His scientific interests lie mostly in Mineralogy, Copper, Silicate, Partition coefficient and Analytical chemistry. His research integrates issues of Basalt, Igneous rock, Mafic and Ultramafic rock in his study of Mineralogy. His Igneous rock research incorporates elements of Fugacity, Pegmatite and Ore genesis.
His work focuses on many connections between Copper and other disciplines, such as Molybdenum, that overlap with his field of interest in Molybdate, Chlorine and Crystallization. Magnetite is closely connected to Brine in his research, which is encompassed under the umbrella topic of Analytical chemistry. The concepts of his Magnetite study are interwoven with issues in Sulfide, Pyrrhotite, Sulfur, Fluid inclusions and Vapor pressure.
His primary scientific interests are in Mineralogy, Analytical chemistry, Geochemistry, Partition coefficient and Silicate. Philip A. Candela has researched Mineralogy in several fields, including Equilibrium constant and Quartz, Hydrothermal circulation, Fluid inclusions. His biological study spans a wide range of topics, including Crystallization, Magnetite, Pyrrhotite, Copper and Brine.
His research in Brine tackles topics such as Chloride which are related to areas like Sodium, Inorganic chemistry and Sulfur. Partition coefficient is integrated with Solubility and Saturation in his study. His work in Silicate covers topics such as Molybdenum which are related to areas like Tungsten, Molybdenite and Oxide.
His main research concerns Mineralogy, Geochemistry, Analytical chemistry, Indium and Hydrothermal circulation. His Mineralogy research incorporates themes from Banded iron formation and Amphibole. His study in the field of Continental crust is also linked to topics like Composition.
Philip A. Candela applies his multidisciplinary studies on Analytical chemistry and Partition coefficient in his research. His Hydrothermal circulation research includes elements of Talc, Quartz and Dissolution. His research investigates the connection between Silicate and topics such as Metal that intersect with problems in Carbide.
Philip A. Candela focuses on Mineralogy, Analytical chemistry, Pyrrhotite, Partition coefficient and Dissolution. His work carried out in the field of Mineralogy brings together such families of science as Asbestiform and Asbestos. His Analytical chemistry study combines topics from a wide range of disciplines, such as Sulfide and Mafic.
His research in Dissolution intersects with topics in Geochemistry, Mantle, Crust, Sedimentary exhalative deposits and Hydrothermal circulation. His Hydrothermal circulation research is multidisciplinary, incorporating elements of Mineral deposit and Copper. Throughout his Saturation studies, Philip A. Candela incorporates elements of other sciences such as Sulfur, Mineral redox buffer, Silicate and Dacite.
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The partitioning of copper and molybdenum between silicate melts and aqueous fluids
Philip A Candela;Heinrich D Holland.
Geochimica et Cosmochimica Acta (1984)
Apatite in Igneous Systems
Philip M. Piccoli;Philip A. Candela.
Reviews in Mineralogy & Geochemistry (2002)
A Review of Shallow, Ore-related Granites: Textures, Volatiles, and Ore Metals
Philip A. Candela.
Journal of Petrology (1997)
A mass transfer model for copper and molybdenum in magmatic hydrothermal systems; the origin of porphyry-type ore deposits
Philip A. Candela;Heinrich D. Holland.
Economic Geology (1986)
Controls on ore metal ratios in granite-related ore systems: an experimental and computational approach
Philip A. Candela.
Transactions of The Royal Society of Edinburgh-earth Sciences (1992)
Copper partitioning in a melt-vapor-brine-magnetite-pyrrhotite assemblage
Adam C. Simon;Thomas Pettke;Philip A. Candela;Philip M. Piccoli.
Geochimica et Cosmochimica Acta (2006)
Apatite in felsic rocks; a model for the estimation of initial halogen concentrations in the Bishop Tuff (Long Valley) and Tuolumne Intrusive Suite (Sierra Nevada Batholith) magmas
Philip Piccoli;Philip Candela.
American Journal of Science (1994)
Magnetite solubility and iron transport in magmatic-hydrothermal environments
Adam C. Simon;Thomas Pettke;Philip A. Candela;Philip M. Piccoli.
Geochimica et Cosmochimica Acta (2004)
Magmatic sulfides and Au:Cu ratios in porphyry deposits: an experimental study of copper and gold partitioning at 850°C, 100 MPa in a haplogranitic melt pyrrhotite intermediate solid solution gold metal assemblage, at gas saturation
P.J. Jugo;P.A. Candela;P.M. Piccoli.
Lithos (1999)
The influence of oxygen fugacity on tungsten and molybdenum partitioning between silicate melts and ilmenite
Philip A. Candela;Stephen L. Bouton.
Economic Geology (1990)
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