MafiCH: a general model for H2O–CO2 solubility in mafic magmas
Author:
Funder
national science foundation
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
https://link.springer.com/content/pdf/10.1007/s00410-022-01903-y.pdf
Reference50 articles.
1. Allison CM, Roggensack K, Clarke AB (2019) H2O–CO2 solubility in alkali-rich mafic magmas: new experiments at mid-crustal pressures. Contrib Mineral Petrol 174:58. https://doi.org/10.1007/s00410-019-1592-4
2. Baker MB, Grove TL (1985) Kinetic controls on pyroxene nucleation and metastable liquid lines of descent in a basaltic andesite. Am Mineral 70:279–287
3. Behrens H, Misiti V, Freda C, Vetere F, Botcharnikov RE, Scarlato P (2009) Solubility of H2O and CO2 in ultrapotassic melts at 1200 and 1250 degrees C and pressure from 50 to 500 MPa. Am Mineral 94:105–120. https://doi.org/10.2138/am.2009.2796
4. Berndt J, Liebske C, Holtz F, Freise M, Nowak M, Ziegenbein D, Hurkuck W, Koepke J (2002) A combined rapid-quench and H2-membrane setup for internally heated pressure vessels: description and application for water solubility in basaltic melts. Am Mineral 87:1717–1726
5. Blank JG, Brooker RA (1994) Experimental studies of carbon dioxide in silicate melts: solubility, speciation, and stable carbon isotope behavior. In: Carroll MR, Holloway JR (eds) Volatiles in magmas, vol 30. Mineralogical Society of America, Washington, pp 157–186
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