Registro completo de metadatos
| Campo DC | Valor | Lengua/Idioma |
|---|---|---|
| dc.creator | Zambrano Zambrano | - |
| dc.creator | Rapalini, Augusto Ernesto | - |
| dc.creator | Davila, Federico Miguel | - |
| dc.creator | Astini, Ricardo Alfredo | - |
| dc.creator | Spagnuolo, Cecilia Mariel | - |
| dc.date | 2019-01-28T19:45:09Z | - |
| dc.date | 2019-01-28T19:45:09Z | - |
| dc.date | 2011-04 | - |
| dc.date | 2019-01-28T14:02:04Z | - |
| dc.date.accessioned | 2019-04-29T15:43:27Z | - |
| dc.date.available | 2019-04-29T15:43:27Z | - |
| dc.date.issued | 2019-01-28T19:45:09Z | - |
| dc.date.issued | 2019-01-28T19:45:09Z | - |
| dc.date.issued | 2011-04 | - |
| dc.date.issued | 2019-01-28T14:02:04Z | - |
| dc.identifier | Zambrano Zambrano; Rapalini, Augusto Ernesto; Davila, Federico Miguel; Astini, Ricardo Alfredo; Spagnuolo, Cecilia Mariel; Magnetostratigraphy and paleomagnetism of early and middle Miocene synorogenic strata: Basement partitioning and minor block rotation in Argentine broken foreland; Springer; International Journal of Earth Sciences; 100; 2; 4-2011; 591-602 | - |
| dc.identifier | 1437-3254 | - |
| dc.identifier | http://hdl.handle.net/11336/68798 | - |
| dc.identifier | 1437-3262 | - |
| dc.identifier | CONICET Digital | - |
| dc.identifier | CONICET | - |
| dc.identifier.uri | http://rodna.bn.gov.ar:8080/jspui/handle/bnmm/300366 | - |
| dc.description | Magnetostratigraphic and paleomagnetic studies on early Andean synorogenic strata (Del Crestón Fm.), in the Famatina Belt (28.7°S, 67.5°W) clarify details of chronology that permit calculation of sedimentation rates within the broken foreland of west Argentina. The Del Crestón Fm represents the first record of broken foreland sedimentation within the southern Central Andean belt and the earliest retroarc volcanic rocks exposed several hundred kilometers from the trench. Twenty-five out of 49 sites collected along the succession presented a primary remanence, as determined through positive fold and reversal tests. Correlation of the local magnetic polarity section with the global polarity time scale indicates that the sedimentation of Del Crestón Fm started at ~16.7 Ma and continued until ~14.5 Ma. The youngest strata are represented by conglomerates bearing abundant Lower Paleozoic granite boulders indicating unroofing of the crystalline basement within the NW Sierras Pampeanas. This result supports the hypothesis of an early broken foreland stage at these latitudes of the Andes, with involvement of the basement in deformation and coeval retroarc volcanism, common attributes of flat-subduction regimes. A mean site paleomagnetic direction of Dec: 6.3°, Inc: -43.6° (α95: 8.0°, N = 24) confirm our earlier intrepretation that the central part of the Famatina Belt within the Sierras Pampeanas did not undergo large vertical axes rotations since the Middle Miocene. | - |
| dc.description | Fil: Zambrano Zambrano. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Geología; Argentina | - |
| dc.description | Fil: Rapalini, Augusto Ernesto. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Geología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina | - |
| dc.description | Fil: Davila, Federico Miguel. 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: Astini, Ricardo Alfredo. 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: Spagnuolo, Cecilia Mariel. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Geología; Argentina. Universidad Nacional de Tucuman. Facultad de Cs.naturales E Instituto Miguel Lillo. Laboratorio de Sedimentologia; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina | - |
| dc.format | application/pdf | - |
| dc.format | application/pdf | - |
| dc.language | eng | - |
| dc.publisher | Springer | - |
| dc.relation | info:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1007/s00531-010-0570-x | - |
| dc.relation | info:eu-repo/semantics/altIdentifier/url/https://link.springer.com/article/10.1007%2Fs00531-010-0570-x | - |
| 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 | CENOZOIC | - |
| dc.subject | CENTRAL ANDES | - |
| dc.subject | FORELAND BASIN | - |
| dc.subject | MAGNETOSTRATIGRAPHY | - |
| dc.subject | PALEOMAGNETISM | - |
| dc.subject | Otras Ciencias de la Tierra y relacionadas con el Medio Ambiente | - |
| dc.subject | Ciencias de la Tierra y relacionadas con el Medio Ambiente | - |
| dc.subject | CIENCIAS NATURALES Y EXACTAS | - |
| dc.title | Magnetostratigraphy and paleomagnetism of early and middle Miocene synorogenic strata: Basement partitioning and minor block rotation in Argentine broken foreland | - |
| 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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