STEIN - Stochastic erosion in-situ cosmogenic nuclide model

DOI

The stochastic erosion in-situ cosmogenic nuclide model is a 1D numerical model that simulates the evolution of the concentrations of in situ-produced Be-10, C-14, and He-3 alongside the bedrock thermal field in the shallow Earth surface. It is useful for evaluating cosmogenic nuclide data derived from field samples, in order to determine the erosion rate, erosion style, as well as the time-integrated bedrock thermal history. The model simulates erosion in four styles: no erosion, uniform (steady-state) erosion, episodic erosion, and stochastic erosion. It is particularly useful for evaluating the time-temperature evolution of bedrock hillslopes in mountainous regions.

Copyright 2022 Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences

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Identifier
DOI https://doi.org/10.5880/GFZ.3.3.2022.001
Related Identifier https://doi.org/10.1029/2021JF006580
Metadata Access http://doidb.wdc-terra.org/oaip/oai?verb=GetRecord&metadataPrefix=oai_datacite&identifier=oai:doidb.wdc-terra.org:7346
Provenance
Creator Dennis, Donovan P. ORCID logo; Scherler, Dirk ORCID logo
Publisher GFZ Data Services
Contributor Dennis, Donovan P.; Scherler, Dirk
Publication Year 2022
Funding Reference H2020 European Research Council, 759639
Rights BSD 3-clause License; https://opensource.org/licenses/BSD-3-Clause
OpenAccess true
Contact Dennis, Donovan P. (GFZ German Research Centre for Geosciences, Potsdam, Germany)
Representation
Resource Type Software
Discipline Geosciences