1887
Volume 27, Issue 5
  • E-ISSN: 1365-2117

Abstract

Abstract

Although the Neuquén basin in Argentina forms a key transitional domain between the south‐central Andes and the Patagonian Andes, its Cenozoic history is poorly documented. We focus on the sedimentologic and tectonic evolution of the southern part of this basin, at 39–40°30′S, based on study of 14 sedimentary sections. We provide evidence that this basin underwent alternating erosion and deposition of reworked volcaniclastic material in continental and fluvial settings during the Neogene. In particular, basement uplift of the Sañico Massif, due to Late Miocene–Pliocene intensification of tectonic activity, led to sediment partitioning in the basin. During this interval, sedimentation was restricted to the internal domain and the Collon Cura basin evolved towards an endorheic intermontane basin. From stratigraphic interpretation, this basin remained isolated 7–11 Myr. Nevertheless, ephemeral gateways seem to have existed, because we observe a thin succession downstream of the Sañico Massif contemporaneous with the Collon Cura basin‐fill sequence. Comparisons of stratigraphic, paleoenvironmental and tectonic features of the southern Neuquén basin with other foreland basins of South America allow us to classify it as a broken foreland with the development of an intermontane basin from Late Miocene to Late Pliocene. This implies a thick‐skinned structural style for this basin, with reactivation of basement faults responsible for exhumation of the Sañico Massif. Comparison of several broken forelands of South America allows us to propose two categories of intermontane basins according to their structural setting: subsiding or uplifted basins, which has strong implications on their excavation histories.

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2014-09-29
2020-05-25
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References

  1. Allmendinger, R.W., Ramos, V.A., Jordan, T.E., Palma, M. & Isacks, B.L. (1983) Paleogeography and Andean structural geometry, northwest Argentina. Tectonics, 2, 1–16.
    [Google Scholar]
  2. Assine, M.L. & Soares, P.C. (2004) Quaternary of the Pantanal, west‐central Brazil. Quat. Int., 114, 23–34.
    [Google Scholar]
  3. Barrio, C., Carlini, A.A. & Goin, F.J. (1989) Litogenesis y antiguedad de la F. Chichinales de Paso Cordova (Rio Negro, Argentina).. Actas 4° Congreso Argentino de Paleontologia y Bioestigrafia, 4, 149–156.
    [Google Scholar]
  4. Bilmes, A., D'Elia, L., Franzese, J.R., Veiga, G.D. & Hernández, M. (2013) Miocene block uplift and basin formation in the Patagonian foreland: the Gastre Basin, Argentina. Tectonophysics, 601, 98–111.
    [Google Scholar]
  5. Branney, M. & Kokelaar, B.P. (2002) Sedimentation of ignimbrites from pyroclastic density currents. Memoir of the Geological Society of London, 27, 150 pp.
  6. Burns, W., Jordan, T., Copeland, P & Kelley, S. (2006) The case for extensional tectonics in the Oligocene‐Miocene Southern Andes as recorded in the Cura Mallin basin (36°–38°S). In: Evolution of an Andean Margin: A Tectonic and Magmatic View from the Andes to the Neuquén Basin (35°–39°S lat) (Ed. by Kay, S.M. & Ramos, V.A. ) Geol. S. Am. S. 407, 163–184.
    [Google Scholar]
  7. Catuneanu, O. (2004) Retroarc foreland systems‐evolution through time. J. Afr. Earth Sci., 38, 225–242.
    [Google Scholar]
  8. Cazau, L., Mancini, D., Cangini, J. & Spalletti, L. (1989) Cuenca de Ñirihuau. In: Cuencas Sedimentarias Argentinas, Serie Correlacion Gologica (Ed. by G.Chebli & L.Spalletti ), 6, 299–318. Instituto Superior de Correlacion Geologica, San Miguel de Tucuman.
    [Google Scholar]
  9. Chase, C.G., Sussman, A.J. & Coblentz, D.D. (2009) Curved Andes: Geoid forebulge, and flexure. Lithosphere, 1, 358–363.
    [Google Scholar]
  10. Cobbold, P.R. & Rossello, E.A. (2003) Aptian to recent compressional deformation, foothills of the Neuquén Basin, Argentina. Mar. Petrol. Geol., 20, 429–443.
    [Google Scholar]
  11. Covey, M. (1986) The evolution of foreland basins to steady state: evidence from the western Taiwan foreland basin. In: Foreland Basins (Ed. by P.A.Allen & P.Homewood ), Blackwell Scientific, Spec. Pub. Int. Ass. Sediment, 8, 77–90.
    [Google Scholar]
  12. Crampton, S.L. & Allen, P.A. (1995) Recognition of forebulge unconformities associated with early stage foreland basin development: example from the North Alpine foreland basin. AAPG Bull., 79, 1495–1514.
    [Google Scholar]
  13. Cucchi, R., Leanza, H.A., Repol, D., Escosteguy, L., Gonzalez, R. & Daniela, J.C. (2005) Hoja Geologica 3972‐IV, Junin de Los Andes. Provincia del Neuquén. Instituto de Geologia y Recursos Minerales, Servicio Geologico Minero Argentino, 357, 102.
    [Google Scholar]
  14. Dávila, F.M. & Astini, R.A. (2003) Early Middle Miocene broken foreland development in the southern Central Andes: evidence for extension prior to regional shortening. Basin Res., 15, 379–396.
    [Google Scholar]
  15. Dávila, F.M., Giménez, M.E., Nòbile, J.C. & Martinez, M.P. (2012) The evolution of the high‐elevated depocenters of the northern Sierras Pampeanas (ca. 28° SL), Argenine broken foreland, South‐Central Andes: the Pipanaco Basin. Basin Res., 24, 615–636.
    [Google Scholar]
  16. DeCelles, P.G. & Giles, K.A. (1996) Foreland basin systems. Basin Res., 8, 105–123.
    [Google Scholar]
  17. DeCelles, P.G. & Horton, B.K. (2003) Early to middle Tertiary foreland basin development and the history of Andean crustal shortening in Bolivia. Geol. Soc. Am. Bull., 115, 58–77.
    [Google Scholar]
  18. DeCelles, P.G., Carrapa, B., Horton, B.K. & Gehrels, G.E. (2011) Cenozoic foreland basin system in the central Andes of northwestern Argentina: implications for Andean geodynamics and modes of deformation. Tectonics, 30, doi:10.1029/2011TC002948.
    [Google Scholar]
  19. D'Elia, L., Muravchik, M., Franzese, J.R. & Lopez, L. (2012) Tectonostratigraphic analysis of the Late Triassic‐Early Jurassic syn‐rift sequence of the Neuquén Basin in the Sanico depocentre, Neuquén Province, Argentina. Andean Geol., 39, 133–157.
    [Google Scholar]
  20. Dessanti, R.N. (1972) Andes Patagonicos Septentrionales. In: Geologia Regional Argentina (Ed. by A.F.Leanza ), pp. 655–688. Academia Nacional de Ciencias, Cordoba.
    [Google Scholar]
  21. Doering, A. (1882) Geologia. In: Informe official de la Comision Cientifica agregada al Estado Mayor General de la Expedicion al Rio Negro (Patagonia) realizada en los meses de Abril, Mayo y Junio de 1879, bajo las ordened del General Julio A. Roca, 3a parte, Geologia, pp. 299–530, Buenos Aires.
    [Google Scholar]
  22. Escosteguy, L. & Franchi, M. (2010) Estratigrafia de la region de Chapelco, Provincia del Nqueuén. Revista de la Asociacion Geologica Argentina, 66, 418–429.
    [Google Scholar]
  23. Fisher, R.V. (1961) Proposed classification of volcanoclastic sediments and rocks. Geol. Soc. Am. Bull., 72, 1409–1414.
    [Google Scholar]
  24. Flemings, P.B. & Jordan, T. (1989) A synthetic stratigraphic model of foreland basin development. J. Geophys. Res., 94, 3851–3866.
    [Google Scholar]
  25. Flint, R.F. & Fidalgo, F. (1968) Drift glacial al este de los Andes entre Bariloche y Esquel. Inst. Nac. Geol. y Min Bol., 119, 1–14.
    [Google Scholar]
  26. Folguera, A. & Ramos, V.A. (2011) Repeated eastward shifts of arc magmatism in the Southern Andes: a revision to the long‐term pattern of Andean uplift and magmatism. J. S. Am. Earth Sci., 32, 531–546.
    [Google Scholar]
  27. Folguera, A. & Zarate, M. (2011) Neogene sedimentation in the Argentine foreland between 34°30′S and 41°S and its relation to the Andes evolution. In: Cenozoic Geology of the Central Andes of Argentina: Salta (Ed. by JASalfity , RAMarquillas ), pp. 123–134. SCS Publisher, Salta.
    [Google Scholar]
  28. Folguera, A., Zapata, T. & Ramos, V.A. (2006) Late Cenozoic extension and the evolution of the Neuquén Andes. In: Evolution of an Andean margin: a tectonic and magmatic view from the Andes to the Neuquén basin (35° ‐ 39° S lat.) (Ed. by S.Kay & V.Ramos ), Geol. S. Am. S., 407, 267–285.
    [Google Scholar]
  29. Folguera, A., Introcaso, A., Giménez, M., Ruiz, F., Martinez, P., Tunstall, C., Garcia, M. & Ramos, V.A. (2007) Crustal attenuation in the southern Andean retroarc (30°‐39°30′S) determined from tectonic and gravimetric studies: the Lonco‐Luan asthenospheric anomaly. Tectonophysics, 439, 129–147.
    [Google Scholar]
  30. Fossa Mancini, E., Feruglio, E. & Yussen de Campana, J.C. (1938) Una reunion de geologos de Y.P.F. y el problema de la terminologia estratigrafica. Boletin de Informaciones Petroleras, 15, 1–67.
    [Google Scholar]
  31. Franzese, J.R. & Spalletti, L.A. (2001) Late Triassic‐early Jurassic continental extension in southwestern Gondwana: tectonic segmentation and pre‐break‐up rifting. J. S. Am. Earth Sci., 14, 257–270.
    [Google Scholar]
  32. Galland, O., Hallot, E., Cobbold, P.R., Ruffet, G. & de Bremond d'Ars, J. (2007) Volcanism in a compressional Andean setting: a structural and geochronological study of Tromen volcano (Neuquén province, Argentina). Tectonics, 26, , doi: 10.1029/2006TC002011.
    [Google Scholar]
  33. Galli, C.A. (1954) Acerca de una nueva interpretacion de las Formaciones Rético‐liasicas de la Patagonia septentrional. Revista de la Asociacion Geologica Argentina, 8, 220–235.
    [Google Scholar]
  34. Galli, C.A. (1969) Descripcion geologica de la Hoja 38c, Piedra del Aguila, Prov. Del Neuquén y Rio Negro. Dir. Nac. Geol. Min. Bol., 111, 65.
    [Google Scholar]
  35. García Morabito, E.G. & Ramos, V.A. (2012) Andean evolution of the Aluniné fold and thrust belt, Northern Patagonian Andes (38°30′‐40°30′S). J. S. Am. Earth Sci., 38, 13–30.
    [Google Scholar]
  36. García Morabito, E.G., Götze, H.J. & Ramos, V.A. (2011) Tertiary tectonics of the Patagonian Andes retro‐arc area between 38°15′ and 40°S latitude. Tectonophysics, 499, 1–21.
    [Google Scholar]
  37. Giacosa, R., Heredia, N., Césari, O. & Zubia, M. (2001) Hoja Geologica 4172‐IV, San Carlos de Bariloche (provincias de Rio Negro and Neuquén). Instituto de Geologico Minero Argentino279, 67.
    [Google Scholar]
  38. Giambiagi, L.B., Tunik, M. & Ghiglione, M. (2001) Cenozoic tectonic evolution of the Alto Tunuyann foreland basin above the transition zone between the flat and normal subduction segment (33°30′‐34°S), western Argentina. J. S. Am. Earth Sci., 14, 707–724.
    [Google Scholar]
  39. Gonzalez Diaz, E.F. & Nullo, F. (1980) Cordillera Neuquina. Segundo Simposio de Geologia Regional Argentina, Academia Nacional de Ciencas, 2, 1099–1147.
    [Google Scholar]
  40. Gonzalez Diaz, E.F., Riggi, J.C. & Fauque, L. (1986) Formacion Caleufu (Nov. Nom): reinterpretacion de las Formationes Rio Negro y Alicura, en el area de Collon Cura, sur del Neuquén. Asociación Geológica Argentina, Revista XLI, 1–2, 81–105.
    [Google Scholar]
  41. Gonzalez Diaz, E.F., Ostera, H.A., Riggi, J.C. & Fauqué, L. (1990) Una propuesta temporal acerca del Miembro Limay Chico (ex “Rionegrense”) de la Formacion Caleufu, en el valle del rio Collon Cura y adyacencias (SE del Neuquén). 11° Congreso Geologico Argentino (San Juan), 2, 243–246.
    [Google Scholar]
  42. Gracia, R. (1958) Informe geologicode las Cartas Paso Flores y Traful. Secret. Ejerc. Direc. Gral. Ing., Buenos Aires.
  43. Grier, M.E., Salfity, J.A. & Allmendinger, R.W. (1991) Andean reactivation of the Cretaceous Salta rift, northwestern Argentina. J. S. Am. Earth Sci., 4, 351–372.
    [Google Scholar]
  44. Hain, M.P., Strecker, M.R., Boohkagen, B., Alonso, R.N., Pingel, H. & Schmitt, A.K. (2011) Neogene to Quaternary broken foreland formation and sedimentation dynamics in the Andes of NW Argentina (25°S). Tectonics, 30, doi: 10; 1029/2010TC002703.
    [Google Scholar]
  45. Hilley, G.E. & Strecker, M.R. (2005) Processes of oscillatory basin filling and excavation in a tectonically active orogen: Quebrada del Toro Basin, NW Argentina. Geol. Soc. Am. Bull., 117, 887–901.
    [Google Scholar]
  46. Horton, B.K. & DeCelles, P.G. (1997) The modern foreland basin system adjacent to the Central Andes. Geology, 25, 895–898.
    [Google Scholar]
  47. Horton, B.K. & DeCelles, P.G. (2001) Modern and ancient fluvial megafans in the foreland basin system of the central Andes, southern Bolivia: implications for drainage network evolution in fold‐thrust belts. Basin Res., 13, 43–63.
    [Google Scholar]
  48. Hugo, C.A. & Leanza, H.A. (2001) Hoja Geologica 3669‐IV, General Roca. Provincia del Neuquén. Instituto de Geologia y Recursos Minerales, Servicio Geologico Minero Argentino308, 70.
    [Google Scholar]
  49. Iriondo, M. (2004) Large Wetland of South America: a model for Quaternary humid environments. Quat. Int., 114, 3–9.
    [Google Scholar]
  50. Jordan, T.E. (1995) Retroarc Foreland and Related Basins. In: Tectonics of Sedimentary Basins (Ed. by C.J.Busby , R.V.Ingersoll ), pp. 331–362. Blackwell Science, Oxford.
    [Google Scholar]
  51. Kay, S.M., Burns, M., Copeland, P. & Mancilla, O. (2006) Upper Cretaceous to Hollocene magmatism and evidence for transient Miocene shallowing of the Andean subduction zone under the northern Neuquén Basin. In: Evolution of an Andean Margin: A Tectonic and Magmatic view from the Andes to the Neuquén Basin (35° ‐ 39° S lat.) (Ed. by S.Kay & V.Ramos ), Geol. S. Am. S., 407, 19–60.
    [Google Scholar]
  52. Leanza, H.A. (1985) Descripcion geologica de la Hoja 36b, cerro Chachil, provincia del Neuquen. Servicio Geologico Nacional, 114 p.
  53. Leanza, H.A., Hugo, C.A., Herrero, J.C., Donnari, E. & Pucci, J.C. (1997) Hoja Geologica 3969‐III, Picun Leufu. Instituto de Geologia y Recursos Minerales, Servicio Geologico Minero Argentino: Boletin218, 135.
    [Google Scholar]
  54. Manceda, R. & Figueroa, D. (1995) Inversion of the Mesozoic Neuquén rift in the Malargüe fold and thrust belt, Mendoza, Argentina. In: Petroleum Basins of South America (Ed. by A.J.Tankard , R.Suàrez , R.Soruco & H.J.Welskink ) AAPG Memoirs, 62, 369–382.
    [Google Scholar]
  55. Marshall, L.G., Pascual, L., Curtis, G.H. & Drake, R.E. (1977) South American geochronology: radiometric time scale for middle to late Tertiary mammal‐bearing horizons in Patagonia. Science, 195, 1325–1328.
    [Google Scholar]
  56. Mazzoni, M. & Benvenuto, A. (1990) Radiometric ages of tertiary ignimbrites and the Collon Cura Formation, northwestern Patagonia. 11° Congreso Geologico Argentino, 1, 87–90.
    [Google Scholar]
  57. Mazzoni, M.M. & Rapela, C.W. (1991) Caracteristicas quimicas e isotopicas de ignimbritas Miocenas. Andes Patagonicos septentrionales (SVZ), Argentina. Congreso Geologico Chileno, 6, 125–128.
    [Google Scholar]
  58. McGlue, M.M. & Cohen, A.S. (2006) The evolution of topographic closure and foreland basin lakes: a modern time‐slice perspective from the Andes. Geol. Soc. Am., Abstract with Programs. 38, 368.
    [Google Scholar]
  59. Messager, G., Nivière, B., Martinod, J., Lacan, P. & Xavier, J.‐P. (2010) Geomorphic evidence for Pio‐Quaternary compression in the Andean foothills of the southern Neuquén Bain, Argentina. Tectonics, 29, doi:10.1029/2009TC002609.
    [Google Scholar]
  60. Molnar, P. & England, P. (1990) Late Cenozoic uplift of mountain ranges and global climate change: chiken or egg ?Nature, 346, 29–34.
    [Google Scholar]
  61. Mortimer, E., Carrapa, B., Coutand, I., Schoenbohm, L., Sobel, E.R., Gomez, J.S. & Strecker, M.R. (2007) Fragmentation of a foreland basin in response to out‐of‐sequence basement uplifts and structural reactivations: El Cajon‐Campo del Arenl basin, NW Argentina. Geol. Soc. Am. Bull., 119, 637–653.
    [Google Scholar]
  62. Mosquera, A. & Ramos, V.A. (2006) Intraplate deformation in the Neuquén Embayment. In: Evolution of an Andean margin: A Tectonic and Magmatic View from the Andes to the Neuquén Basin (35°‐39°S lat) (Ed. by S.M.Kay & V.A.Ramos ), Geol. S. Am. S., 407, 97–123.
    [Google Scholar]
  63. Mouthereau, F., Watts, A. & Burov, E. (2013) Structure of orogenic belts controlled by lithosphere age. Nature Geosci., 6, 785–789.
    [Google Scholar]
  64. Nivière, B., Messager, G., Carretier, S. & Lacan, P. (2013) Geomorphic expression of the southern Central Andes forebulge (37°S, Argentina). Terra Nova, 25, 361–367. doi:10.1111/ter.12044.
    [Google Scholar]
  65. Nullo, F. (1979) Descripcion geologica de la Hoja 39c, Paso Flores, provincias de Rio Negro y Neuquén. Servicio Geologico Nacional, Boletin, 167, 73p.
    [Google Scholar]
  66. del Papa, C., Hongn, F., Powell, J., Payrola, P., Do Campo, M., Strecker, M.R., Petrinovic, I., Schmitt, A.K. & Pereyra, P. (2013) Middle Eocene‐Oligocene broken‐foreland evolution in the Andean Calchaqui Valley, NW Argentina: insights from stratigraphic, structural and provenance studies. Basin Res., 25, 574–593.
    [Google Scholar]
  67. Pardo‐Casas, F. & Molnar, P. (1987) Relative motion of the Nazca (Farallon) and South American plates since Lates Cretaceous time. Tectonics, 6, 233–248.
    [Google Scholar]
  68. Pascual, R. & Odreman Rivas, O. (1971) Evolucion de las comunidades de los vertebrados del Terciario Argentino. Los aspectos paleozoogeograficos y paleoclimaticos relacionados. Ameghiniana, 8, 372–412.
    [Google Scholar]
  69. Pascual, R.P., Bondesio, M.G., Vucetich, G., Scillato Yañe, G., Bond, M. & Tonni, E.P. (1984) Vertebrados fosiles cenozoicos. Relatorio 9° Congreso Geologico Argentino, 2, 439–461.
    [Google Scholar]
  70. Peizhen, Z., Molnar, P. & Downs, W.R. (2001) Increase sedimentation rates and grain sizes 2‐4 Myr ago due to the influence of climate change on erosion rates. Nature, 410, 891–897.
    [Google Scholar]
  71. Pozzo, A. (1956) Descripcion geologica de la zona Bajo de Ortiz‐Cañadon Lonco Vaca, provincia de Rio Negro. Informe Inédito, Y.P.F.
  72. Rabassa, J. (1975) Geologia de la region de Pilcaniyeu‐Comallo, Provincia de Rio Negro, Argentina. Publicacion Fundacion Bariloche, Departamento Recursos Naturales y Energéticos, 17, 129p., San Carlos de Bariloche.
  73. Ramos, V.A. (1999) Evolución tectónica de la Argentina. In: Geología Argentina (Ed. by R.Caminos ), Instituto de Geologiía y Recursos Minerales, 29, 715–759.
    [Google Scholar]
  74. Ramos, V.A. & Folguera, A. (2005) Tectonic evolution of the Andes of Neuquén: constraints derived from the magmatic arc and foreland deformation in the Neuquén Basin: a case study. In: Sequence Stratigraphy and Basin Dynamics (Ed. by G.D.Veiga ), Geol. Soc. Sp., 252, 15–35.
    [Google Scholar]
  75. Ramos, V.A. & Kay, S.M. (2006) Overview of the tectonic evolution of the southern Central Andes of Mendoza and Neuquén (35°‐39°S latitude). In: Evolution of an Andean Margin: A Tectonic and Magmatic View from the Andes to the Neuquén Basin (35°‐39°S lat) (Ed. by S.M.Kay & V.A.Ramos ), Geol. S. Am. S., 407, 1–18.
    [Google Scholar]
  76. Ramos, V.A., Cristallini, E. & Pérez, D.J. (2002) The Pampean flat‐slab of the Central Andes. J. S. Am. Earth Sci., 15, 59–78.
    [Google Scholar]
  77. Ramos, V.A., Litvak, V., Folguera, A. & Spagnuolo, M. (2014a) An Andean tectonic cycle: from crustal thickening to extension in a thin crust (34°‐37°SL). Geosci. Front., 5, 351–367.
    [Google Scholar]
  78. Ramos, M.E., Folguera, A., Fennel, L., Giménez, M., Litvak, V.D., Dzierma, Y. & Ramos, V.A. (2014b) Tectonic evolution of the North Patagonian Andes from field and gravity data (39‐40°S). J. S. Am. Earth Sci., 51, 59–75.
    [Google Scholar]
  79. Rojas Vera, E.A., Folguera, A., Valcarce, G.Z., Giménez, M., Ruiz, F., Martínez, P., Bottesi, G. & Ramos, V.A. (2010) Neogene to Quaternary extensional reactivation of a fold and thrust belt: the Agrio belt in the Southern Central Andes and its relation to the Loncopue' trough (38–39°S). Tectonophysics, 492, 279–294.
    [Google Scholar]
  80. Rojas Vera, E.A., Folguera, A., Zamora Valcarce, G., Bottesi, G. & Ramos, V.A. (2014) Structure and development of the Andean system between 36° and 39°S. J. Geodyn., 73, 34–52.
    [Google Scholar]
  81. Rolleri, E., Dellapé, D.A. & Manceñido, M.O. (1984) Relaciones estratigraphicas y correlación de las Formaciones Pichi Picún Leufú y Collón Cura (Miembro Naupa Huen) aflorantes en el curso iferior y medio del cañadón Michihuau, provincia de Río Negro. 9° Congreso Geológico, 1, 257–265.
    [Google Scholar]
  82. Roth, S. (1899) Reconocimiento de la region andina de la Republica Argentina. Apuntes sobre la geologia y paleontologia de Rio Negro y Neuquén. Revista Museo de La Plata, 9, 141–197.
    [Google Scholar]
  83. Sempere, T.R.F., Butler, D.R., Richards, L.G., Marshall, L.G., Sharp, W. & Swisher, C.C. (1997) Stratigraphy and chronology of Late Cretaceous‐early Paleogene strata in Bolivia and northwest Argentina. Geo. Soc. Am. Bull., 109, 709–727.
    [Google Scholar]
  84. Siks, B.C. & Horton, B.K. (2011) Growth and fragmentation of the Andean foreland basin during eastward advance of fold‐thrust deformation, Puna plateau and Eastern Cordillera, northern Argentina. Tectonics, 30, doi:10.1029/2011TC002944.
    [Google Scholar]
  85. Silvestro, J., Kraemer, P., Achilli, F. & Brinkworth, W. (2005) Evolucion de las cuencas sinorogenicas de la Cordillera Principal entre 35°‐36°S, Malargue. Revista de la Asociacion Geologica Argentina, 60, 627–643.
    [Google Scholar]
  86. Somoza, R. (1998) Updated Nazca (Farallon)‐South America relative motions during the last 40 My: implications for mountain building in the central Andean region. J. S. Am. Earth Sci., 11, 211–215.
    [Google Scholar]
  87. Steinmann, G. (1929) Geologie von Peru. University Buchhandlung, Heidelberg, Germany, 448 pp.
    [Google Scholar]
  88. Strecker, M.R., Hilley, G.E., Bookhagen, B. & Sobel, E.R. (2011) Structural, geomorphic, and depositional characteristics of contiguous and broken foreland basins: examples from the eastern flanks of the central Andes in Bolivia and NW Argentina. In: Tectonics of Sedimentary Basins: Recent Advances (Ed. by CBusby , AAzor ), pp. 506–521. Blackwell, Boston, MA.
    [Google Scholar]
  89. Tunik, M., Folguera, A., Naipauer, M., Pimentel, M. & Ramos, V.A. (2010) Early uplift and orogenic deformation in the Neuquén Basin: constraints on the Andean uplift from U‐Pb and Hf isotopic data of detrital zircons. Tectonophysics, 489, 258–273.
    [Google Scholar]
  90. Turcotte, D.L. & Schubert, G. (2002) Geodynamics, 2nd edn. Cambridge University Press, Cambridge.
    [Google Scholar]
  91. Turner, J.C.M. (1973) Descripcion geologica de la Hoja 37 a‐b, Junin de los Andes, provincia del Neuquén. Servicio Nacional Minero Geologico, Boletin138, 86p., Buenos Aires.
  92. Uliana, M.A. (1979) Geologia de la region comprendida entre los rios Colorado y Negro, provincias de Neuquen y Rio Negro. Tesis Doctoral, Universidad Nacional de La Plata, 117 p.
  93. Uliana, M.A. & Legarreta, L. (1993) Hydrocarbons habitat in a Triassic‐to‐Cretaceous Sub‐Andean setting: Neuquén Basin, Argentina. J. Petrol. Geol., 16, 397–420.
    [Google Scholar]
  94. Urien, C.M. & Zambrano, J.J. (1994) Petroleum systems in the Neuquén Basin, Argentina. In: The Petroleum System‐from Source to Trap (Ed. by L.B.Magoon & W.G.Dow ), AAPG Memoir, 60, 513–534.
    [Google Scholar]
  95. Vergani, G.D., Tankard, A.J., Belotti, H.J. & Welsink, H.J. (1995) Tectonic evolution and paleogeography of the Neuquén Basin, Argentina. In: Petroleum Basins of South America (Ed. by A. J.Tankard , R.Suàrez , R.Soruco & H. J.Welskink ), AAPG Memoir, 62, 383–402.
    [Google Scholar]
  96. White, J.D.L. & Houghton, B.F. (2006) Primary volcaniclastic rocks. Geology, 34, 677–680.
    [Google Scholar]
  97. Wichmann, R. (1927) Los estratos con dinosaurios y su techo en el este del Territorio del Neuquén. Publicacion Direccion General de Mineria, Geologia e Hidrologia, 32, 1–25.
    [Google Scholar]
  98. Windhausen, A. (1918) The problem of the Cretaceous/Tertiary boundary in South America, and the stratigraphic position of the San Jorge Formation in Patagonia. Am. J. Sci., 44, 1–53.
    [Google Scholar]
  99. Windhausen, A. (1922) Estudios geolocicos en el valle superior del Rio Negro. Ministerio de Agricultura, Direccion General de Minas, Geologia e Hidrologia 29 (Serie B), 89 p., Buenos Aires.
  100. Yrigoyen, M.R. (1969) Problemas estratigraficos del tertciaro de Argentina. Ameghiniana, 6, 315–329.
    [Google Scholar]
  101. Zamora Valcarce, G., Zapata, T., del Pino, D. & Ansa, A. (2006) Structural evolution of the Agrio fold and thrust belt. In: Evolution of an Andean Margin: A Tectonic and Magmatic View from the Andes to the Neuquén Basin (35° ‐ 39° S lat.) (Ed. by S.Kay & V.Ramos ), Geol. S. Am. S., 407, 125–145.
    [Google Scholar]
  102. Zapata, T. & Folguera, A. (2005) Tectonic evolution of the Andean Fold and Trhust Belt of the Southern Neuquén Basin, Argentina. In: The Neuquén Basin: A Case Study in Sequence Stratigraphy and Basin Dynamics (Ed. by G.D.Veiga , L.A.Spalletti , J.A.Howell & E.Schwarz ), Geol. Soc. London, Spec. Pub., 252, 37–56.
    [Google Scholar]
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