Arid
DOI10.1016/j.jsames.2020.102905
Naturally elevated arsenic in the Altiplano-Puna, Chile and the link to recent (Mio-Pliocene to Quaternary) volcanic activity, high crustal thicknesses, and geological structures
Tapia, J.; Schneider, B.; Inostroza, M.; Alvarez-Amado, F.; Luque, J. A.; Aguilera, F.; Parra, S.; Bravo, M.
通讯作者Tapia, J (corresponding author), Univ Catolica Norte, Dept Ciencias Geol, Fac Ingn & Ciencias Geol, Antofagasta, Chile.
来源期刊JOURNAL OF SOUTH AMERICAN EARTH SCIENCES
ISSN0895-9811
EISSN1873-0647
出版年2021
卷号105
英文摘要The compilation of water, sediment, rock, and condensed gas data of arsenic (As) in the Altiplano-Puna of Chile reveals a link between its natural enrichment and volcanic activity, high crustal thicknesses, and regional structures. Two zones were studied which encompass the Altiplano-Puna and western lowlands of Chile: the Northern Zone (including Los Pintados, Surire, and Huasco) and Southern Zone (including Pedernales, Grande, and Laguna Verde). A positive correlation was found between average As concentrations in saline and brackish water of salt flats and crustal thicknesses of the two studied zones with heightened values to the east (up to 25 mg.L-1 of dissolved As in water and a 64 km depth to the Mohorovicic discontinuity). Furthermore, in the studied Altiplano-Puna salt flats, surrounding Mio-Pliocene to Quaternary felsic and intermediate volcanic outcrops are abundant and As is well correlated with other dissolved components (e.g. Li and B). Sediments show extreme As values at punctual locations within the Altiplano-Puna, where the crust is thick, recent volcanic and hydrothermal activity is present, and regional faults are found. Volcanic rocks and condensed gas in the Altiplano-Puna are also enriched with As (up to 221 and 1234 mg.kg(-1) respectively). In this tectonic environment, it is hypothesized that volcanism represents an important source of As and the thick continental crust can provide a large reservoir of As that can be leached by rising thermal fluids. Regional scale fault systems also can allow for preferential upwelling and the heightened concentration of As in fractures. Hydrological processes at the surface transport dissolved As to lower elevation regions through groundwater in aquifers and surface water in perennial rivers, creeks, and gorges, diluting element concentrations where significant evapoconcentration is not present.
英文关键词Arsenic Altiplano-Puna plateau Volcanic activity Hydrothermal fluids Amuyo ponds Salt flats
类型Article
语种英语
收录类别SCI-E
WOS记录号WOS:000606797900002
WOS关键词ATACAMA DESERT ; TRACE-ELEMENTS ; NORTHERN CHILE ; CENTRAL ANDES ; HYDROTHERMAL SYSTEMS ; TIBETAN PLATEAU ; DRINKING-WATER ; LATIN-AMERICA ; GROUNDWATER ; EVOLUTION
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/348044
作者单位[Tapia, J.; Luque, J. A.; Aguilera, F.] Univ Catolica Norte, Dept Ciencias Geol, Fac Ingn & Ciencias Geol, Antofagasta, Chile; [Schneider, B.] Montgomery & Associates, Santiago, Chile; [Inostroza, M.] Univ Catolica Norte, Programa Doctorado Ciencias Menc Geol, Antofagasta, Chile; [Inostroza, M.; Aguilera, F.] Univ Catolica Norte, Nucleo Invest Riesgo Volcan Ckelar Volcanes, Antofagasta, Chile; [Alvarez-Amado, F.] Univ Concepcion, Dept Ciencias Tierra, Concepcion, Chile; [Parra, S.; Bravo, M.] Pontificia Univ Catolica Valparaiso, Inst Quim, Valparaiso, Chile
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Tapia, J.,Schneider, B.,Inostroza, M.,et al. Naturally elevated arsenic in the Altiplano-Puna, Chile and the link to recent (Mio-Pliocene to Quaternary) volcanic activity, high crustal thicknesses, and geological structures[J],2021,105.
APA Tapia, J..,Schneider, B..,Inostroza, M..,Alvarez-Amado, F..,Luque, J. A..,...&Bravo, M..(2021).Naturally elevated arsenic in the Altiplano-Puna, Chile and the link to recent (Mio-Pliocene to Quaternary) volcanic activity, high crustal thicknesses, and geological structures.JOURNAL OF SOUTH AMERICAN EARTH SCIENCES,105.
MLA Tapia, J.,et al."Naturally elevated arsenic in the Altiplano-Puna, Chile and the link to recent (Mio-Pliocene to Quaternary) volcanic activity, high crustal thicknesses, and geological structures".JOURNAL OF SOUTH AMERICAN EARTH SCIENCES 105(2021).
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