Magnetic characterization of a retroarc extensional basin: The Loncopué Trough
The Loncopué Trough is a Pliocene to Quaternary extensional basin developed over the hinterland area of the Southern Central Andes. This basin is bounded by two neotectonic extensional fault systems delimiting a narrow topographic low. Previous studies have mostly focused on structural and geochemic...
Guardado en:
| Autor principal: | |
|---|---|
| Otros Autores: | , , , |
| Formato: | Capítulo de libro |
| Lenguaje: | Inglés |
| Publicado: |
Elsevier Ltd
2019
|
| Acceso en línea: | Registro en Scopus DOI Handle Registro en la Biblioteca Digital |
| Aporte de: | Registro referencial: Solicitar el recurso aquí |
| LEADER | 14468caa a22010457a 4500 | ||
|---|---|---|---|
| 001 | PAPER-25834 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518205758.0 | ||
| 008 | 190410s2019 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-85056585505 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Pesce, A. | |
| 245 | 1 | 0 | |a Magnetic characterization of a retroarc extensional basin: The Loncopué Trough |
| 260 | |b Elsevier Ltd |c 2019 | ||
| 270 | 1 | 0 | |m Pesce, A.; IGSV, Instituto Geofísico-Sismológico Volponi, Facultad de Ciencias Exactas, Fsicas y Naturales, Universidad, Nacional de San Juan, CONICETArgentina; email: pesce.agustina@gmail.com |
| 506 | |2 openaire |e Política editorial | ||
| 504 | |a Aisengar, T., Inversão do vetor de magnetização, com e sem o uso de vínculo geológico, nas regiões de Araxá e Tapira, Minas Gerais-Brasil (2015) 14th International Congress of The Brazilian Geophysical Society, Rio de Janeiro, Brazil | ||
| 504 | |a Amante, C., Eakins, B.W., ETOPO1 1 Arc-minute Global Relief Model: Procedures, Data Sources and Analysis (2009), National Geophysical Data Center, NOAA Boulder Colorado; Anci, S., Ruiz, F., Lince Klinger, F., Leiva, F., García, H., Acosta, G., Interpretación de la corteza superior a partir demétodos potenciales en la región de la Payenia y faja plegada y corrida de Malargüe (2016) Rev. Asoc. Geol. Argent., 73, pp. 159-172 | ||
| 504 | |a Baranov, V., A new method for interpretation of aeromagnetic maps: pseudo-gravimetric anomalies (1957) Geophysics, 22, pp. 359-382 | ||
| 504 | |a Blakely, R.J., Potential Theory in Gravity and Magnetic Applications (1996), Cambridge University Press; Blanco-Montenegro, I., Nicolosi, I., Pignatelli, A., García, A., Chiappini, M., New evidence about the structure and growth of ocean island volcanoes from aeromagnetic data: the case of Tenerife, Canary Islands (2011) J. Geophys. Res.: Solid Earth, 116 | ||
| 504 | |a Briggs, I.C., Machine contouring using minimum curvature (1974) Geophysics, 39, pp. 39-48 | ||
| 504 | |a Delgado, F., Estudio aeromagnético de la estructura interna de los volcanes Villarrica y Quetrupillán (Andes del Sur, Chile) (2012) Congreso Geológico Chileno, 13, pp. 624-626. , Antofagasta, Chile | ||
| 504 | |a Ellis, R.G., de Wet, B., Macleod, I.N., Inversion of magnetic data for remanent and induced sources (2012) ASEG Extended Abstracts, 2012, p. 1 | ||
| 504 | |a Folguera, A., Ramos, V.A., Díaz, E.F.G., Hermanns, R., Miocene to quaternary deformation of the guañacos Fold and thrust belt in the neuquén Andes between 37° S and 37°30’ S (2006) GSA (Geol. Soc. Am.) Spec. Pap. (Reg. Stud.), 407, pp. 247-266 | ||
| 504 | |a Folguera, A., Introcaso, A., Giménez, M., Ruiz, F., Martinez, P., Tunstall, C., García Morabito, E., Ramos, V.A., Crustal attenuation in the Southern Andean retroarc (38°-39°30’ S) determined from tectonic and gravimetric studies: the Lonco-Luán asthenospheric anomaly (2007) Tectonophysics, 439, pp. 129-147 | ||
| 504 | |a Folguera, A., Rojas Vera, E., Bottesi, G., Valcarce, G.Z., Ramos, V.A., The Loncopué trough: a cenozoic basin produced by extension in the southern central Andes (2010) J. Geodyn., 49, pp. 287-295 | ||
| 504 | |a Galland, O., Hallot, E., Cobbold, P.R., Ruffet, G., de Bremond d'Ars, J., Volcanism in a compressional Andean setting: a structural and geochronological study of Tromen volcano (Neuquén province, Argentina) (2007) Tectonics, 26 | ||
| 504 | |a García, A., Chiappini, M., Blanco-Montenegro, I., Carluccio, R., D'Ajello Caracciolo, F., De Ritis, R., Nicolosi, I., Boschi, E., High resolution magnetic anomaly map of Tenerife, Canary Islands (2007) Ann. Geophys., 50 | ||
| 504 | |a Garcia 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) Rev. Asoc. Geol. Argent., 60, pp. 742-761 | ||
| 504 | |a Gianni, G.M., García, H.P.A., Lupari, M., Pesce, A., Folguera, A., Plume overriding triggers shallow subduction and orogeny in the southern Central Andes (2017) Gondwana Res., 49, pp. 387-395 | ||
| 504 | |a Hinze, W.J., Von Frese, R.R.B., Saad, A.H., Gravity and Magnetic Exploration: Principles, Practices, and Applications (2013), Cambridge University Press; Jordan, T.E., Burns, W.M., 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., Copeland, P., Early to middle Miocene backarc magmas of the Neuquén Basin: geochemical consequences of slab shallowing and the westward drift of South America (2006) GSA (Geol. Soc. Am.) Spec. Pap. (Reg. Stud.), 407, pp. 185-213 | ||
| 504 | |a López-Loera, H., Urrutia-Fucugauchi, J., Alva-Valdivia, L., Estudio aeromagnético del complejo volcánico de Colima, occidente de México–implicaciones tectónicas y estructurales (2011) Rev. Mex. Ciencias Geol., 28, pp. 349-370 | ||
| 504 | |a Li, C., Lu, Y., Wang, J., A global reference model of Curie-point depths based on EMAG2 (2017) Sci. Rep., 7, p. 45129 | ||
| 504 | |a Mamaní, M., Borzotta, E., Venencia, J., Maidana, A., Moyano, C., Castiglione, B., Electric structure of the Copahue volcano (neuquén province, Argentina), from magnetotelluric soundings: 1D and 2D modellings (2000) J. S. Am. Earth Sci., 13, pp. 147-156. , https://doi.org/10.1016/S0895-9811(00)00011-0 | ||
| 504 | |a Maus, S., Barckhausen, U., Berkenbosch, H., Bournas, N., Brozena, J., Childers, V., Dostaler, F., Caratori Tontini, F., Emag2: a 2arc min resolution earth magnetic anomaly grid compiled from satellite, airborne, and marine magnetic measurements (2009) G-cubed, 10 | ||
| 504 | |a Messager, G., Nivière, B., Martinod, J., Lacan, P., Xavier, J.P., Geomorphic evidence for plio-quaternary compression in the andean foothills of the southern Neuquén Basin, Argentina (2010) Tectonics, 29 | ||
| 504 | |a Miller, H.G., Singh, V., Potential field tilt-a new concept for location of potential field sources (1994) J. Appl. Geophys., 32, pp. 213-217 | ||
| 504 | |a Paine, J., De Ritis, R., Ventura, G., Longo, M., Ravat, D., Speranza, F., Chiappini, M., Inverse modelling of the reversely magnetized, shallow plumbing system hosting oil reservoirs of the Auca Mahuida volcano (Payeina retroarc, neuquén Basin, Argentina) (2015) Geophys. J. Int., 204, pp. 852-867 | ||
| 504 | |a Pesicek, J.D., Engdahl, E.R., Thurber, C.H., DeShon, H.R., Lange, D., Mantle subducting slab structure in the region of the 2010 M8.8 Maule earthquake (30-40° S), Chile (2012) Geophys. J. Int., 191, pp. 317-324 | ||
| 504 | |a Phillips, J.D., Geosoft EXecutables (GX's) Developed by the US Geological Survey, Version 2.0, with Notes on GX Development from Fortran Code (2007), US Geological Survey; Radic, J.P., Las cuencas cenozoicas y su control en el volcanismo de los Complejos Nevados de Chillán y Copahue-Callaqui (Andes del Sur, 36-39 S) (2010) Andean Geol., 37, pp. 220-246 | ||
| 504 | |a Radic, J.P., Rojas, L., Carpinelli, A., Zurita, E., Evolución tectónica de la cuenca terciaria de Cura-Mallín, región cordillerana chileno Argentina (36°30’-39° S) (2002) Congreso Geológico Argentino, pp. 233-241 | ||
| 504 | |a Ramos, V.A., Estructura de la cuenca Neuquina (1978) Congreso Geológico Argentino, pp. 99-118 | ||
| 504 | |a Ramos, V.A., Folguera, A., Tectonic evolution of the Andes of Neuquén: constraints derived from the magmatic arc and foreland deformation (2005) Geol. Soc., London, Spec. Pub., 252, pp. 15-35 | ||
| 504 | |a Rojas Vera, E., Folguera, A., Valcarce, G.Z., Ramos, V.A., The Loncopué Trough: a major orogenic collapse at the western Agrio fold and thrust belt (Andes of Neuquén, 36°40’-38°40’ S) (2008) 7th International Symposium on Andean Geodynamics Nize, pp. 609-612 | ||
| 504 | |a Rojas Vera, E.A., Folguera, A., Valcarce, G.Z., Gimenez, M., Ruiz, F., Martínez, P., Bottesi, G., Ramos, V.A., Neogene to Quaternary extensional reactivation of a fold and thrust belt: the Agrio belt in the Southern Central Andes and its relation to the Loncopué trough (38°-39° S) (2010) Tectonophysics, 492, pp. 279-294 | ||
| 504 | |a Rojas Vera, E.A., Folguera, A., Zamora Valcarce, G., Bottesi, G., Ramos, V.A., Structure and development of the Andean system between 36° and 39° S (2014) J. Geodyn., 73, pp. 34-52 | ||
| 504 | |a Ross, H.E., Blakely, R.J., Zoback, M.D., Testing the use of aeromagnetic data for the determination of Curie depth in California (2006) Geophysics, 71, pp. L51-L59 | ||
| 504 | |a Salem, A., Williams, S., Fairhead, D., Smith, R., Ravat, D., Interpretation of magnetic data using tilt-angle derivatives (2007) Geophysics, 73, pp. L1-L10 | ||
| 504 | |a Salem, A., Williams, S., Fairhead, J.D., Ravat, D., Smith, R., Tilt-depth method: a simple depth estimation method using first-order magnetic derivatives (2007) Lead. Edge, 26, pp. 1502-1505 | ||
| 504 | |a Soler, S.R., Métodos Espectrales para la determinación de la Profundidad del Punto de Curie y Espesor Elástico de la corteza Terrestre (2015); Suarez, M., Emparan, C., The stratigraphy, geochronology and paleophysiography of a Miocene fresh-water interarc basin, southern Chile (1995) J. S. Am. Earth Sci., 8, pp. 17-31 | ||
| 504 | |a Tanaka, A., Okubo, Y., Matsubayashi, O., Curie point depth based on spectrum analysis of the magnetic anomaly data in East and Southeast Asia (1999) Tectonophysics, 306, pp. 461-470 | ||
| 504 | |a Thurston, J.B., Smith, R.S., Automatic conversion of magnetic data to depth, dip, and susceptibility contrast using the SPI (TM) method (1997) Geophysics, 62, pp. 807-813 | ||
| 504 | |a Varekamp, J., Hesse, A., Mandeville, C., Back-arc basalts from the loncopue graben (province of Neuquen, Argentina) (2010) J. Volcanol. Geoth. Res., 197, pp. 313-328 | ||
| 504 | |a Yuan, X., Asch, G., Bataille, K., Bock, G., Bohm, M., Echtler, H., Kind, R., Wölbern, I., Deep seismic images of the southern Andes (2006) GSA (Geol. Soc. Am.) Spec. Pap. (Reg. Stud.), 407, pp. 61-72 | ||
| 504 | |a Zamora Valcarce, G., Zapata, T., del Pino, D., Ansa, A., Structural evolution and magmatic characteristics of the Agrio fold-and-thrust belt (2006) Spec. Pap. Geol. Soc. Am., 407, p. 125 | ||
| 520 | 3 | |a The Loncopué Trough is a Pliocene to Quaternary extensional basin developed over the hinterland area of the Southern Central Andes. This basin is bounded by two neotectonic extensional fault systems delimiting a narrow topographic low. Previous studies have mostly focused on structural and geochemical aspects of this feature. However, geophysical surveys, aimed to unravel deep structure beneath a thick-younger than 5 My volcanic coverage, are scarce and based their interpretations on low resolution data sets. In this study, we collected new aeromagnetic data with the objective of characterizing the magnetic properties of the crust in the Loncopué Through and nearby zones. Additionally, we analyze the spatial relation between geological structures, volcanic fields and magnetic data. In order to highlight the boundaries of the magnetic sources and calculate the basement depth, we applied derivative techniques and the source parameter imaging. Also, we estimated an effective susceptibility model using the Magnetization Vector Inversion method, which takes into account the combined effects of remanence and induced magnetization. To determine the thermal structure of the area, we calculated the Curie depth points through the spectral analysis technique. From the analysis of magnetic data we were able to characterize the main structures and lineaments associated with this retroarc extensional trough. Notably, only the Loncopué eastern fault system seems to be a crustal-scale tectonic feature, while E-W-, ENE- and ESE-trending lineaments are interpreted as relatively minor structures segmenting the basement. Finally, our susceptibility model, together with the analysis of the Curie point, revealed potential magmatic/hydrothermal reservoirs in the Copahue volcano, and the Codihue and Cajón de Almanza regions that could be connected at depth forming a regional magmatic body. © 2018 |l eng | |
| 536 | |a Detalles de la financiación: Consejo Nacional de Investigaciones Científicas y Técnicas, PICT 2014 1697 Project | ||
| 536 | |a Detalles de la financiación: The authors wish to thank to CONICET and the AGENCIA by funding provided through the PICT 2014 1697 Project. PIP 2015-2017 CONICET. We also thank Gas and Petroleum of Neuquen S.A. for providing the aeromagnetic data. | ||
| 593 | |a IGSV, Instituto Geofísico-Sismológico Volponi, Facultad de Ciencias Exactas, Fsicas y Naturales, Universidad, Nacional de San Juan, CONICET, Argentina | ||
| 593 | |a IDEAN, Instituto de Estudios Andinos, Universidad de Buenos Aires-CONICET, Argentina | ||
| 690 | 1 | 0 | |a AEROMAGNETIC DATA |
| 690 | 1 | 0 | |a EFFECT SUSCEPTIBILITY MODEL |
| 690 | 1 | 0 | |a LONCOPUE TROUGH |
| 690 | 1 | 0 | |a MAGNETIC CHARACTERIZATION |
| 690 | 1 | 0 | |a SOUTHERN CENTRAL ANDES |
| 690 | 1 | 0 | |a AEROMAGNETIC SURVEY |
| 690 | 1 | 0 | |a DATA INTERPRETATION |
| 690 | 1 | 0 | |a EXTENSIONAL TECTONICS |
| 690 | 1 | 0 | |a MAGNETIC FIELD |
| 690 | 1 | 0 | |a MAGNETIC SUSCEPTIBILITY |
| 690 | 1 | 0 | |a NEOTECTONICS |
| 690 | 1 | 0 | |a PLIOCENE-PLEISTOCENE BOUNDARY |
| 690 | 1 | 0 | |a REMANENT MAGNETIZATION |
| 690 | 1 | 0 | |a STRUCTURAL GEOLOGY |
| 690 | 1 | 0 | |a TROUGH |
| 690 | 1 | 0 | |a ANDES |
| 700 | 1 | |a Gimenez, M.E. | |
| 700 | 1 | |a Gianni, G.M. | |
| 700 | 1 | |a Folguera, A. | |
| 700 | 1 | |a Martinez, P. | |
| 773 | 0 | |d Elsevier Ltd, 2019 |g v. 89 |h pp. 55-62 |p J. South Am. Earth Sci. |x 08959811 |w (AR-BaUEN)CENRE-1080 |t Journal of South American Earth Sciences | |
| 856 | 4 | 1 | |u https://www.scopus.com/inward/record.uri?eid=2-s2.0-85056585505&doi=10.1016%2fj.jsames.2018.11.001&partnerID=40&md5=235c5c07a8bc9c69a8651f1a8f93c994 |y Registro en Scopus |
| 856 | 4 | 0 | |u https://doi.org/10.1016/j.jsames.2018.11.001 |y DOI |
| 856 | 4 | 0 | |u https://hdl.handle.net/20.500.12110/paper_08959811_v89_n_p55_Pesce |y Handle |
| 856 | 4 | 0 | |u https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08959811_v89_n_p55_Pesce |y Registro en la Biblioteca Digital |
| 961 | |a paper_08959811_v89_n_p55_Pesce |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 86787 | ||