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Published December 15, 2015 | public
Journal Article

A reporting protocol for thermochronologic modeling illustrated with data from the Grand Canyon

Abstract

Apatite (U–Th)/He and fission-track dates, as well as ^4He/^3He and fission-track length data, provide rich thermal history information. However, numerous choices and assumptions are required on the long road from raw data and observations to potentially complex geologic interpretations. This paper outlines a conceptual framework for this path, with the aim of promoting a broader understanding of how thermochronologic conclusions are derived. The tiered structure consists of thermal history model inputs at Level 1, thermal history model outputs at Level 2, and geologic interpretations at Level 3. Because inverse thermal history modeling is at the heart of converting thermochronologic data to interpretation, for others to evaluate and reproduce conclusions derived from thermochronologic results it is necessary to publish all data required for modeling, report all model inputs, and clearly and completely depict model outputs. Here we suggest a generalized template for a model input table with which to arrange, report and explain the choice of inputs to thermal history models. Model inputs include the thermochronologic data, additional geologic information, and system- and model-specific parameters. As an example we show how the origin of discrepant thermochronologic interpretations in the Grand Canyon can be better understood by using this disciplined approach.

Additional Information

© 2015 Elsevier B.V. Received in revised form 29 September 2015; Accepted 30 September 2015; Available online 21 October 2015. Supported by NSF EAR-1144500 and EAR-1126991. We thank Todd Ehlers and Lon Abbott for insightful comments on the manuscript.

Additional details

Created:
August 22, 2023
Modified:
October 25, 2023