Mössbauer Study of Serpentine Minerals in the Ultramafic Body of Tehuitzingo, Southern Mexico

@article{GonzlezMancera2003MssbauerSO,
  title={M{\"o}ssbauer Study of Serpentine Minerals in the Ultramafic Body of Tehuitzingo, Southern Mexico},
  author={Guillermina Gonz{\'a}lez-Mancera and Fernando Ortega-Guti{\'e}rrez and Noel Nava and Humberto Arriola},
  journal={Hyperfine Interactions},
  year={2003},
  volume={148-149},
  pages={61-71}
}
Serpentine “polymorph” minerals (chrysotile, lizardite, and antigorite) are hydrous Mg–Fe silicates that commonly form serpentine rock (serpentinite) by hydration of olivine-pyroxene peridotites from the mantle of the Earth. During the complex geologic history of orogenic belts, the redox and hydration state of the mantle changes, and olivine and pyroxenes are replaced by serpentine group minerals during tectonic deformation and uplift. Unfortunately, modern microanalysis of minerals by… 

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