Lithium and Brine Geochemistry in the Salars of the Southern Puna, Andean Plateau of Argentina

被引:17
|
作者
Lopez Steinmetz, Romina Lucrecia [1 ]
Salvi, Stefano [2 ]
Sarchi, Carisa [1 ]
Santamans, Carla [1 ]
Lopez Steinmetz, Lorena Cecilia [3 ]
机构
[1] Univ Nacl Jujuy, CONICET, Inst Geol & Min, Inst Ecorreg Andinas CONICET INECOA, Av Bolivia 1661, RA-4600 San Salvador De Jujuy, Argentina
[2] Univ Toulouse, Geosci Environm Toulouse GET, Inst Rech Dev IRD, Observ Midi Pyrenees OMP,CNRS, 14 Av Edouard Beliu, F-31400 Toulouse, France
[3] Univ Nacl Cordoba, Inst Invest Psicol, IIPsi, UNC,CONICET, Blvd Reforma & Enfermera Gordillo S-N,2do Piso, RA-5000 Cordoba, Argentina
关键词
NORTHERN PUNA; MAGMA GENESIS; ORDOVICIAN; EVOLUTION; DEPOSITS; LI; ALTIPLANO;
D O I
10.5382/econgeo.4754
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
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 degrees S-26 degrees 30'S). Hydrochemical data indicate that the shallowest brines are characterized by highly vari- able 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 RincOn 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.
引用
收藏
页码:1079 / 1096
页数:18
相关论文
共 50 条
  • [31] Recent, slow normal and strike-slip faulting in the Pasto Ventura region of the southern Puna Plateau, NW Argentina
    Zhou, Renjie
    Schoenbohm, Lindsay M.
    Cosca, Michael
    TECTONICS, 2013, 32 (01) : 19 - 33
  • [32] Velocity structure beneath the southern Puna plateau: Evidence for delamination
    Calixto, Frank J.
    Sandvol, Eric
    Kay, Suzanne
    Mulcahy, Patrick
    Heit, Benjamin
    Yuan, Xiaohui
    Coira, Beatriz
    Comte, Diana
    Alvarado, Patricia
    GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS, 2013, 14 (10) : 4292 - 4305
  • [33] Oligocene to present shallow subduction beneath the southern Puna plateau
    Gianni, Guido M.
    Garcia, Hector P. A.
    Pesce, Agustina
    Lupari, Marianela
    Gonzalez, Marcelo
    Giambiagi, Laura
    TECTONOPHYSICS, 2020, 780
  • [34] Growth and fragmentation of the Andean foreland basin during eastward advance of fold-thrust deformation, Puna plateau and Eastern Cordillera, northern Argentina
    Department of Geological Sciences, University of Texas at Austin, 1 University Station C9000, Austin, TX 78712, United States
    Tectonics, 6
  • [35] Cenozoic Exhumation and Deformation of the Intermontane Pastos Chicos Basin in the Southern Central Andes: Implications for the Tectonic Evolution of the Andean Plateau (Puna) and the Eastern Cordillera Between 23° and 24°S, NW Argentina
    Pingel, Heiko
    Deeken, Anke
    Coutand, Isabelle
    Alonso, Ricardo N.
    Riller, Ulrich
    Sobel, Edward R.
    Cottle, John M.
    Strecker, Manfred R.
    TECTONICS, 2023, 42 (02)
  • [36] Growth and fragmentation of the Andean foreland basin during eastward advance of fold-thrust deformation, Puna plateau and Eastern Cordillera, northern Argentina
    Siks, Benjamin C.
    Horton, Brian K.
    TECTONICS, 2011, 30
  • [37] THE MULTITEMPORALITY OF LANDSCAPES: A CASE OF THE ANDEAN AREA (CUSI CUSI, PUNA DE JUJUY, ARGENTINA)
    Vaquer, Jose Maria
    Pey, Laura
    Gerola, Ignacio
    RELACIONES, 2023, 48 : 20 - 38
  • [38] VALLEYS OR PUNA? DISCUSSING INTERACTION OF THE COMPOSITIONAL CHARACTERIZATION OF POTTERY. THE CASE OF ANTOFAGASTA, SOUTHERN PUNA, ARGENTINA
    Lopez Campeny, Sara M. L.
    ESTUDIOS ATACAMENOS, 2012, (43): : 139 - 166
  • [39] Eruptive style and flow dynamics of the pyroclastic density currents related to the Holocene Cerro Blanco eruption (Southern Puna plateau, Argentina)
    Baez, W.
    Bustos, E.
    Chiodi, A.
    Reckziegel, F.
    Arnosio, M.
    de Silva, S.
    Giordano, G.
    Viramonte, J. G.
    Sampietro-Vattuone, M. M.
    Pena-Monne, J. L.
    JOURNAL OF SOUTH AMERICAN EARTH SCIENCES, 2020, 98
  • [40] Preliminary data on the structure and potential of the Tocomar geothermal field (Puna plateau, Argentina)
    Giordano, G.
    Ahumada, F.
    Aldega, L.
    Baez, W.
    Becchio, R.
    Bigi, S.
    Caricchi, C.
    Chiodi, A.
    Corrado, S.
    De Benedetti, A. A.
    Favetto, A.
    Filipovich, R.
    Fusari, A.
    Groppelli, G.
    Invernizzi, C.
    Maffucci, R.
    Norini, G.
    Pinton, A.
    Pomposiello, C.
    Tassi, F.
    Taviani, S.
    Viramonte, J.
    EUROPEAN GEOSCIENCES UNION GENERAL ASSEMBLY 2016, 2016, 97 : 202 - 209