Evolution of the Azufre volcano (northern Chile): Implications for the Cerro Pabellón Geothermal Field as inferred from long lasting eruptive activity

Godoy, Benigno; Taussi, Marco; González-Maurel, Osvaldo; Hübner, Darío; Lister, James; Sellés, Daniel; Roux, Petrus le; Renzulli, Alberto; Rivera, Germain; Morata, Diego

doi:10.1016/j.jvolgeores.2022.107472

Cited by 5 publications

(2 citation statements)

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“…Hydrogeochemical processes operating within the catchment may be summarized using TDS vs. location within the catchment, FIGURE 8 (A) distribution of low pmC, HCO 3 :Cl, and temperature representing groups I-III. Also shown are the extent of the San Pedro-Linzor low resistivity zone (Mancini et al, 2019), and the El Tatio hydrothermal field (Giggenbach, 1978) and low resistivity zone (Letelier et al, 2021), the Cerro Pabellon geothermal field (Godoy et al, 2022), and the Sol de Manana hydrothermal field (Morata et al, 2020). (B) three component mixing diagram for groups I-III.…”

Section: Baseflow Characteristics and Interaction With Aquifersmentioning

confidence: 99%

“…These lowresistivity zones occur at depths of <60 m and 200-400 m hinting at possible reservoirs for groups II and III waters. Several hydrothermal, and fumarolic vents associated with argillic alteration are located within and adjacent to the watershed of the Salado (Figure 8) (Scandiffio and Alvarez, 1992;Mancini et al, 2019;Morata et al, 2020;Taussi et al, 2021;Godoy et al, 2022) offering potential pathways for magmatic water to ascend, and mix with surface and groundwater.…”

Section: Potential Sources Of Invariant Rechargementioning

confidence: 99%

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The provenance and persistence of the perennial Río Loa in the Atacama Desert: links between crustal processes and surface hydrology

Houston

2023

Front. Earth Sci.

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The Río Loa is a perennial river that crosses the Atacama Desert. A basin-wide survey enables for the first time, the hydrologic regime origin, persistence and processes to be identified. Perennial baseflow in the Ríos Loa and Salado largely originates from intra-arc aquifers which are poorly known. However, the data indicate that despite flood flow being largely confined to the summer (DJF) season, sufficient storage exists in these aquifers to maintain year-round stream flow from high-altitude, across the Atacama Desert to the coast. The intra-arc aquifers of the Western Cordillera receive recharge from time-variable precipitation infiltration and time-invariant lithospheric inputs. Lithospheric inputs potentially include slab/mantle dehydration, upper crustal melt devolatilization and/or thermally induced upflow of deeply penetrating meteoric water through buried evaporites or carbonates. Downstream, aquifers in the Pre-Andean basins variably interact with surface water, depending on location, river stage and time of year, but they do not supply significant additional sources of baseflow. Hydrochemical processes include those related to volcanic activity, soil carbonate generation, silicate weathering, CO2 degassing and calcite precipitation. Solutes undergo concentration by evaporation, gypsum dissolution, and are further affected by localized NO3, and SO4 inputs and mixing with saline waters. Stable isotopes reveal subcatchment specific precipitation and evaporation, whilst carbon and tritium isotopes are used to analyze recharge sources and processes in the intra-arc aquifers and downstream mixing.

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