Registro completo de metadatos
| Campo DC | Valor | Lengua/Idioma |
|---|---|---|
| dc.creator | Pinotti, Lucio Pedro | - |
| dc.creator | D'eramo, Fernando Javier | - |
| dc.creator | Weinberg, Roberto F. | - |
| dc.creator | Demartis, Manuel | - |
| dc.creator | Tubía Martinez, José María | - |
| dc.creator | Coniglio, Jorge Enrique | - |
| dc.creator | Radice, Stefania | - |
| dc.creator | Maffini, María Natalia | - |
| dc.creator | Aragon, Eugenio | - |
| dc.date | 2018-06-19T16:43:10Z | - |
| dc.date | 2018-06-19T16:43:10Z | - |
| dc.date | 2016-11 | - |
| dc.date | 2018-06-18T21:22:41Z | - |
| dc.date.accessioned | 2019-04-29T15:34:43Z | - |
| dc.date.available | 2019-04-29T15:34:43Z | - |
| dc.date.issued | 2016-11 | - |
| dc.identifier | Pinotti, Lucio Pedro; D'eramo, Fernando Javier; Weinberg, Roberto F.; Demartis, Manuel; Tubía Martinez, José María; et al.; Contrasting magmatic structures between small plutons and batholiths emplaced at shallow crustal level (Sierras de Córdoba, Argentina); Pergamon-Elsevier Science Ltd; Journal Of Structural Geology; 92; 11-2016; 46-58 | - |
| dc.identifier | 0191-8141 | - |
| dc.identifier | http://hdl.handle.net/11336/49298 | - |
| dc.identifier | CONICET Digital | - |
| dc.identifier | CONICET | - |
| dc.identifier.uri | http://rodna.bn.gov.ar:8080/jspui/handle/bnmm/297002 | - |
| dc.description | Processes like injection, magma flow and differentiation and influence of the regional strain field are here described and contrasted to shed light on their role in the formation of small plutons and large batholiths their magmatic structures. The final geometric and compositional arrangement of magma bodies are a complex record of their construction and internal flow history. Magma injection, flow and differentiation, as well as regional stresses, all control the internal nature of magma bodies. Large magma bodies emplaced at shallow crustal levels result from the intrusion of multiple magma batches that interact in a variety of ways, depending on internal and external dynamics, and where the early magmatic, growth-related structures are commonly overprinted by subsequent history. In contrast, small plutons emplaced in the brittle-ductile transition more likely preserve growth-related structures, having a relatively simple cooling history and limited internal magma flow. Outcrop-scale magmatic structures in both cases record a rich set of complementary information that can help elucidate their evolution. Large and small granitic bodies of the Sierra Pampeanas preserve excellent exposures of magmatic structures that formed as magmas stepped through different rheological states during pluton growth and solidification. These structures reveal not only the flow pattern inside magma chambers, but also the rheological evolution of magmas in response to temperature evolution. | - |
| dc.description | Fil: Pinotti, Lucio Pedro. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de Río Cuarto; Argentina | - |
| dc.description | Fil: D'eramo, Fernando Javier. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de Río Cuarto; Argentina | - |
| dc.description | Fil: Weinberg, Roberto F.. Monash University; Australia | - |
| dc.description | Fil: Demartis, Manuel. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de Río Cuarto; Argentina | - |
| dc.description | Fil: Tubía Martinez, José María. 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: Coniglio, Jorge Enrique. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de Río Cuarto; Argentina | - |
| dc.description | Fil: Radice, Stefania. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de Río Cuarto; Argentina | - |
| dc.description | Fil: Maffini, María Natalia. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Universidad Nacional de Río Cuarto; Argentina | - |
| dc.description | Fil: Aragon, Eugenio. Universidad del País Vasco; España | - |
| dc.format | application/pdf | - |
| dc.format | application/pdf | - |
| dc.format | application/pdf | - |
| dc.format | application/pdf | - |
| dc.format | application/pdf | - |
| dc.format | application/pdf | - |
| dc.format | application/pdf | - |
| dc.language | eng | - |
| dc.publisher | Pergamon-Elsevier Science Ltd | - |
| dc.relation | info:eu-repo/semantics/altIdentifier/doi/https://dx.doi.org/10.1016/j.jsg.2016.09.009 | - |
| dc.relation | info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0191814116301390 | - |
| 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 | BATHOLITH | - |
| dc.subject | GRANITE | - |
| dc.subject | MAGMA FLOW | - |
| dc.subject | MAGMATIC STRUCTURES | - |
| dc.subject | MELT SEGREGATIONS | - |
| 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 | Contrasting magmatic structures between small plutons and batholiths emplaced at shallow crustal level (Sierras de Córdoba, 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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