Registro completo de metadatos
| Campo DC | Valor | Lengua/Idioma |
|---|---|---|
| dc.creator | Casquet, César | - |
| dc.creator | Rapela, Carlos Washington | - |
| dc.creator | Pankhurst, Robert J. | - |
| dc.creator | Baldo, Edgardo Gaspar Agustín | - |
| dc.creator | Galindo, Carmen | - |
| dc.creator | Fanning, Cristopher M. | - |
| dc.creator | Dahlquist, Juan Andrés | - |
| dc.date | 2018-07-16T18:36:17Z | - |
| dc.date | 2018-07-16T18:36:17Z | - |
| dc.date | 2012-09 | - |
| dc.date | 2018-07-11T17:45:50Z | - |
| dc.date.accessioned | 2019-04-29T15:57:00Z | - |
| dc.date.available | 2019-04-29T15:57:00Z | - |
| dc.identifier | Casquet, César; Rapela, Carlos Washington; Pankhurst, Robert J.; Baldo, Edgardo Gaspar Agustín; Galindo, Carmen; et al.; Fast sediment underplating and essentially coeval juvenile magmatism in the Ordovician margin of Gondwana, Western Sierras Pampeanas, Argentina; Elsevier Science; Gondwana Research; 22; 2; 9-2012; 664-673 | - |
| dc.identifier | 1342-937X | - |
| dc.identifier | http://hdl.handle.net/11336/52244 | - |
| dc.identifier | CONICET Digital | - |
| dc.identifier | CONICET | - |
| dc.identifier.uri | http://rodna.bn.gov.ar:8080/jspui/handle/bnmm/306030 | - |
| dc.description | Metasedimentary high-pressure upper amphibolite facies gneisses (1.2 ± 0.1. GPa and 780 ± 45 °C) at Las Chacras, Sierra de Valle Fértil, are tectonically juxtaposed to the westernmost parts (outboard) of the Famatinian (Early Ordovician) magmatic arc, which underwent syn-plutonic middle crust high-grade metamorphism at lower pressure. U-Pb SHRIMP zircon data suggest that the gneisses contain Famatinian igneous detritus, so that their sedimentary protoliths were probably deposited in a forearc basin and then rapidly underthrust and accreted to the lower crust of the arc, essentially coevally with arc magmatism at 468 ± 4. Ma. Chemically and isotopically juvenile garnetiferous amphibolites within the gneisses are recognised as representing the most primitive magmas so far observed in this belt, which has often been considered to be a continental arc derived from isotopically mature sources. This is consistent with the idea that at least part of the dominant Famatinian magmatism originated in depleted mantle but was heavily contaminated by crustal components. © 2012 International Association for Gondwana Research. | - |
| dc.description | Fil: Casquet, César. Universidad Complutense de Madrid; España | - |
| dc.description | Fil: Rapela, Carlos Washington. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina | - |
| dc.description | Fil: Pankhurst, Robert J.. British Geological Survey; Reino Unido | - |
| dc.description | Fil: Baldo, Edgardo Gaspar Agustín. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina | - |
| dc.description | Fil: Galindo, Carmen. Universidad Complutense de Madrid; España | - |
| dc.description | Fil: Fanning, Cristopher M.. The Australian National University. Research School of Earth Sciences; Australia | - |
| dc.description | Fil: Dahlquist, Juan Andrés. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Córdoba. Centro de Investigaciones en Ciencias de la Tierra. Universidad Nacional de Córdoba. Facultad de Ciencias Exactas Físicas y Naturales. Centro de Investigaciones en Ciencias de la Tierra; Argentina | - |
| dc.format | application/pdf | - |
| dc.format | application/pdf | - |
| dc.language | eng | - |
| dc.publisher | Elsevier Science | - |
| dc.relation | info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S1342937X12001232 | - |
| dc.relation | info:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1016/j.gr.2012.05.001 | - |
| dc.rights | info:eu-repo/semantics/restrictedAccess | - |
| dc.rights | https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ | - |
| dc.source | reponame:CONICET Digital (CONICET) | - |
| dc.source | instname:Consejo Nacional de Investigaciones Científicas y Técnicas | - |
| dc.source | instacron:CONICET | - |
| dc.subject | FAMATINIAN MAGMATIC ARC | - |
| dc.subject | GONDWANA | - |
| dc.subject | JUVENILE MAGMATISM | - |
| dc.subject | SIERRAS PAMPEANAS | - |
| dc.subject | U-PB SHRIMP ZIRCON GEOCHRONOLOGY | - |
| dc.subject | Meteorología y Ciencias Atmosféricas | - |
| dc.subject | Ciencias de la Tierra y relacionadas con el Medio Ambiente | - |
| dc.subject | CIENCIAS NATURALES Y EXACTAS | - |
| dc.title | Fast sediment underplating and essentially coeval juvenile magmatism in the Ordovician margin of Gondwana, Western Sierras Pampeanas, Argentina | - |
| dc.type | info:eu-repo/semantics/article | - |
| dc.type | info:eu-repo/semantics/publishedVersion | - |
| dc.type | info:ar-repo/semantics/articulo | - |
| Aparece en las colecciones: | CONICET | |
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