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• W2109359181 abstract "Research Article| August 01, 2007 Measuring Timescales of Magmatic Evolution Simon Turner; Simon Turner 1GEMOC, Department of Earth and Planetary Sciences, Macquarie University, Sydney NSW 2109, Australia E-mail: sturner@els.mq.edu.au Search for other works by this author on: GSW Google Scholar Fidel Costa Fidel Costa 2CSIC, Institut de Ciències de la Terra `Jaume Almera', c/Lluís Solé i Sabarís s/n, 08028 Barcelona, Spain E-mail: fcosta@ija.csic.es Search for other works by this author on: GSW Google Scholar Author and Article Information Simon Turner 1GEMOC, Department of Earth and Planetary Sciences, Macquarie University, Sydney NSW 2109, Australia E-mail: sturner@els.mq.edu.au Fidel Costa 2CSIC, Institut de Ciències de la Terra `Jaume Almera', c/Lluís Solé i Sabarís s/n, 08028 Barcelona, Spain E-mail: fcosta@ija.csic.es Publisher: Mineralogical Society of America First Online: 09 Mar 2017 Online ISSN: 1811-5217 Print ISSN: 1811-5209 © 2007 by the Mineralogical Society of America Elements (2007) 3 (4): 267–272. https://doi.org/10.2113/gselements.3.4.267 Article history First Online: 09 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 Simon Turner, Fidel Costa; Measuring Timescales of Magmatic Evolution. Elements 2007;; 3 (4): 267–272. doi: https://doi.org/10.2113/gselements.3.4.267 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 SocietyElements Search Advanced Search Abstract Advances in analytical methods have provided new insights into the timescales of magmatic processes. Data on the abundances of U-series isotopes in bulk rocks and crystal separates indicate magma differentiation over thousands of years. Residence and differentiation times of silicic magmas based on single-crystal, in situ age data vary from 10,000 to 100,000 years, with abundant evidence for crystal recycling from previous intrusive episodes. Chemical zoning patterns in single crystals indicate that processes such as mixing and mingling of magmas and crustal assimilation may occur over much shorter timescales of months to decades. Quantifying the rates of magma generation, emplacement and differentiation constrains the processes involved and may contribute to the evaluation of volcanic hazards. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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