Journal of Geophysical Research Atmospheres· 2012
Transdimensional inverse thermal history modeling for quantitative thermochronology
- 751citations
- 2012year
Short summary
A novel Bayesian transdimensional Markov Chain Monte Carlo method quantifies thermal history models by producing an ensemble of accepted histories with associated probability distributions, reducing over-interpretation of results.
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Key points
- Introduces a Bayesian transdimensional Markov Chain Monte Carlo method for inverse thermal history modeling.
- Allows flexible prior specification for time and temperature, including geological constraints.
- Naturally favors simpler models that fit data, reducing over-interpretation.
- Outputs an ensemble of thermal histories as a posterior probability distribution.
- Can combine multiple thermochronological data types (e.g., fission track, U-Th/He).
AI-generated from the title and abstract; the full text is not read.
Abstract
A new approach for inverse thermal history modeling is presented. The method uses Bayesian transdimensional Markov Chain Monte Carlo and allows us to specify a wide range of possible thermal history models to be considered as general prior information on time, temperature (and temperature offset for multiple samples in a vertical profile). We can also incorporate more focused geological constraints in terms of more specific priors. The Bayesian approach naturally prefers simpler thermal history models (which provide an adequate fit to the observations), and so reduces the problems associated with over interpretation of inferred thermal histories. The output of the method is a collection or ensemble of thermal histories, which quantifies the range of accepted models in terms a (posterior) probability distribution. Individual models, such as the best data fitting (maximum likelihood) model or the expected model (effectively the weighted mean from the posterior distribution) can be examined. Different data types (e.g., fission track, U‐Th/He, 40 Ar/ 39 Ar) can be combined, requiring just a data‐specific predictive forward model and data fit (likelihood) function. To demonstrate the main features and implementation of the approach, examples are presented using both synthetic and real data.
The authors' abstract, as published at the source. Journal of Geophysical Research Atmospheres, 2012 · DOI ↗
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Field: Mechanics of Materials
Mechanics of MaterialsEngineering