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Journal articles on the topic 'Puna plateau'

Author: Grafiati

Published: 4 June 2021

Last updated: 9 February 2022

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1

Schurr, B., G. Asch, A. Rietbrock, et al. "Seismicity and average velocities beneath the Argentine Puna Plateau." Geophysical Research Letters 26, no. 19 (1999): 3025–28. http://dx.doi.org/10.1029/1999gl005385.

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2

Allmendinger, R. W., M. Strecker, J. E. Eremchuk, and P. Francis. "Neotectonic deformation of the southern Puna Plateau, northwestern Argentina." Journal of South American Earth Sciences 2, no. 2 (1989): 111–30. http://dx.doi.org/10.1016/0895-9811(89)90040-0.

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3

Gianni, Guido M., Héctor P. A. García, Agustina Pesce, Marianela Lupari, Marcelo González, and Laura Giambiagi. "Oligocene to present shallow subduction beneath the southern Puna plateau." Tectonophysics 780 (April 2020): 228402. http://dx.doi.org/10.1016/j.tecto.2020.228402.

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4

Coutand, Isabelle, Peter R. Cobbold, Marc de Urreiztieta, et al. "Style and history of Andean deformation, Puna plateau, northwestern Argentina." Tectonics 20, no. 2 (2001): 210–34. http://dx.doi.org/10.1029/2000tc900031.

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5

Calixto, Frank J., Eric Sandvol, Suzanne Kay, et al. "Velocity structure beneath the southern Puna plateau: Evidence for delamination." Geochemistry, Geophysics, Geosystems 14, no. 10 (2013): 4292–305. http://dx.doi.org/10.1002/ggge.20266.

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6

Ducea, M. N., A. C. Seclaman, K. E. Murray, D. Jianu, and L. M. Schoenbohm. "Mantle-drip magmatism beneath the Altiplano-Puna plateau, central Andes." Geology 41, no. 8 (2013): 915–18. http://dx.doi.org/10.1130/g34509.1.

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7

López Steinmetz, Romina Lucrecia, Stefano Salvi, Carisa Sarchi, Carla Santamans, and Lorena Cecilia López Steinmetz. "Lithium and Brine Geochemistry in the Salars of the Southern Puna, Andean Plateau of Argentina." Economic Geology 115, no. 5 (2020): 1079–96. http://dx.doi.org/10.5382/econgeo.4754.

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Abstract The Andean plateau is a small region of South America extending between northwest Argentina, southwest Bolivia, and northern Chile. It concentrates the largest global resources of lithium brines in its numerous salars. Of these, the giant salars in Bolivia and Chile have been relatively well studied; however, only little is known about the smaller but numerous salars in the Argentine Puna region. In this article, we present the results of the first regional-scale reconnaissance exploration of the 12 major salars situated in the southern part of the Puna plateau (24°S–26°30’S). Hydrochemical data indicate that the shallowest brines are characterized by highly variable Li concentrations, with mean Li grades ranging between 57 and 570 mg L−1, and mean Li/Mg ratios from 0.01 to 1.24. A survey of the brine chemistry of the salars across the Puna plateau, including its northern part, has revealed the absence of a geographical pattern in Li+ grade distribution. However, a comparison among mean Li+ grades, Li+/Mg2+ ratios, and the sizes of all salars allows an estimation of their Li mining potential. Specifically, the salt pan of Arizaro represents the highest potential, mainly due to its size; Antofalla-Botijuelas has a large surface and promising Li/Mg ratios for Li recovery via brine evaporation, though its elongated shape is a constraint; and Pastos Grandes, Pozuelos, and Rincón have encouraging Li grades, interesting salar sizes, and relatively easy access. Olaroz, Cauchari, and Hombre Muerto contain the highest Li+ grades in brines of the Argentine Puna and embody the most interesting perspectives of the Argentine plateau in a regional context. Salar sizes could be related to maximum Li+ grade of brines. Larger salars would then be expected to contain brines with higher Li+ grades than smaller ones, which could be considered as a useful criterion for surveys of brine-type deposits.

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8

Henríquez, Susana, Peter G. DeCelles, Bárbara Carrapa, Amanda N. Hughes, George H. Davis, and Patricia Alvarado. "Deformation history of the Puna plateau, Central Andes of northwestern Argentina." Journal of Structural Geology 140 (November 2020): 104133. http://dx.doi.org/10.1016/j.jsg.2020.104133.

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9

Allmendinger, Richard W., Teresa E. Jordan, Suzanne M. Kay, and Bryan L. Isacks. "THE EVOLUTION OF THE ALTIPLANO-PUNA PLATEAU OF THE CENTRAL ANDES." Annual Review of Earth and Planetary Sciences 25, no. 1 (1997): 139–74. http://dx.doi.org/10.1146/annurev.earth.25.1.139.

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10

ALLMENDINGER, RICHARD W. "Tectonic development, southeastern border of the Puna Plateau, northwestern Argentine Andes." Geological Society of America Bulletin 97, no. 9 (1986): 1070. http://dx.doi.org/10.1130/0016-7606(1986)97<1070:tdsbot>2.0.co;2.

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11

Jordan, T. E., P. L. Nester, N. Blanco, G. D. Hoke, F. Dávila, and A. J. Tomlinson. "Uplift of the Altiplano-Puna plateau: A view from the west." Tectonics 29, no. 5 (2010): n/a. http://dx.doi.org/10.1029/2010tc002661.

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12

Allmendinger, R. W., and T. Gubbels. "Pure and simple shear plateau uplift, Altiplano-Puna, Argentina and Bolivia." Tectonophysics 259, no. 1-3 (1996): 1–13. http://dx.doi.org/10.1016/0040-1951(96)00024-8.

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13

Prezzi, Claudia, María Paula Iglesia Llanos, Hans-Jürgen Götze, and Sabine Schmidt. "Thermal and geodynamic contributions to the elevation of the Altiplano–Puna plateau." Physics of the Earth and Planetary Interiors 237 (December 2014): 51–64. http://dx.doi.org/10.1016/j.pepi.2014.10.002.

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14

Bianchi, M., B. Heit, A. Jakovlev, et al. "Teleseismic tomography of the southern Puna plateau in Argentina and adjacent regions." Tectonophysics 586 (February 2013): 65–83. http://dx.doi.org/10.1016/j.tecto.2012.11.016.

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15

Schoenbohm, Lindsay M., and Manfred R. Strecker. "Normal faulting along the southern margin of the Puna Plateau, northwest Argentina." Tectonics 28, no. 5 (2009): n/a. http://dx.doi.org/10.1029/2008tc002341.

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16

Mors, R. Agustin, Ricardo A. Astini, and Fernando J. Gomez. "Coexisting active travertines and tufas in the southeastern border of the Puna plateau." Sedimentary Geology 389 (July 2019): 200–217. http://dx.doi.org/10.1016/j.sedgeo.2019.06.009.

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17

Vandervoort, Dirk S., Teresa E. Jordan, Peter K. Zeitler, and Ricardo N. Alonso. "Chronology of internal drainage development and uplift, southern Puna plateau, Argentine central Andes." Geology 23, no. 2 (1995): 145. http://dx.doi.org/10.1130/0091-7613(1995)023<0145:coidda>2.3.co;2.

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18

Calixto, Frank J., Danielle Robinson, Eric Sandvol, et al. "Shear wave splitting and shear wave splitting tomography of the southern Puna plateau." Geophysical Journal International 199, no. 2 (2014): 688–99. http://dx.doi.org/10.1093/gji/ggu296.

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19

Assumpção, Marcelo, and Mario Araujo. "Effect of the Altiplano-Puna plateau, South America, on the regional intraplate stresses." Tectonophysics 221, no. 3-4 (1993): 475–96. http://dx.doi.org/10.1016/0040-1951(93)90174-i.

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20

Babeyko, Andrey Y., and Stephan V. Sobolev. "Quantifying different modes of the late Cenozoic shortening in the central Andes." Geology 33, no. 8 (2005): 621–24. http://dx.doi.org/10.1130/g21126ar.1.

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Abstract Since the late Miocene, the two main segments of the central Andean high plateau, Altiplano and Puna, demonstrate different styles and magnitudes of tectonic shortening. Through numerical simulation of thermomechanical processes, we show that different shortening modes—pure and simple shear accompanied by thin-or thick-skinned tectonics—might be controlled by strength of the foreland uppermost crust and by temperature of the foreland lithosphere. Mechanical weakening and failure of the thick Paleozoic sediments overlying the cold lithosphere in the Altiplano foreland at 13–9 Ma explains the transition from pure to simple shear shortening accompanied by broad thin-skinned thrusting, started before the major uplift of the plateau. However, the high strength of the uppermost crust combined with a relatively warm lithosphere results in the thick-skinned shortening typical for the foreland of the Puna. Failure of Paleozoic sediments in the Altiplano foreland significantly reduces the force required to shorten the lithosphere, which may be the reason for the increased bulk shortening rate in the late Miocene.

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21

Insel, N., M. Grove, M. Haschke, J. B. Barnes, A. K. Schmitt, and M. R. Strecker. "Paleozoic to early Cenozoic cooling and exhumation of the basement underlying the eastern Puna plateau margin prior to plateau growth." Tectonics 31, no. 6 (2012): n/a. http://dx.doi.org/10.1029/2012tc003168.

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22

Filipovich, Rubén, Walter Báez, Gianluca Groppelli, et al. "Geological Map of the Tocomar Basin (Puna Plateau, NW Argentina). Implication for the Geothermal System Investigation." Energies 13, no. 20 (2020): 5492. http://dx.doi.org/10.3390/en13205492.

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This paper presents a detailed geological map at the 1:20,000 scale of the Tocomar basin in the Central Puna (north-western Argentina), which extends over an area of about 80 km2 and displays the spatial distribution of the Quaternary deposits and the structures that cover the Ordovician basement and the Tertiary sedimentary and volcanic units. The new dataset includes litho-facies descriptions, stratigraphic and structural data and new 234U/230Th ages for travertine rocks. The new reconstructed stratigraphic framework, along with the structural analysis, has revealed the complex evolution of a small extensional basin including a period of prolonged volcanic activity with different eruptive centres and styles. The geological map improves the knowledge of the geology of the Tocomar basin and the local interplay between orogen-parallel thrusts and orogen-oblique fault systems. This contribution represents a fundamental support for in depth research and also for encouraging geothermal exploration and exploitation in the Puna Plateau region.

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23

Babeyko, A. Yu, S. V. Sobolev, R. B. Trumbull, O. Oncken, and L. L. Lavier. "Numerical models of crustal scale convection and partial melting beneath the Altiplano–Puna plateau." Earth and Planetary Science Letters 199, no. 3-4 (2002): 373–88. http://dx.doi.org/10.1016/s0012-821x(02)00597-6.

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24

Aubry, Laurent, Pierrick Roperch, Marc de Urreiztieta, Eduardo Rossello, and Annick Chauvin. "Paleomagnetic study along the southeastern edge of the Altiplano - Puna Plateau: Neogene tectonic rotations." Journal of Geophysical Research: Solid Earth 101, B8 (1996): 17883–99. http://dx.doi.org/10.1029/96jb00807.

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25

Báez, Walter, Gerardo Carrasco Nuñez, Guido Giordano, José G. Viramonte, and Agostina Chiodi. "Polycyclic scoria cones of the Antofagasta de la Sierra basin, Southern Puna plateau, Argentina." Geological Society, London, Special Publications 446, no. 1 (2016): 311–36. http://dx.doi.org/10.1144/sp446.3.

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26

Marrett, Randall, and Steven H. Emerman. "The relations between faulting and mafic magmatism in the Altiplano-Puna plateau (central Andes)." Earth and Planetary Science Letters 112, no. 1-4 (1992): 53–59. http://dx.doi.org/10.1016/0012-821x(92)90006-h.

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27

Haag, Maurício Barcelos, Walter Ariel Baez, Carlos Augusto Sommer, José Marcelo Arnosio, and Rubén Eduardo Filipovich. "Geomorphology and spatial distribution of monogenetic volcanoes in the southern Puna Plateau (NW Argentina)." Geomorphology 342 (October 2019): 196–209. http://dx.doi.org/10.1016/j.geomorph.2019.06.008.

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28

Marrett, R. A., R. W. Allmendinger, R. N. Alonso, and R. E. Drake. "Late Cenozoic tectonic evolution of the Puna Plateau and adjacent foreland, northwestern Argentine Andes." Journal of South American Earth Sciences 7, no. 2 (1994): 179–207. http://dx.doi.org/10.1016/0895-9811(94)90007-8.

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29

Fernandez, Luis, and Julieta Andreoli Bize. "Trichomycterus alterus (Marini, Nichols & La Monte, 1933) and T. corduvensis Weyenberg 1877 (Siluriformes: Trichomycteridae): new records from the High Andean Plateau." Check List 13, no. 2 (2017): 2068. http://dx.doi.org/10.15560/13.2.2068.

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New records of two Trichomycterus species are herein added to the existing checklist of catfishes living at elevations above 3,000 m in the Andes of South America. Trichomycterus alterus and T. corduvensis are recorded at 3,430 m above sea level from the High Andean Plateau (or Puna) in a stream near Antofagasta de la Sierra, Provincia de Catamarca, Argentina. Morphometric and meristic data of examined specimens are included.

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30

Fuchs, María L., Héctor H. Varela, and José A. Cocilovo. "Kinship and Phenotypic Divergence in the Ancient Population of the Puna Plateau of Northwestern Argentina." Advances in Anthropology 06, no. 01 (2016): 1–10. http://dx.doi.org/10.4236/aa.2016.61001.

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31

Simón, Valeria, Marcelo Arnosio, Robert B. Trumbull, et al. "Geology, geochemistry and geochronology of Lindero porphyry gold deposit in the Southern Puna plateau, Argentina." Journal of South American Earth Sciences 105 (January 2021): 103047. http://dx.doi.org/10.1016/j.jsames.2020.103047.

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32

Peralta Arnold, Y., J. Cabassi, F. Tassi, P. J. Caffe, and O. Vaselli. "Fluid geochemistry of a deep-seated geothermal resource in the Puna plateau (Jujuy Province, Argentina)." Journal of Volcanology and Geothermal Research 338 (May 2017): 121–34. http://dx.doi.org/10.1016/j.jvolgeores.2017.03.030.

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33

Guzmán, Silvina, and Ivan Petrinovic. "The Luingo caldera: The south-easternmost collapse caldera in the Altiplano–Puna plateau, NW Argentina." Journal of Volcanology and Geothermal Research 194, no. 4 (2010): 174–88. http://dx.doi.org/10.1016/j.jvolgeores.2010.05.009.

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34

Kay, Suzanne Mahlburg, Beatriz L. Coira, Pablo J. Caffe, and Chang-Hwa Chen. "Regional chemical diversity, crustal and mantle sources and evolution of central Andean Puna plateau ignimbrites." Journal of Volcanology and Geothermal Research 198, no. 1-2 (2010): 81–111. http://dx.doi.org/10.1016/j.jvolgeores.2010.08.013.

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35

Zhou, Renjie, and Lindsay M. Schoenbohm. "Late Miocene upper-crustal deformation within the interior of the southern Puna Plateau, central Andes." Lithosphere 7, no. 3 (2015): 336–52. http://dx.doi.org/10.1130/l396.1.

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36

Hermanns, Reginald L., Samuel Niedermann, Arturo Villanueva Garcia, Jose Sosa Gomez, and Manfred R. Strecker. "Neotectonics and catastrophic failure of mountain fronts in the southern intra-Andean Puna Plateau, Argentina." Geology 29, no. 7 (2001): 619. http://dx.doi.org/10.1130/0091-7613(2001)029<0619:nacfom>2.0.co;2.

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37

Giordano, G., F. Ahumada, L. Aldega, et al. "Preliminary Data on the Structure and Potential of the Tocomar Geothermal Field (Puna Plateau, Argentina)." Energy Procedia 97 (November 2016): 202–9. http://dx.doi.org/10.1016/j.egypro.2016.10.055.

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38

Hooper, James, Samuel K. Marx, Jan-Hendrik May, et al. "Dust deposition tracks late-Holocene shifts in monsoon activity and the increasing role of human disturbance in the Puna-Altiplano, northwest Argentina." Holocene 30, no. 4 (2020): 519–36. http://dx.doi.org/10.1177/0959683619895814.

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The Puna-Altiplano plateau represents a regionally significant dust source, which is critically located at the nexus between the tropical and sub-polar synoptic systems that dominate the South American climate. Dust emissions in this region would therefore be expected to be sensitive to changes in these systems, in particular the strength and position of the South American Summer Monsoon (SASM). Here, we present a late-Holocene multi-proxy study where changes in dust flux, reconstructed from a high-altitude peat mire, are examined in light of climate variability and human impacts. Results show that for most the 4300 cal. yr BP record, dust flux sensitively tracked changes in SASM activity. Prior to 2600 cal. yr BP relatively high dust flux implies dry conditions prevailed across the Puna-Altiplao in association with reduced SASM activity. The chemistry of dust deposited at this time matched the large endorheic basins on the Puna, which host ephemeral lakes and terminal fans, indicating these were actively supplying dust to the airstream. After 2600 cal. yr BP, SASM activity increased while dust flux decreased and the dust chemistry changed, collectively implying the shutting down of the Puna-Altiplano as a significant dust source. Dust flux increased after 1000 cal. yr BP during the ‘Medieval Warm Period’, associated with a return to drier conditions and reactivation of dust sources across the endorheic basins of the Puna. Natural variability in dust flux was dwarfed, however, by the very significant increase in flux after 400 cal. yr BP following Spanish Colonisation and associated changing landuse practices. This finding attests to the globally significant role of humans on dust emissions.

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39

Muñoz-Pedreros, Andrés, Patricio De los Ríos-Escalante, and Patricia Möller. "Zooplankton of the highland bogs of Putana, a desert wetland of the high puna, northern Chile." Crustaceana 88, no. 10-11 (2015): 1235–44. http://dx.doi.org/10.1163/15685403-00003482.

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The Atacama “puna” (high-altitude plateau) is situated among the high peaks of the Andes at over 4000 m a.s.l. This ecosystem covers parts of north-eastern Chile, north-western Argentina, south-eastern Peru, and mid-western Bolivia. The puna brings together several types of wetlands, such as salt-flats, lakes, rivers, high marshes, and highland bogs. Highland bogs are peatlands associated with endorheic basins. The object of this study was to analyse the specific composition and structure of the zooplankton of the bogs of the Putana River, on the Altiplano of northern Chile. In 2012, zooplankton samples were taken for qualitative and quantitative analysis at nine stations of the bog. Nine taxa of zooplanktonic crustaceans were recorded. The species richness is higher than records in other high Andean wetland at a similar altitude, although the species found have been reported for other high Andean wetlands and Andean lakes in Chile and from neighbouring countries.

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40

Heit, B., M. Bianchi, X. Yuan, et al. "Structure of the crust and the lithosphere beneath the southern Puna plateau from teleseismic receiver functions." Earth and Planetary Science Letters 385 (January 2014): 1–11. http://dx.doi.org/10.1016/j.epsl.2013.10.017.

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41

Giordano, Guido, Annamaria Pinton, Paola Cianfarra, et al. "Structural control on geothermal circulation in the Cerro Tuzgle–Tocomar geothermal volcanic area (Puna plateau, Argentina)." Journal of Volcanology and Geothermal Research 249 (January 2013): 77–94. http://dx.doi.org/10.1016/j.jvolgeores.2012.09.009.

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42

Strecker, M. R., R. Alonso, B. Bookhagen, et al. "Does the topographic distribution of the central Andean Puna Plateau result from climatic or geodynamic processes?" Geology 37, no. 7 (2009): 643–46. http://dx.doi.org/10.1130/g25545a.1.

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43

de Urreiztieta, M., D. Gapais, C. Le Corre, P. R. Cobbold, and E. Rossello. "Cenozoic dextral transpression and basin development at the southern edge of the Puna Plateau, northwestern Argentina." Tectonophysics 254, no. 1-2 (1996): 17–39. http://dx.doi.org/10.1016/0040-1951(95)00071-2.

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44

Lucrecia López Steinmetz, R., Stefano Salvi, M. Gabriela García, et al. "Northern Puna Plateau-scale survey of Li brine-type deposits in the Andes of NW Argentina." Journal of Geochemical Exploration 190 (July 2018): 26–38. http://dx.doi.org/10.1016/j.gexplo.2018.02.013.

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45

Martínez, C., C. Jaramillo, A. Correa-Metrío, et al. "Neogene precipitation, vegetation, and elevation history of the Central Andean Plateau." Science Advances 6, no. 35 (2020): eaaz4724. http://dx.doi.org/10.1126/sciadv.aaz4724.

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Andean uplift played a fundamental role in shaping South American climate and species distribution, but the relationship between the rise of the Andes, plant composition, and local climatic evolution is poorly known. We investigated the fossil record (pollen, leaves, and wood) from the Neogene of the Central Andean Plateau and documented the earliest evidence of a puna-like ecosystem in the Pliocene and a montane ecosystem without modern analogs in the Miocene. In contrast to regional climate model simulations, our climate inferences based on fossil data suggest wetter than modern precipitation conditions during the Pliocene, when the area was near modern elevations, and even wetter conditions during the Miocene, when the cordillera was around ~1700 meters above sea level. Our empirical data highlight the importance of the plant fossil record in studying past, present, and future climates and underscore the dynamic nature of high elevation ecosystems.

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46

Tapia, J., J. Murray, M. Ormachea, N. Tirado, and D. K. Nordstrom. "Origin, distribution, and geochemistry of arsenic in the Altiplano-Puna plateau of Argentina, Bolivia, Chile, and Perú." Science of The Total Environment 678 (August 2019): 309–25. http://dx.doi.org/10.1016/j.scitotenv.2019.04.084.

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47

Risse, Andreas, Robert B. Trumbull, Beatriz Coira, Suzanne M. Kay, and Paul van den Bogaard. "40Ar/39Ar geochronology of mafic volcanism in the back-arc region of the southern Puna plateau, Argentina." Journal of South American Earth Sciences 26, no. 1 (2008): 1–15. http://dx.doi.org/10.1016/j.jsames.2008.03.002.

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48

L. Steinmetz, R. L., and C. I. Galli. "Basin development at the eastern border of the Northern Puna and its relationship with the plateau evolution." Journal of South American Earth Sciences 63 (November 2015): 244–59. http://dx.doi.org/10.1016/j.jsames.2015.07.017.

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49

Kraemer, B., D. Adelmann, M. Alten, et al. "Incorporation of the Paleogene foreland into the Neogene Puna plateau: The Salar de Antofalla area, NW Argentina." Journal of South American Earth Sciences 12, no. 2 (1999): 157–82. http://dx.doi.org/10.1016/s0895-9811(99)00012-7.

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50

Coutand, Isabelle, Annick Chauvin, Peter Robert Cobbold, Pierre Gautier, and Pierrick Roperch. "Vertical axis rotations across the Puna plateau (northwestern Argentina) from paleomagnetic analysis of Cretaceous and Cenozoic rocks." Journal of Geophysical Research: Solid Earth 104, B10 (1999): 22965–84. http://dx.doi.org/10.1029/1999jb900148.

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