Thermal equation of state of Cr-pyrope: implications for entrapment pressure of Cr-pyrope inclusion in diamond
Author:
Funder
National Natural Science Foundation of China
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
https://link.springer.com/content/pdf/10.1007/s00410-022-01932-7.pdf
Reference125 articles.
1. Angel RJ (2000) Equations of state rev. Mineral Geochem 41(1):35–59. https://doi.org/10.2138/rmg.2000.41.2
2. Angel RJ, Mazzucchelli ML, Alvaro M, Nimis P, Nestola F (2014a) Geobarometry from host-inclusion systems: the role of elastic relaxation. Am Mineral 99(10):2146–2149. https://doi.org/10.2138/am-2014-5047
3. Angel RJ, Gonzalez-Platas J, Alvaro M (2014b) EosFit7c and a Fortran module (library) for equation of state calculations. Z Krystallogr 229(5):405–419. https://doi.org/10.1515/zkri-2013-1711
4. Angel RJ, Alvaro M, Nestola F, Mazzucchelli ML (2015) Diamond thermoelastic properties and implications for determining the pressure of formation of diamond-inclusion systems. Russ Geol Geophys 56(1):211–220. https://doi.org/10.1016/j.rgg.2015.01.014
5. Angel RJ, Mazzucchelli ML, Alvaro M, Nestola F (2017) EosFit-Pinc: A simple GUI for host-inclusion elastic thermobarometry. Am Mineral 102:1957–1960. https://doi.org/10.2138/am-2017-6190
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