Tectonostratigraphic history of the Neogene Maimará basin, Northwest Argentina
This paper presents the tectonostratigraphic evolution of the Maimará Basin and explores the relationship between the clastic sediments and pyroclastic deposits in the basin and the evolution of the adjacent orogeny and magmatic arc. The sedimentary facies in this part of the basin include, in ascen...
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2016
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| LEADER | 27837caa a22017417a 4500 | ||
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| 001 | PAPER-15518 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230607131904.0 | ||
| 008 | 190411s2016 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-84988005907 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Galli, C.I. | |
| 245 | 1 | 0 | |a Tectonostratigraphic history of the Neogene Maimará basin, Northwest Argentina |
| 260 | |b Elsevier Ltd |c 2016 | ||
| 270 | 1 | 0 | |m Galli, C.I.; INECOA-Facultad de Ingeniería, Universidad Nacional de Jujuy, Av. Bolivia 1661, S.S. de Jujuy, Facultad de Ciencias Naturales, Universidad Nacional de SaltaArgentina; email: claudiagalli@fibertel.com.ar |
| 506 | |2 openaire |e Política editorial | ||
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| 520 | 3 | |a This paper presents the tectonostratigraphic evolution of the Maimará Basin and explores the relationship between the clastic sediments and pyroclastic deposits in the basin and the evolution of the adjacent orogeny and magmatic arc. The sedimentary facies in this part of the basin include, in ascending order, an ephemeral fluvial system, a deep braided fluvial system and a medial to distal ephemeral fluvial system. We interpret that Maimará Formation accumulated in a basin that has developed two stages of accumulation. Stage 1 extended from 7 to 6.4 Ma and included accelerated tectonic uplift in the source areas, and it corresponds to the ephemeral fluvial system deposits. Stage 2, which extended from 6.4 to 4.8 Ma, corresponds to a tectonically quiescent period and included the development of the deep braided fluvial system deposits. The contact between the Maimará and Tilcara formations is always characterized by a regional unconformity and, in the study area, also shows pronounced erosion. Rare earth element and other chemical characteristics of the tuff intervals in the Maimará Formation fall into two distinct groups suggesting the tuffs were erupted from two distinct late Miocene source regions. The first and most abundant group has characteristics that best match tuffs erupted from the Guacha, Pacana and Pastos Grandes calderas, which are located 200 and 230 km west of the study area at 22º-23º30′S latitude. The members the second group are chemically most similar to the Merihuaca Ignimbrite from the Cerro Galán caldera 290 km south-southwest of the studied section. The distinctive geochemical characteristics are excellent tools to reconstruct the stratigraphic evolution of the Neogene Maimará basin from 6.4 to 4.8 Ma. © 2016 Elsevier Ltd |l eng | |
| 536 | |a Detalles de la financiación: Agencia Córdoba Ciencia, SECTER 08/E036, 08/E037, PICT-2012-1984 | ||
| 536 | |a Detalles de la financiación: This research was funded by the AGENCIA ( PICT-2012-1984 ), UNJu ( SECTER 08/E036 and 08/E037 ), and UNSa ( CI-UNSa ). We thank Roberto Liquin, Paulino Cachizumba and Robert Kay for their support of the laboratory work and Silvia Rosas for her assistance with the graphics and layout. We are grateful for constructive reviews by constructive and positive reviews by Brian Horton and anonymous reviewer. | ||
| 593 | |a INECOA-Facultad de Ingeniería, Universidad Nacional de Jujuy, Facultad de Ciencias Naturales, Universidad Nacional de Salta, Av. Bolivia 1661, S.S. de Jujuy, Salta, Argentina | ||
| 593 | |a INECOA-CONICET, Instituto de Geología y Minería, Av. Bolivia, S.S. de Jujuy, 1661, Argentina | ||
| 593 | |a CEGA-CONICET, Universidad Nacional de Salta, Campo Castañares, Salta, 4400, Argentina | ||
| 593 | |a CONICET-INGEODAV, Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales (FCEyN), Universidad de Buenos Aires, Ciudad Universitaria, Pabellón 2, Buenos Aires, C1428EHA, Argentina | ||
| 593 | |a IGeBA -CONICET, Departamento de Ciencias Geológicas, Facultad de Ciencias Exactas y Naturales (FCEyN), Universidad de Buenos Aires, Ciudad Universitaria, Pabellón 2, Buenos Aires, C1428EHA, Argentina | ||
| 593 | |a Departments of Earth and Atmospheric Sciences, Cornell University, Ithaca, NY, United States | ||
| 690 | 1 | 0 | |a GEOCHEMISTRY TUFFS |
| 690 | 1 | 0 | |a HUMAHUACA |
| 690 | 1 | 0 | |a MAIMARA FORMATION |
| 690 | 1 | 0 | |a PALEOMAGNETISM |
| 690 | 1 | 0 | |a PROVENANCE |
| 690 | 1 | 0 | |a BASIN EVOLUTION |
| 690 | 1 | 0 | |a CALDERA |
| 690 | 1 | 0 | |a FLUVIAL DEPOSIT |
| 690 | 1 | 0 | |a IGNEOUS GEOCHEMISTRY |
| 690 | 1 | 0 | |a NEOGENE |
| 690 | 1 | 0 | |a PALEOMAGNETISM |
| 690 | 1 | 0 | |a PROVENANCE |
| 690 | 1 | 0 | |a TECTONOSTRATIGRAPHY |
| 690 | 1 | 0 | |a TUFF |
| 690 | 1 | 0 | |a UPLIFT |
| 651 | 4 | |a ARGENTINA | |
| 700 | 1 | |a Coira, B.L. | |
| 700 | 1 | |a Alonso, R.N. | |
| 700 | 1 | |a Iglesia Llanos, M.P. | |
| 700 | 1 | |a Prezzi, C.B. | |
| 700 | 1 | |a Kay, S.M. | |
| 773 | 0 | |d Elsevier Ltd, 2016 |g v. 72 |h pp. 137-158 |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-s2.0-84988005907&doi=10.1016%2fj.jsames.2016.09.007&partnerID=40&md5=a2ae3e18c40171086d5d96b608e26275 |y Registro en Scopus |
| 856 | 4 | 0 | |u https://doi.org/10.1016/j.jsames.2016.09.007 |y DOI |
| 856 | 4 | 0 | |u https://hdl.handle.net/20.500.12110/paper_08959811_v72_n_p137_Galli |y Handle |
| 856 | 4 | 0 | |u https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08959811_v72_n_p137_Galli |y Registro en la Biblioteca Digital |
| 961 | |a paper_08959811_v72_n_p137_Galli |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 76471 | ||