Philip M. Piccoli mainly investigates Geochemistry, Analytical chemistry, Mineralogy, Copper and Apatite. In general Geochemistry study, his work on Syenogranite often relates to the realm of Hypersolvus, Group and Proterozoic, thereby connecting several areas of interest. His research in Analytical chemistry focuses on subjects like Solubility, which are connected to Fluid inclusions.
His research ties Secondary ion mass spectrometry and Mineralogy together. His Copper research includes themes of Pyrrhotite, Aqueous solution and Chloride. His Apatite research includes elements of Felsic and Igneous rock.
The scientist’s investigation covers issues in Geochemistry, Mineralogy, Analytical chemistry, Silicate and Brine. Mantle, Metamorphism, Felsic, Zircon and Mafic are among the areas of Geochemistry where Philip M. Piccoli concentrates his study. His work investigates the relationship between Felsic and topics such as Apatite that intersect with problems in Igneous rock.
His research in Mineralogy tackles topics such as Crystallization which are related to areas like Fugacity. The various areas that Philip M. Piccoli examines in his Analytical chemistry study include Copper, Pyrrhotite, Aqueous solution and Solubility. His study in Solubility is interdisciplinary in nature, drawing from both Metal and Dissolution.
Philip M. Piccoli focuses on Geochemistry, Petrology, Mantle, Zircon and Eclogite. His study on Geochemistry is mostly dedicated to connecting different topics, such as Indium. His Schist study in the realm of Petrology interacts with subjects such as Path.
His Zircon study combines topics from a wide range of disciplines, such as Phengite and Plagioclase. Philip M. Piccoli has researched Archean in several fields, including Pyrrhotite, Pyrite and Crust. His Biotite research is multidisciplinary, relying on both Crystallization, Anorthite and Analytical chemistry.
Philip M. Piccoli spends much of his time researching Geochemistry, Mantle, North china, Mafic and Coesite. Philip M. Piccoli has included themes like Fugacity and Oceanic crust in his Geochemistry study. His Mantle research integrates issues from Metamorphism, Petrology, Protolith and Amphibole.
His biological study spans a wide range of topics, including Phase equilibrium and Bay.
This overview was generated by a machine learning system which analysed the scientist’s body of work. If you have any feedback, you can contact us here.
Tectonic discrimination of granitoids
Papu D. Maniar;Philip M. Piccoli.
Geological Society of America Bulletin (1989)
Further characterisation of the 91500 zircon crystal
Michael Wiedenbeck;John M. Hanchar;William H. Peck;Paul Sylvester.
Geostandards and Geoanalytical Research (2004)
Can otolith microchemistry chart patterns of migration and habitat utilization in anadromous fishes
David H. Secor;A. Henderson-Arzapalo;P.M. Piccoli.
Journal of Experimental Marine Biology and Ecology (1995)
Apatite in Igneous Systems
Philip M. Piccoli;Philip A. Candela.
Reviews in Mineralogy & Geochemistry (2002)
Comparison of accuracy, precision, and sensitivity in elemental assays of fish otoliths using the electron microprobe, proton-induced X-ray emission, and laser ablation inductively coupled plasma mass spectrometry
S E Campana;S R Thorrold;C M Jones;D Günther.
Canadian Journal of Fisheries and Aquatic Sciences (1997)
Magmatic Apatite: A Powerful, Yet Deceptive, Mineral
James D. Webster;Philip M. Piccoli.
Elements (2015)
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)
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