Research Article| January 01, 2005 Forward Modeling and Interpretation of (U-Th)/He Ages Tibor J. Dunai Tibor J. Dunai Faculty of Earth and Life Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV, Amsterdam, The Netherlands, dunt@geo.vu.nl Search for other works by this author on: GSW Google Scholar Author and Article Information Tibor J. Dunai Faculty of Earth and Life Sciences, Vrije Universiteit, De Boelelaan 1085, 1081 HV, Amsterdam, The Netherlands, dunt@geo.vu.nl Publisher: Mineralogical Society of America First Online: 03 Mar 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2005) 58 (1): 259–274. https://doi.org/10.2138/rmg.2005.58.10 Article history First Online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Tibor J. Dunai; Forward Modeling and Interpretation of (U-Th)/He Ages. Reviews in Mineralogy and Geochemistry 2005;; 58 (1): 259–274. doi: https://doi.org/10.2138/rmg.2005.58.10 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 Soon after the initial studies on He-diffusion in apatite pointed out the use of the (U-Th)/ He system for low temperature geochronology (Zeitler et al. 1987; Wolf et al. 1996; Warnock et al. 1997), the potential value of forward modeling for refined interpretation of (U-Th)/He dating was indicated (Wolf et al. 1998). While the first studies provided evidence for the low closure temperature (TC, Dodson 1973) of the (U-Th)/He system in apatite for monotonously cooling systems, the latter study investigated the sensitivity of the (U-Th)/He system for a wide range... 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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