Amanote Research
Register
Sign In
The Stability of Graphite and Diamond as a Function of the Oxygen Fugasity in the Mantle
doi 10.29173/ikc1023
Full Text
Open PDF
Abstract
Available in
full text
Date
Unknown
Authors
Unknown
Publisher
University of Alberta
Related search
The Stability of Carbonate Melts in the Mantle
Acta Geologica Sinica
Geology
The Role of fO2 Regime in Evolution of Mantle Metasomatism and Diamond Formation
The Proterozoic: Its Role in Diamond Petrogenesis and the Emplacement of Mantle Derived Intrusives
Graphite Pseudomorphs After Diamond in the Eclogite-Peridotite Massif of Beni Bousera, Morocco and a Review of Anomalous Diamond Occurrences
Oxygen Transport in Hemorrhagic Shock as a Function of the Hematocrit Ratio
American Journal of Physiology-Legacy Content
Determination of the Ferric Iron Content of Diamond Inclusions From George Creek Using Mossbauer Specrtoscopy With Implications for Mantle Oxygen Fugacity During Diamond Genesis
Controls on the Stability and Composition of Amphibole in the Earth’s Mantle
Contributions to Mineralogy and Petrology
Petrology
Geochemistry
Geophysics
Crystallization and Texturing of Diamond Formed by the Direct Transformation From Graphite
Nihon Kessho Gakkaishi
Stability of (Mg,Fe)SiO3perovskite and the Structure of the Lowermost Mantle
Geophysical Research Letters
Earth
Planetary Sciences
Geophysics
