Forward and Inverse Modeling of Low-Temperature Thermochronometry Data

Research Article| January 01, 2005 Forward and Inverse Modeling of Low-Temperature Thermochronometry Data Richard A. Ketcham Richard A. Ketcham Jackson School of Geosciences, The University of Texas at Austin, Austin, Texas, 78712, U.S.A., ketcham@mail.utexas.edu Search for other works by this author on: GSW Google Scholar Reviews in Mineralogy and Geochemistry (2005) 58 (1): 275–314. https://doi.org/10.2138/rmg.2005.58.11 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 Richard A. Ketcham; Forward and Inverse Modeling of Low-Temperature Thermochronometry Data. Reviews in Mineralogy and Geochemistry 2005;; 58 (1): 275–314. doi: https://doi.org/10.2138/rmg.2005.58.11 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 The thermochronometric systems discussed in this volume broadly share three features: parent isotopes, daughter products, and one or more time-dependent, temperature-sensitive processes by which daughter products are altered or lost. If these processes can be measured in the laboratory, and their behavior confidently extrapolated to geological time scales, it becomes possible to construct a forward model of the system that predicts how a given instance of it will evolve assuming a particular starting arrangement and subsequent time-temperature history. Once a forward model has been created and verified, it then becomes possible to apply it in the inverse sense: given a... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.