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dc.contributor.author
Paterson, Greig A.
dc.contributor.author
Roberts, Andrew P.
dc.contributor.author
Mac Niocaill, Conall
dc.contributor.author
Muxworthy, Adrian R.
dc.contributor.author
Gurioli, Lucia
dc.contributor.author
Viramonte, Jose German

dc.contributor.author
Navarro, Carlos
dc.contributor.author
Weider, Shoshana
dc.date.available
2019-02-22T17:35:05Z
dc.date.issued
2010-04
dc.identifier.citation
Paterson, Greig A.; Roberts, Andrew P.; Mac Niocaill, Conall; Muxworthy, Adrian R.; Gurioli, Lucia; et al.; Paleomagnetic determination of emplacement temperatures of pyroclastic deposits: An under-utilized tool; Springer; Bulletin Of Volcanology; 72; 3; 4-2010; 309-330
dc.identifier.issn
0258-8900
dc.identifier.uri
http://hdl.handle.net/11336/70721
dc.description.abstract
Paleomagnetic data from lithic clasts collected from Mt. St. Helens, USA, Volcán Láscar, Chile, Volcán de Colima, Mexico and Vesuvius, Italy have been used to determine the emplacement temperature of pyroclastic deposits at these localities and to highlight the usefulness of the paleomagnetic method for determining emplacement temperatures. At Mt. St. Helens, the temperature of the deposits (Tdep) at three sites from the June 12, 1980 eruption was found to be ≥532°C, ≥509°C, and 510-570°C, respectively. One site emplaced on July 22, 1980 was emplaced at ≥577°C. These new paleomagnetic temperatures are in good agreement with previously published direct temperature measurements and paleomagnetic estimates. Lithic clasts from pyroclastic deposits from the 1993 eruption of Láscar were fully remagnetized above the respective Curie temperatures, which yielded a minimum Tdep of 397°C. Samples were also collected from deposits thought to be pyroclastics from the 1913, 2004 and 2005 eruptions of Colima. At Colima, the sampled clasts were emplaced cold. This is consistent with the sampled clasts being from lahar deposits, which are common in the area, and illustrates the usefulness of the paleomagnetic method for distinguishing different types of deposit. Tdep of the lower section of the lithic rich pyroclastic flow (LRPF) from the 472 A. D. deposits of Vesuvius was ~280-340°C. This is in agreement with other, recently published paleomagnetic measurements. In contrast, the upper section of the LRPF was emplaced at higher temperatures, with Tdep ~520°C. This temperature difference is inferred to be the result of different sources of lithic clasts between the upper and lower sections, with the upper section containing a greater proportion of vent-derived material that was initially hot. Our studies of four historical pyroclastic deposits demonstrates the usefulness of paleomagnetism for emplacement temperature estimation.
dc.format
application/pdf
dc.language.iso
eng
dc.publisher
Springer

dc.rights
info:eu-repo/semantics/restrictedAccess
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.subject
EMPLACEMENT TEMPERATURE
dc.subject
MT. ST. HELENS
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PALEOMAGNETISM
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PYROCLASTIC DEPOSITS
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VESUVIUS
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VOLCÁN DE COLIMA
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VOLCÁN LÁSCAR
dc.subject.classification
Meteorología y Ciencias Atmosféricas

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Ciencias de la Tierra y relacionadas con el Medio Ambiente

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CIENCIAS NATURALES Y EXACTAS

dc.title
Paleomagnetic determination of emplacement temperatures of pyroclastic deposits: An under-utilized tool
dc.type
info:eu-repo/semantics/article
dc.type
info:ar-repo/semantics/artículo
dc.type
info:eu-repo/semantics/publishedVersion
dc.date.updated
2019-01-23T18:56:19Z
dc.journal.volume
72
dc.journal.number
3
dc.journal.pagination
309-330
dc.journal.pais
Alemania

dc.journal.ciudad
Berlin
dc.description.fil
Fil: Paterson, Greig A.. University of Southampton; Reino Unido
dc.description.fil
Fil: Roberts, Andrew P.. University of Southampton; Reino Unido
dc.description.fil
Fil: Mac Niocaill, Conall. University of Oxford; Reino Unido
dc.description.fil
Fil: Muxworthy, Adrian R.. Imperial College London; Reino Unido
dc.description.fil
Fil: Gurioli, Lucia. University of Hawaii; Estados Unidos
dc.description.fil
Fil: Viramonte, Jose German. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Salta. Instituto de Investigaciones en Energía no Convencional. Universidad Nacional de Salta. Facultad de Ciencias Exactas. Departamento de Física. Instituto de Investigaciones en Energía no Convencional; Argentina
dc.description.fil
Fil: Navarro, Carlos. Universidad de Colima; México
dc.description.fil
Fil: Weider, Shoshana. University of Oxford; Reino Unido
dc.journal.title
Bulletin Of Volcanology

dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1007/s00445-009-0324-4
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://link.springer.com/article/10.1007/s00445-009-0324-4
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