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dc.contributor.authorSchmitt, Axel Kstockli, Daniel Fhausback, Brian P.
dc.datenov-15
dc.date2006
dc.date.accessioned2018-07-12T17:00:33Z
dc.date.available2018-07-12T17:00:33Z
dc.identifier.isbn0377-0273
dc.identifier.urihttps://colecciondigital.cemiegeo.org/xmlui/handle/123456789/3206
dc.description.abstractLas Tres Virgenes volcano is a calc-alkaline composite cone located near the main Gulf of California escarpment on the E coast of the Baja California peninsula. High-sensitivity ion microprobe U-series (Th-230/U-238) ages for zircon from La Virgen tephra average 121(-10)(+12) ka (1 sigma; MSWD= 2.7), with discrete age peaks at similar to 100 and 160 ka. The noble gas mass spectrometric (U-Th)/He zircon age, corrected for disequilibrium and pre-eruptive storage, is 36 +/- 3 ka. This result for the eruption age of La Virgen tephra is significantly older than previously postulated historic or Holocene ages that were based on an 18th century map reference and C-14 dating of accidental charcoal, respectively. The new (U-Th)/He zircon age is consistent with a > 26 +/- 4 ka age derived from cosmogenic He exposure dating of an overlying basaltic lava flow [Hausback, B.P. and Abrams, M.J., 1996. Plinian eruption of La Virgen Tephra, Volcan Las Tres Virgenes, Baja California Sur, Mexico. Eos, Transactions, American Geophysical Union, 77(46, Suppl.): 813-814.]. U-Pb zircon analysis of ignimbrites erupted from the adjacent Early Pleistocene La Reforma and El Aguajito calderas yielded ages of 1.38 +/- 0.03 Ma (n= 12; MSWD= 1.0) and 1.17 +/- 0.07 Ma (n=23; MSWD= 1.3), respectively. No evidence for these ages is found among La Virgen zircons, whereas pre-Quaternary zircon xenocrysts are common. The La Virgen magma, therefore, evolved unrelated to Early Pleistocene magmatisin in adjacent calderas, but assimilated local basement rocks. A gap between average Th-U and (U-Th)/He zircon ages suggests that zircon crystallization was discontinuous in the La Virgen magma chamber. In addition, partial resorption of zircon suggests episodic thermal rejuvenation, most likely by basaltic recharge. Based on the zircon record, the > 100 ka lifetime of the thermal anomaly that sustained repeated intrusive pulses significantly exceeds the age of the last eruption. This strengthens the view that Tres Virgenes has a potential for future eruptions. (c) 2006 Elsevier B.V. All rights reserved.
dc.languageEnglish
dc.rightsReaders who download papers from this site should honor the copyright of the original authors and may not copy or distribute the work further without the permission of the original publisher.
dc.sourceWOS
dc.subjectGulf of California; volcanism; He-4; U-238/Th-230; zircon; magma chambers]_curad
dc.subjectVOLCANIC-ROCKS; RESIDENCE TIMES; MEXICO; SUR; CALDERA; APATITE; SYSTEM; FIELD; GULF]_curad
dc.subjectGeosciences, Multidisciplinary]_curad
dc.subjectGeology]_curad
dc.titleEruption and magma crystallization ages of Las Tres Virgenes (Baja California) constrained by combined Th-230/U-238 and (U-Th)/He dating of zircon
dc.typeArtículoES
dc.relation.issue03-abr
dc.relation.journalJournal of Volcanology and Geothermal Research
dc.relation.volume158
dc.identifier.doihttps://doi.org/10.1016/j.jvolgeores.2006.07.005
dc.relation.startingPage281
dc.description.campoLas Tres Virgenes


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