peridoxia 2.1

Package for assessing redox during mantle melting

Peridoxia

Peridoxia is an empirical partitioning model designed to assess redox evolution during mantle melting in the shallow garnet and spinel fields. It uses natural and experimental results to constrain ferric iron partitioning between mantle phases. It was first developed by Suzanne Birner (birners AT berea.edu) in 2024 for the manuscript "Deep, hot, ancient melting recorded by ultralow oxygen fugacity in peridotites" (https://www.nature.com/articles/s41586-024-07603-w)

Documentation and Examples may be foud here: https://peridoxia.readthedocs.io/en/latest/

This package requires a virtual environment with python 3.10. For help with installation in a virtual environment, please see the Installation Guide: https://peridoxia.readthedocs.io/en/latest/installation.html.