern part of the Sierra de Velasco (Sierras Pampeanas, NW Argentina) is formed by the large Huaco (40 × 30 km) and Sanagasta (25 × 15 km) granite massifs and the small La Chinchilla stock (2 × 2 km). The larger granites intrude into Ordovician metagranitoids and crosscut Devonian (?) mylonitic shear zones, whereas the small stock sharply intrudes into the Huaco granite.
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WhatsAppLower Carboniferous postorogenic granites in centraleastern Sierra de Velasco, Sierras Pampeanas, Argentina: U–Pb monazite geochronology, geochemistry and Sr–Nd isotopes July 2008
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WhatsApp· The centraleastern part of the Sierra de Velasco (Sierras Pampeanas, NW Argentina) is formed by the large Huaco (40 × 30 km) and Sanagasta (25 × 15 km) granite massifs and the small La Chinchilla stock (2 × 2 km). The larger granites intrude into Ordovician metagranitoids and crosscut Devonian (?) mylonitic shear zones, whereas the small stock sharply intrudes into the Huaco granite.
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WhatsAppThe Famatinian granites outcrop intermittently between brilliant red successions of Permian age strata. As my PhD is focused on millionyearold tectonics, we made the trek from La Rioja to Chilecito in a day via RN 40. This road was spectacular and warranted numerous photo stops.
WhatsAppTwo weathering profiles evolved on peneplainrelated granites in Sierra Norte, Córdoba province, were examined. Several weathering levels, of no more
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WhatsAppThe petrogenetic nature of Atype granites is a controversial problem. The Vinquis batholith in the Sierras Pampeanas of Argentina contains unusual Frich and strongly peraluminous Atype monzogranites. A new LAMCICPMS UPb zircon crystallization age of 355 ± 7 Ma indicates emplacement in latest Devonian or earliest Carboniferous time, overlapping with extensive
WhatsAppWeathering profiles in granites, Sierra Norte (Córdoba, Argentina) Article in Journal of South American Earth Sciences 19(4):479493 · September 2005 with 25 Reads How we measure ''reads''
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