Skip Nav Destination
Article navigation
Other|
February 01, 1992
High-pressure fluid-absent melting experiments in the presence of graphite; oxygen fugacity, ferric/ferrous ratio and dissolved CO 2
John R. Holloway;
John R. Holloway
Arizona State Univ., Geol. Dep., Tempe, AZ, United States
Search for other works by this author on:
John R. Holloway
Arizona State Univ., Geol. Dep., Tempe, AZ, United States
Vivian Pan
Gisli Gudmundsson
Publisher: Deutsche Mineralogische Gesellschaft, Sociedad Española de Mineralogia, Societá Italiana di Mineralogia e Petrologia, Société Francaise de Minéralogie
First Online:
02 Mar 2017
Online Issn: 1617-4011
Print Issn: 0935-1221
GeoRef, Copyright 2008, American Geological Institute. Reference includes data from Geoline, Bundesanstalt fur Geowissenschaften und Rohstoffe, Hanover, Germany
European Journal of Mineralogy (1992) 4 (1): 105–114.
Article history
First Online:
02 Mar 2017
Citation
John R. Holloway, Vivian Pan, Gisli Gudmundsson; High-pressure fluid-absent melting experiments in the presence of graphite; oxygen fugacity, ferric/ferrous ratio and dissolved CO 2. European Journal of Mineralogy 1992;; 4 (1): 105–114. doi:
Download citation file:
You could not be signed in. Please check your email address / username and password and try again.
Index Terms/Descriptors
Citing articles via
Related Articles
Role of iron and reducing conditions on the stability of dolomite + coesite between 4.25 and 6 GPa – a potential mechanism for diamond formation during subduction
European Journal of Mineralogy
Related Book Content
High-pressure mineralogy of diamond genesis
Advances in High-Pressure Mineralogy
Discovery of the oldest oxic granitoids in the Kaapvaal Craton and its implications for the redox evolution of early Earth
Evolution of Early Earth's Atmosphere, Hydrosphere, and Biosphere - Constraints from Ore Deposits
Density at High Pressure; Compressibility
Handbook of Physical Constants
Mica chemistry as an indicator of oxygen and halogen fugacities in the CanTung and other W-related granitoids in the North American Cordillera
Ore-bearing Granite Systems; Petrogenesis and Mineralizing Processes