Forward and Inverse Modeling of Low-Temperature Thermochronometry Data
By Richard A. Ketcham. 2005
1,288 citations recorded by the source corpus.
Subfields: Artificial Intelligence, Mechanics of Materials, Statistical and Nonlinear Physics
View Paper: https://www.semanticscholar.org/paper/5545c31794f94df31778192fbba2f409070f84e0
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In Artificial Intelligence
In Mechanics of Materials
In Statistical and Nonlinear Physics
Citations in the corpus
- Improved measurement of fission-track annealing in apatite using c-axis projection (2007, background): “Ketcham (2005b) demonstrated that c-axis projection improves reproducibility for one user among replicate experiments, and that it increases compatibility among results obtained with and without enhancement of track revelation using Cf-irradiation.”
- Transdimensional inverse thermal history modeling for quantitative thermochronology (2012, background): “…a continuous function (i.e., thermal history) is represented by a finite number of parameters, such as coefficients of Legendre polynomials [Corrigan, 1991], or more commonly discrete time temperature points [Lutz and Omar, 1991; Gallagher, 1995;Willett, 1997; Ketcham, 2005; Harrison et al., 2005].”
- Apatite (U-Th)/He thermochronometry using a radiation damage accumulation and annealing model (2009, methodology): “Refer to Ketcham (2005) for further details regarding inverse modeling and statistically significant data fits in HeFTy.”
- Past, Present, and Future of Thermochronology (2005, methodology): “For example, forward and inverse models of thermochronologic data became available and widely used (e.g., Laslett et al. 1987; Gallagher 1995; Ketcham 1999, 2005; Willett 1997).”
- Crustal Thermal Processes and the Interpretation of Thermochronometer Data (2005, methodology): “Many thermochronology studies focus on extracting the thermal history of a sample using fi ssion-track length distributions and track annealing models (e.g., Ketcham 2005, and references therein).”
- Helium diffusion in natural zircon: Radiation damage, anisotropy, and the interpretation of zircon (U-Th)/He thermochronology (2013, methodology): “For each zoned zircon, we model the uncorrected date, the FTZ corrected date using the “redistribution” option in HeFTy, and the FTH corrected date.”