Non-hydrostatic stress field orientation inferred from orthopyroxene (Pbca) to low-clinoenstatite (P21/c) inversion in partially dehydrated serpentinites
- DOI
- 10.2138/am-2018-6362
- Published
- 2018-06-01
- Container
- American Mineralogist
- Publisher
- Mineralogical Society of America
- Open access
- unknown
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Cite this work
BibTeX
@article{allodium:10.2138/am-2018-6362,
title = {Non-hydrostatic stress field orientation inferred from orthopyroxene (Pbca) to low-clinoenstatite (P21/c) inversion in partially dehydrated serpentinites},
author = {Maxime Clément and José Alberto Padrón-Navarta and Andréa Tommasi and David Mainprice},
year = {2018},
journal = {American Mineralogist},
doi = {10.2138/am-2018-6362},
url = {https://doi.org/10.2138/am-2018-6362}
}RIS
TY - JOUR TI - Non-hydrostatic stress field orientation inferred from orthopyroxene (Pbca) to low-clinoenstatite (P21/c) inversion in partially dehydrated serpentinites AU - Maxime Clément AU - José Alberto Padrón-Navarta AU - Andréa Tommasi AU - David Mainprice PY - 2018 JO - American Mineralogist DO - 10.2138/am-2018-6362 UR - https://doi.org/10.2138/am-2018-6362 ER -
APA
Clément, M., Padrón-Navarta, J. A., Tommasi, A., & Mainprice, D. (2018). Non-hydrostatic stress field orientation inferred from orthopyroxene (Pbca) to low-clinoenstatite (P21/c) inversion in partially dehydrated serpentinites. American Mineralogist. https://doi.org/10.2138/am-2018-6362
Source records
- crossref · retrieved 2026-09-25T10:22:03.567Z