What is he best known for?
The fields of study he is best known for:
- Sedimentary rock
- Mineral
- Paleontology
Philippe Muchez mainly focuses on Geochemistry, Mineralogy, Diagenesis, Fluid inclusions and Calcite.
In his research, Petrography is intimately related to Mineralization, which falls under the overarching field of Geochemistry.
In his research on the topic of Mineralogy, Isotopes of strontium and Magnetite is strongly related with Provenance.
His research integrates issues of Orogeny, Rift, Digenite, Fold and thrust belt and Hypogene in his study of Diagenesis.
His Fluid inclusions research entails a greater understanding of Quartz.
The study incorporates disciplines such as Carbonate and Meteoric water in addition to Calcite.
His most cited work include:
- 7: Extensional tectonics and the timing and formation of basin-hosted deposits in Europe (109 citations)
- Carbonate-Hosted Zn-Pb Deposits in Upper Silesia, Poland: Origin and Evolution of Mineralizing Fluids and Constraints on Genetic Models (102 citations)
- Zinc, sulfur and lead isotopic variations in carbonate-hosted Pb–Zn sulfide deposits, southwest China (79 citations)
What are the main themes of his work throughout his whole career to date?
His scientific interests lie mostly in Geochemistry, Mineralogy, Paleontology, Fluid inclusions and Archaeology.
His Geochemistry study frequently draws connections between related disciplines such as Mineralization.
Philippe Muchez interconnects Mining engineering and Foreland basin in the investigation of issues within Mineralization.
He is interested in Dolomite, which is a branch of Mineralogy.
In his work, Carbonate is strongly intertwined with Calcite, which is a subfield of Fluid inclusions.
His research investigates the link between Quartz and topics such as Metamorphic rock that cross with problems in Metamorphism.
He most often published in these fields:
- Geochemistry (54.95%)
- Mineralogy (15.02%)
- Paleontology (15.02%)
What were the highlights of his more recent work (between 2014-2021)?
- Geochemistry (54.95%)
- Pegmatite (8.41%)
- Mineralization (10.51%)
In recent papers he was focusing on the following fields of study:
Philippe Muchez focuses on Geochemistry, Pegmatite, Mineralization, Quartz and Fluid inclusions.
His Geochemistry study combines topics from a wide range of disciplines, such as Inclusion, Orogeny and Hydrothermal circulation.
His Pegmatite research includes elements of Muscovite, Vein and Mineral.
The concepts of his Mineralization study are interwoven with issues in Mine planning, Geologic map, Earth science and Pyrite.
Philippe Muchez focuses mostly in the field of Fluid inclusions, narrowing it down to matters related to Calcite and, in some cases, Sphalerite, Siliciclastic, Diagenesis and Meteoric water.
His Sedimentary rock research incorporates elements of Nappe, Dolomite and Breccia.
Between 2014 and 2021, his most popular works were:
- Fluid fractionation of tungsten during granite–pegmatite differentiation and the metal source of peribatholitic W quartz veins: Evidence from the Karagwe-Ankole Belt (Rwanda) (47 citations)
- Diagenetic origin of the stratiform Cu–Co deposit at Kamoto in the Central African Copperbelt (36 citations)
- Unraveling rare earth element signatures in hydrothermal carbonate minerals using a source–sink system (35 citations)
In his most recent research, the most cited papers focused on:
- Sedimentary rock
- Mineral
- Paleontology
Philippe Muchez mostly deals with Geochemistry, Pegmatite, Petrography, Fluid inclusions and Sedimentary rock.
His biological study spans a wide range of topics, including Inclusion and Orogeny.
His work carried out in the field of Pegmatite brings together such families of science as Muscovite, Anticline, Metasomatism and Greisen.
The various areas that Philippe Muchez examines in his Petrography study include Hearth, Conglomerate, Archaeometallurgy and Syncline.
His study in Sedimentary rock is interdisciplinary in nature, drawing from both Nappe, Mineralization, Pyrite, Ophiolite and Carbonate platform.
His Calcite research is multidisciplinary, incorporating perspectives in Fault, Carbonate, Tectonics and Radiogenic nuclide.
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