2006
DOI: 10.1007/s10967-006-0447-4
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Geochemical characterization of volcanic ashes from recent events in Northern Patagonia Andean Range by INAA

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Cited by 16 publications
(25 citation statements)
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“…Tephras were sieved (>500 µm, 500–250 µm, 250–125 µm, 125–63 µm, <63 µm fractions), and the juvenile volcanic components were identified and separated from the silty matrix according to Daga et al . (2006). White and brownish pumice shards, scoria fragments and glass shards were morphologically characterised under a binocular magnifying glass and scanning electron microscope, operating at 10 kV.…”
Section: Methodsmentioning
confidence: 99%
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“…Tephras were sieved (>500 µm, 500–250 µm, 250–125 µm, 125–63 µm, <63 µm fractions), and the juvenile volcanic components were identified and separated from the silty matrix according to Daga et al . (2006). White and brownish pumice shards, scoria fragments and glass shards were morphologically characterised under a binocular magnifying glass and scanning electron microscope, operating at 10 kV.…”
Section: Methodsmentioning
confidence: 99%
“…The high frequency of volcanic events in this area merits an accurate characterisation of the volcanic products as well as the evaluation of their spatial distribution. Few comprehensive geochemical and morphological characterisations of recent volcanic ash produced by the sources in southern Chile have been undertaken (Daga et al ., 2006, 2008; Bertrand et al ., 2008), with the result that accurate tephrochronological correlations and evaluations of their spatial distribution have not been possible.…”
Section: Introductionmentioning
confidence: 99%
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“…3, 4). Previous studies performed on sedimentary sequences from water bodies from Nahuel Huapi National Park demonstrated that the region was impacted by frequent volcanic eruptions from the Calbuco volcano and Puyehue-Cordón Caulle volcanic system with the Calbuco volcano eruptions being the most important affecting the south of the park (Daga et al, 2006(Daga et al, , 2008a. However, it is not possible to assign dates to the eruptions without a better geochemical characterisation of the tephras providing a basis for correlation with potential source eruptions (Daga et al, 2008a).…”
Section: Discussionmentioning
confidence: 99%
“…Tephra layers were not incorporated into the model but were used as additional data to verify the robustness of the age model. Previous tephrocronological studies in the area helped to identify volcanic eruptions responsible for ash deposition in both lakes during the last 200 years (Daga et al 2006Bertrand et al 2008Bertrand et al , 2014Ribeiro Guevara et al 2010;Fontijn et al 2014;Serra et al 2016, Williams et al 2016). …”
Section: Chronologiesmentioning
confidence: 99%