Metadata-Version: 2.4
Name: peridoxia
Version: 2.1
Summary: Package for assessing redox during mantle melting
Author-email: "Suzanne K. Birner" <birners@berea.edu>
License-Expression: MIT
Project-URL: Homepage, https://gitlab.com/skbirner/peridoxia
Classifier: Programming Language :: Python :: 3
Classifier: Operating System :: OS Independent
Requires-Python: <3.11,>=3.10
Description-Content-Type: text/markdown
License-File: LICENSE
Requires-Dist: deprecation>=2.1.0
Requires-Dist: matplotlib>=3.6.2
Requires-Dist: nptyping
Requires-Dist: numdifftools
Requires-Dist: openpyxl
Requires-Dist: pandas>=1.5.2
Requires-Dist: pytest>=7.2.0
Requires-Dist: pytest-cov>=4.0.0
Requires-Dist: scipy>=1.9.3
Requires-Dist: seaborn>=0.12.1
Requires-Dist: thermoengine>=2.0.0.dev10
Dynamic: license-file

# 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.
