Crustal attenuation in the Southern Andean retroarc (38°-39°30′ S) determined from tectonic and gravimetric studies: The Lonco-Luán asthenospheric anomaly
The western retroarc of the Southern Andes between 38° and 40° S is formed by a NNW-elongated ridge not associated with stacked thrust sheets. On the contrary, during the last 4-3 Ma this ridge was affected by extensional deformation, regional uplift and related folding on a very broad scale. Receiv...
Guardado en:
| Autor principal: | |
|---|---|
| Otros Autores: | , , , , , , |
| Formato: | Capítulo de libro |
| Lenguaje: | Inglés |
| Publicado: |
2007
|
| Materias: | |
| Acceso en línea: | Registro en Scopus DOI Handle Registro en la Biblioteca Digital |
| Aporte de: | Registro referencial: Solicitar el recurso aquí |
| LEADER | 19372caa a22013937a 4500 | ||
|---|---|---|---|
| 001 | PAPER-6485 | ||
| 003 | AR-BaUEN | ||
| 005 | 20250514094327.0 | ||
| 008 | 140217s2007 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-34250853462 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Folguera, A. | |
| 245 | 1 | 0 | |a Crustal attenuation in the Southern Andean retroarc (38°-39°30′ S) determined from tectonic and gravimetric studies: The Lonco-Luán asthenospheric anomaly |
| 260 | |c 2007 | ||
| 270 | 1 | 0 | |m Folguera, A.; Laboratorio de Tectónica Andina, Universidad de Buenos Aires, CONICET, Buenos Aires, Argentina; email: andresfolguera2@yahoo.com.ar |
| 504 | |a Araneda, M., Asch, G., Bataylle, K., A crustal model along 39°S from a seismic refraction profile. ISSA 2000 (2003) Revista Geológica de Chile, 30 (1), pp. 83-101 | ||
| 504 | |a Astini, R., Ramos, V.A., Benedetto, J.L., Vaccari, N.E., La Precordillera: un terreno exótico a Gondwana (1996) Actas, V, pp. 293-324. , XIII° Congreso Geológico Argentino and III° Congreso Exploración de Hidrocarburos | ||
| 504 | |a Basei, M.A.S., Brito Neves, B.B., Varela, R., Teixeira, W., Siga Jr., O., Sato, A.M., Cingolani, C., Isotopic dating on the crystalline basement rocks of the Bariloche region, Río Negro, Argentina (1999) Anales Segemar, 34, pp. 15-18. , II° South American Symposium on Isotope Geology | ||
| 504 | |a Bettini, F.H., Pautas sobre la cronología estructural en el área del cerro Lotena, cerro Granito y su implicancia en el significado de la dorsal del Neuquén, Provincia de Neuquén (1984) Actas, III, pp. 342-362. , IX° Congreso Geológico Argentino | ||
| 504 | |a Blakely, R.J., (1995) Potential Theory in Gravity and Magnetic Applications, , Cambridge University Press | ||
| 504 | |a Brasse, H., Soyer, W., A magnetoteluric study in the Southern Chilean Andes (2001) Geophysical Research Letters, 28 (19), pp. 3757-3760 | ||
| 504 | |a Briggs, J., Machine contouring using minimum curvature (1974) Geophysics, 39, pp. 39-48 | ||
| 504 | |a Burckhardt, C., Profils géologiques transversaux de la Cordillère Argentino-Chilienne (1900) Museo de La Plata, Anales, Sección Geología y Mineralógica, 2, pp. 1-136 | ||
| 504 | |a Chernicoff, C.J., Zappetini, E.O., Delimitación de los terrenos tectono-estratigráficos de la región centro-austral Argentina: evidencias aeromagnéticas (2003) Revista Geológica de Chile, 30 (2), pp. 299-316 | ||
| 504 | |a Chernicoff, J., Zapettini, E., Geophysical evidence for terrane boundaries in South-Central Argentina (2004) Gondwana Research, 7 (4), pp. 1105-1117 | ||
| 504 | |a De Ferraris, C., Edad del Arco o Dorsal Antigua del Neuquén Oriental de acuerdo con la estratigrafía de la zona inmediata (1947) Revista de la Sociedad Geológica Argentina, 2 (3), pp. 256-283 | ||
| 504 | |a Diez Rodríguez, A., Introcaso, A., Perfil transcontinental sudamericano en el paralelo 39°S (1986) Geoacta, 13 (2), pp. 179-201 | ||
| 504 | |a Folguera, A., Ramos, V.A., Hermanns, R.L., Naranjo, J., Neotectonics in the foothills of the southernmost central Andes (37°-38°S): evidence of strike-slip displacement along the Antiñir-Copahue fault zone (2004) Tectonics, 23, pp. TC5008. , 10.1029/2003TC001533 | ||
| 504 | |a Folguera, A., Zapata, T., Ramos, V.A., Late Cenozoic Extension and the evolution of the Neuquén Andes (2006) Geological Society of America, Special Paper, 407, pp. 267-285. , Late Cretaceous to Recent Magmatism and Tectonism of the Southern Andean Margin at the Latitude of the Neuquen Basin (36-39°S). Kay S.M., and Ramos V.A. (Eds) | ||
| 504 | |a Folguera, A., Ramos, V.A., González Díaz, E., Hermanns, R., Miocene to Quaternary deformation of the Guañacos fold-and-thrust belt in the Neuquén Andes between 37° and 37°30′ S (2006) Geological Society of America, Special Paper, 407, pp. 247-266. , Late Cretaceous to Recent Magmatism and Tectonism of the Southern Andean Margin at the Latitude of the Neuquen Basin (36-39° S). Kay S.M., and Ramos V.A. (Eds) | ||
| 504 | |a Franzese, J., Spalletti, L., Late Triassic-early Jurassic continental extension in southwestern Gondwana: tectonic segmentation and pre-break-up rifting (2001) Journal of South American Earth Sciences, 14, pp. 257-270 | ||
| 504 | |a García Morabito, E., Folguera, A., El alto de Copahue-Pino Hachado y la fosa de Loncopué: un comportamiento tectónico episódico, Andes neuquinos (37°-39°S) (2005) Revista de la Asociación Geológica Argentina, 60 (4), pp. 742-761 | ||
| 504 | |a García Morabito, E., Folguera, A., Melnick, D., Ramos, V., Variabilidad en la actividad del retroarco andino entre 37 y 39°S (2003) X° Congreso Geológico de Chile, , Electronic Files | ||
| 504 | |a Grow, J.A., Bowin, C.O., Evidence for high density crust and mantle beneath the Chile trench due to the descending lithosphere (1975) Journal of Geophysical Research, 80, pp. 1449-1458 | ||
| 504 | |a Hackney, R., Echtler, H., Franz, G., Götze, H.-J., Lucassen, F., Marchenko, D., Melnick, D., Wienecke, S., The segmented overriding plate and coupling at the south-central Chile margin (2006) The Andes - Active Subduction Orogeny, Frontiers in Earth Sciences, 1, pp. 351-370. , Oncken G., Chong G., Franz P., Giese H.-J., Götze V., Ramos M., and Wigger P. (Eds), Springer Verlag | ||
| 504 | |a Introcaso, A., Pacino, M.C., Gravity Andean model associated with subduction near 24°25′ South latitude (1988) Revista Geofísica (Madrid), 44, pp. 29-44 | ||
| 504 | |a Introcaso, A., Pacino, M.C., Fraga, H., Gravity, isostasy and Andean crustal shortening between 30° and 35°S latitude (1992) Tectonophysics (Amsterdam), 205 (1-3), pp. 31-48 | ||
| 504 | |a Introcaso, A., Pacino, M., Guspi, F., A gravity chart to quickly evaluate the probable contribution of the lithosphere heating to the isostatic balance of the Central Andes (1997) Bolletin Di Geofisica Teorica ed Applicata, 38 (N1-2), pp. 41-54 | ||
| 504 | |a Isacks, B., Uplift of the Central Andean Plateau and Bending of the Bolivian Orocline (1988) Journal of Geophysical Research, 93 (B4), pp. 3211-3231 | ||
| 504 | |a Jordan, T., Burns, W., Veiga, R., Pángaro, F., Copeland, P., Kelley, S., Mpodozis, C., Extension and basin formation in the Southern Andes caused by increased convergence rate: a Mid-Cenozoic trigger for the Andes (2001) Tectonics, 20, pp. 308-324 | ||
| 504 | |a Kay, S.M., Tertiary to Recent transient shallow subduction zones in the Central and Southern Andes (2002) Actas, III, pp. 282-283. , XV° Congreso Geológico Argentino | ||
| 504 | |a Kay, S.M., Burns, M., Copeland, P., Upper Cretaceous to Holocene Magmatism over the Neuquén Basin: evidence for transient shallowing of the subduction zone under the Neuquén Andes (36°S to 38°S latitude) (2006) Geological Society of America, Special Paper, 407, pp. 19-60. , Late Cretaceous to Recent Magmatism and Tectonism of the Southern Andean Margin at the Latitude of the Neuquen Basin (36-39°S). Kay S.M., and Ramos V.A. (Eds) | ||
| 504 | |a Kostadinoff, J., Font de Affolter, G., Cuenca interserrana bonaerense, Argentina (1982) Actas, IV, pp. 105-121. , V° Congreso Latinoamericano de Geología | ||
| 504 | |a Kostadinoff, J., Gregori, D., Raniolo, A., Configuración geofísica-geológica del sector norte de la Provincia de Río Negro (2005) Revista de la Asociación Geológica Argentina, 60 (2), pp. 368-376 | ||
| 504 | |a Lara, L., Rodríguez, C., Moreno, H., Pérez de Arce, H., Geocronología K-Ar y geoquímica del volcanismo plioceno superior-pleistoceno de los Andes del sur (39°-42°S) (2001) Revista Geológica de Chile, 28 (1), pp. 67-90 | ||
| 504 | |a Lara, L., Folguera, A., Plio-Quaternary narrowing of the volcanic arc at Southern Andes (37°-41°S), southwestern margin of Neuquén Basin: geochronologic and field tectonic data evaluated (2006) Geological Society of America, Special Paper, 407, pp. 299-315. , Late Cretaceous to Recent Magmatism and Tectonism of the Southern Andean Margin at the Latitude of the Neuquen Basin (36-39°S). Kay S.M., and Ramos V.A. (Eds) | ||
| 504 | |a Lüth, S., Wigger, P., A crustal model along 39°S from a seismic refraction profile-ISSA 2000 (2003) Revista Geológica de Chile, 30 (1), pp. 83-101 | ||
| 504 | |a Melnick, D., Folguera, A., Rosenau, M., Echtler, H., Potent, S., Tectonics from the Northern Segment of the Liquiñe-Ofqui fault system (37°-39°S), Patagonian Andes (2002) V International Symposium of Andean Geodynamics, Abstracts, pp. 413-416 | ||
| 504 | |a Melnick, D., Folguera, A., Hechtler, H., Charlet, F., Buttner, O., DeBatist, M., The Lago del Laja fault system: active intraarc orogenic collapse in the Southern Central Andes (37°15′ S) (2003) X° Congreso Geológico de Chile, , Electronic Files | ||
| 504 | |a Melnick, D., Rosenau, M., Folguera, A., Echtler, H., Neogene Tectonics of the Western flank of the Neuquén Andes, 37°-39°30′ S (2006) Geological Society of America, Special Paper, 407, pp. 73-95. , Late Cretaceous to Recent Magmatism and Tectonism of the Southern Andean Margin at the Latitude of the Neuquen Basin (36-39°S). Kay S.M., and Ramos V.A. (Eds) | ||
| 504 | |a Mosquera, A., Ramos, V.A., Intraplate deformation in the Neuquen Embayment (2006) Geological Society of America, Special Paper, 407, pp. 97-123. , Evolution of An Andean Margin: Tectonic and Magmatic View from the Andes to the Neuquén Basin (35°-39°S). Kay S.M., and Ramos V.A. (Eds) | ||
| 504 | |a Muñoz, J., Stern, C., The Quaternary volcanic belt of the Southern continental margin of South America: transverse structural and petrochemical variations across the segment between 38°S and 39°S (1988) Journal of South American Earth Sciences, 1, pp. 147-162 | ||
| 504 | |a Muñoz Bravo, J., Stern, C., Bermúdez, A., Delpino, D., Dobbs, M.F., Frey, F.A., El volcanismo plio-cuaternario a través de los 38° y 39°S de los Andes (1989) Revista de la Asociación Geológica Argentina, 44, pp. 270-286 | ||
| 504 | |a Pacino, M., The Andean elevation in Argentina-Chile at 39°S from gravity data (1997) Geoacta, 22, pp. 91-102 | ||
| 504 | |a Pesce, A., Evolución volcano-tectónica del complejo efusivo Copahue-Caviahue y su modelo geotérmico preliminar (1989) Revista de la Asociación Geológica Argentina, 44 (1-4), pp. 307-327 | ||
| 504 | |a Ploszkiewicz, J.V., Orchuela, I.A., Vaillard, J.C., Viñes, R.F., Compresión y desplazamiento lateral en la zona de Falla Huincul: estructuras asociadas, provincia del Neuquén (1984) Actas, II, pp. 163-169. , IX° Congreso Geológico Argentino | ||
| 504 | |a Ramos, V.A., Estructura (1977) Geología y Recursos Naturales de la Provincia del Neuquén. VII° Congreso Geológico Argentino, Relatorio, 1, pp. 9-24. , Rolleri E.O. (Ed) | ||
| 504 | |a Ramos, V.A., Patagonia: ¿Un continente paleozoico a la deriva? (1984) Actas, II, pp. 311-325. , IX° Congreso Geológico Argentino | ||
| 504 | |a Ramos, V.A., The birth of Southern South America (1989) American Scientist, 77, pp. 444-450 | ||
| 504 | |a Ramos, V.A., Evolución tectónica de la plataforma continental (1996) Geología y Recursos Naturales de la Plataforma Continental Argentina, pp. 385-404. , Ramos V.A., and Turic M.A. (Eds), Asociación Geólogica Argentina e Instituto Argentino del Petróleo, Buenos Aires | ||
| 504 | |a Ramos, V.A., Estructura del sector occidental de la faja plegada y corrida del Agrio, Cuenca Neuquina, Argentina (1998) Actas, II, pp. 105-110. , IX° Congreso Latinoamericano de Geología | ||
| 504 | |a Ramos, V.A., Cuyania, an exotic block to Gondwana: review of a historical success and the present problems (2004) Gondwana Research, 7 (4), pp. 1009-1026 | ||
| 504 | |a Ramos, V.A., Folguera, A., The Andes of Neuquen (36°S-38°S): Evidence of Cenozoic transtension along the arc (1999) IV Geodynamic Symposium, Actas, pp. 606-609 | ||
| 504 | |a Ramos, V.A., Folguera, A., Tectonic evolution of the Andes of Neuquén: constraints derived from the magmatic arc and foreland deformation (2006) Geological Society, London, Special Publications, 252, pp. 15-35. , The Neuquén Basin: a Case Study in Sequence Stratigraphy and Basin Dynamics. Veiga G.D., Spalletti L., Howell J.A., and Schwarz E. (Eds) | ||
| 504 | |a Ramos, V.A., Jordan, T.E., Allmendinger, R.W., Kay, S.M., Cortés, J.M., Palma, M.A., Chilenia: Un terreno alóctono en la evolución paleozoica de los Andes Centrales (1984) Actas, II, pp. 84-106. , IX° Congreso Geológico Argentino | ||
| 504 | |a Silver, P., Russo, R., Lithgow-Bertelloni, C., Coupling of South American and African plate motion and plate deformation (1998) Science, 279 (5347), pp. 60-63. , 10.1126/science.279.5347.60 | ||
| 504 | |a Tassara, A., Swain, C., Hackney, R., Kirby, J., Elastic thickness structure of South America estimated using wavelets and satellite-derived gravity data (2007) Earth and Planetary Science Letters, 253, pp. 17-36 | ||
| 504 | |a Tunstall, C., Geología de la caldera de Pino Hachado (2005) Trabajo Final de Licenciatura, , Universidad de Buenos Aires (inédito), Buenos Aires 70 pp | ||
| 504 | |a Tunstall, C., Folguera, A., Control estructural me el desarrollo de una concentración anómala de calderas en los Andes de Neuquén: Complejo Volcánico Pino Hachado (38°30′ S-71°O) (2005) Revista de la Asociación Geológica Argentina, 60 (4), pp. 731-741 | ||
| 504 | |a Tunstall, C., Folguera, A., Ramos, V.A., Retroarc extensión associated with reactivation of basement structures and retroarc volcanism (38°30′ S-71° W) (2006) Abstract Programs, 68. , Backbone of the Americas. Patagonia to Alaska. 3-6 abril. Geological Society of America and Co-convened by Asociación Geológica Argentina | ||
| 504 | |a Varela, R., Basei, M.A.S., Brito Neves, B.B., Sato, A.M., Teixeira, W., Cingolani, C.A., Siga Jr., O., Isotopic study of igneous and metamorphic rocks of Comallo-Paso Flores, Río Negro, Argentina (1999) Anales Segemar, 34, pp. 148-151. , II South American Symposium on Isotope Geology | ||
| 504 | |a Vergani, G., Tankard, A.J., Belotti, H.J., Welsnik, H.J., Tectonic evolution and Paleogeography of the Neuquén Basin (1995) AAPG Memoir, Tulsa, 62, pp. 383-402. , Petroleum Basins of South America. Tankard A.J., Suárez S.R., and Welsnik H.J. (Eds) | ||
| 504 | |a Von Gosen, W., Thrust tectonics in the North Patagonian Massif (Argentina): implications for a Patagonia plate (2003) Tectonics, 22 (1), p. 1005. , 10.1029/2001ITC901039 | ||
| 504 | |a Yuan, X., Asch, G., Bataile, K., Bohm, M., Echtler, H., Kind, R., Onchen, O., Wölbern, I., Deep seismic images of the Southern Andes (2006) Geological Society of America, Special Paper, 407, pp. 61-72. , Late Cretaceous to Recent Magmatism and Tectonism of the Southern Andean Margin at the Latitude of the Neuquen Basin (36-39°S). Kay S.M., and Ramos V.A. (Eds) | ||
| 504 | |a Zambrano, J., Cuencas sedimentarias en el subsuelo de la Provincia de Buenos Aires y zonas adyacentes (1969) Revista de la Asociación Geológica Argentina, 29 (4), pp. 443-469 | ||
| 504 | |a Zapata, T.R., Folguera, A., Tectonic evolution of the Andean Fold and Thrust Belt, south of the Barrancas River, Neuquén Basin, Argentina (2005) Geological Society, London, Special Publications, 252, pp. 37-56. , The Neuquén Basin: A Case Study in Sequence Stratigraphy and Basin Dynamics. Veiga G.D., Spalletti L., Howell J.A., and Schwarz E. (Eds) | ||
| 504 | |a Zapata, T., Brissón, I., Dzelalija, F., The role of basement in the Andean fold and thrust belt of the Neuquén Basin (1999) Thrust Tectonics, Proceedings, pp. 122-124 | ||
| 506 | |2 openaire |e Política editorial | ||
| 520 | 3 | |a The western retroarc of the Southern Andes between 38° and 40° S is formed by a NNW-elongated ridge not associated with stacked thrust sheets. On the contrary, during the last 4-3 Ma this ridge was affected by extensional deformation, regional uplift and related folding on a very broad scale. Receiver function analysis shows that the drainage divide area and adjacent retroarc lie over an attenuated crust. Expected crustal thickness at these latitudes is around 38 km, whereas in this part of the retroarc the thickness is less than 32 km. The causes for such attenuation have been linked to a moderate steepening of the subducted Nazca plate beneath the South American plate, which is suggested by a westward shift and narrowing of the magmatic arc during the last 4 to 5 Ma. Gravimetric studies show that the upper plate did not react homogeneously to slab steepening, but ancient sutures and lithospheric discontinuities deeply buried under Mesozoic to Cenozoic sequences in the retroarc were locally reactivated. These processes resulted in an asthenospheric anomaly that correlates at the surface with the area of Pliocene to Quaternary doming, widespread extension and three radial troughs. Two of the troughs have accommodated substantial amounts of extension, but the third was probably aborted at an early stage. Moreover, the presence of an anomalous concentration of calderas and large volcanic centers over the proposed asthenospheric anomaly, and their age distribution, may indicate minor migration of the asthenospheric anomaly between 4 and 2 Ma through the western South American plate. © 2007 Elsevier B.V. All rights reserved. |l eng | |
| 593 | |a Laboratorio de Tectónica Andina, Universidad de Buenos Aires, CONICET, Buenos Aires, Argentina | ||
| 593 | |a Instituto de Física de Rosario, Facultad de Ciencias Exactas, Ingeniería y Agrimensura, Universidad Nacional de Rosario, Argentina | ||
| 593 | |a Instituto Geofísico Sismológico Ing. F. S. Volponi, Facultad de Ciencias Exactas, Físicas y Naturales, Universidad Nacional de San Juan, Argentina | ||
| 651 | 4 | |a SOUTH AMERICA | |
| 690 | 1 | 0 | |a ANDEAN GRAVITY |
| 690 | 1 | 0 | |a ASTHENOSPHERIC ANOMALIES |
| 690 | 1 | 0 | |a RETROARC EXTENSION |
| 690 | 1 | 0 | |a RETROARC VOLCANISM |
| 690 | 1 | 0 | |a THERMAL UPLIFT |
| 690 | 1 | 0 | |a ASTHENOSPHERE |
| 690 | 1 | 0 | |a CENOZOIC |
| 690 | 1 | 0 | |a CRUSTAL STRUCTURE |
| 690 | 1 | 0 | |a CRUSTAL THICKNESS |
| 690 | 1 | 0 | |a DEFORMATION |
| 690 | 1 | 0 | |a EXTENSIONAL TECTONICS |
| 690 | 1 | 0 | |a FOLDING |
| 690 | 1 | 0 | |a GRAVIMETRY |
| 690 | 1 | 0 | |a MESOZOIC |
| 690 | 1 | 0 | |a NAZCA PLATE |
| 690 | 1 | 0 | |a SLAB |
| 690 | 1 | 0 | |a TECTONIC PLATE |
| 690 | 1 | 0 | |a THRUST |
| 690 | 1 | 0 | |a UPLIFT |
| 690 | 1 | 0 | |a INDICATOR MINOR |
| 700 | 1 | |a Introcaso, Antonio | |
| 700 | 1 | |a Giménez, M. | |
| 700 | 1 | |a Ruiz, F. | |
| 700 | 1 | |a Martinez, P. | |
| 700 | 1 | |a Tunstall, C. | |
| 700 | 1 | |a García Morabito, E. | |
| 700 | 1 | |a Ramos, V.A. | |
| 773 | 0 | |d 2007 |g v. 439 |h pp. 129-147 |k n. 1-4 |p Tectonophysics |x 00401951 |w (AR-BaUEN)CENRE-81 |t Tectonophysics | |
| 856 | 4 | 1 | |u http://www.scopus.com/inward/record.url?eid=2-s2.0-34250853462&partnerID=40&md5=be6d0fb5e1aa9fb6318e0e0b3dea7429 |y Registro en Scopus |
| 856 | 4 | 0 | |u https://doi.org/10.1016/j.tecto.2007.04.001 |y DOI |
| 856 | 4 | 0 | |u https://hdl.handle.net/20.500.12110/paper_00401951_v439_n1-4_p129_Folguera |y Handle |
| 856 | 4 | 0 | |u https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00401951_v439_n1-4_p129_Folguera |y Registro en la Biblioteca Digital |
| 961 | |a paper_00401951_v439_n1-4_p129_Folguera |b paper |c PE | ||
| 962 | |a info:eu-repo/semantics/article |a info:ar-repo/semantics/artículo |b info:eu-repo/semantics/publishedVersion | ||
| 963 | |a VARI | ||
| 999 | |c 67438 | ||