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Timescales of Magma Chamber Processes and Dating of Young Volcanic Rocks
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Magmatic ProcessVolcanologyEngineeringVolcanismPetrologyEarth ScienceGeochronologyMagma Chamber ProcessesVolcanic ProcessMagmatismIgneous PetrogenesisGeologyTectonicsYoung Volcanic RocksEconomic GeologyEarth SciencesGeochemistryFrance SearchIgneous Process
Research Article| January 01, 2003 Timescales of Magma Chamber Processes and Dating of Young Volcanic Rocks Michel Condomines; Michel Condomines Laboratoire Dynamique de la Lithosphère (LDL, UMR CNRS 5573) et ISTEEM, Université Montpellier 2, place Eugène Bataillon, 34095 Montpellier cedex 5, France Search for other works by this author on: GSW Google Scholar Pierre-Jean Gauthier; Pierre-Jean Gauthier Laboratoire Magmas et Volcans (LMV, UMR CNRS 6524), 5 rue Kessler, 63038 Clermont-Ferrand Cedex, France Search for other works by this author on: GSW Google Scholar Olgeir Sigmarsson Olgeir Sigmarsson Laboratoire Magmas et Volcans (LMV, UMR CNRS 6524), 5 rue Kessler, 63038 Clermont-Ferrand Cedex, France Search for other works by this author on: GSW Google Scholar Reviews in Mineralogy and Geochemistry (2003) 52 (1): 125–174. https://doi.org/10.2113/0520125 Article history first online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Michel Condomines, Pierre-Jean Gauthier, Olgeir Sigmarsson; Timescales of Magma Chamber Processes and Dating of Young Volcanic Rocks. Reviews in Mineralogy and Geochemistry 2003;; 52 (1): 125–174. doi: https://doi.org/10.2113/0520125 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyReviews in Mineralogy and Geochemistry Search Advanced Search One of the initial goals of measuring U-series disequilibria in young volcanic rocks was the development of new dating methods in an age range (about 0–300 ka), where few other methods were applicable at that time (Cerrai et al. 1965; Cherdyntsev et al. 1967; Kigoshi 1967; Taddeucci et al. 1967; Allègre 1968). In the following years, several studies showed that the 238U-230Th method, the first to be applied, was indeed able to give reliable ages on rocks from various volcanoes (e.g., Allègre and Condomines 1976; Condomines et al. 1978).... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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