What is he best known for?
The fields of study he is best known for:
- Mineral
- Sedimentary rock
- Paleontology
Adrian J. Boyce focuses on Geochemistry, Mineralogy, Hydrothermal circulation, Pyrite and Sedimentary rock.
The concepts of his Geochemistry study are interwoven with issues in Mineralization, δ34S and Quartz, Fluid inclusions.
His Mineralogy study integrates concerns from other disciplines, such as Galena, Troilite and Anhydrite.
The Hydrothermal circulation study combines topics in areas such as Sulfur, Sulfide, Zinc, Seawater and Sulfate.
His Pyrite research focuses on Chalcopyrite and how it connects with Tennantite.
His research in Sedimentary rock intersects with topics in Carbonate, Dolomite, Mineral resource classification and Isotopes of oxygen.
His most cited work include:
- High frequencies of alpha-thalassaemia are the result of natural selection by malaria. (348 citations)
- Geologic evolution of the Escondida area, northern Chile: A model for spatial and temporal localization of porphyry Cu mineralization (177 citations)
- Why are some genetic diseases common ? Distinguishing selection from other processes by molecular analysis of globin gene variants (115 citations)
What are the main themes of his work throughout his whole career to date?
His primary areas of study are Geochemistry, Mineralogy, Pyrite, Hydrothermal circulation and δ34S.
His biological study spans a wide range of topics, including Mineralization, Fluid inclusions and Vein.
Vein is a subfield of Quartz that he studies.
Adrian J. Boyce studied Mineralogy and Sulfur that intersect with Sulfate.
Adrian J. Boyce combines subjects such as Arsenopyrite, Chalcopyrite and Diagenesis with his study of Pyrite.
His Hydrothermal circulation research integrates issues from Seawater and Sulfide.
He most often published in these fields:
- Geochemistry (66.30%)
- Mineralogy (23.48%)
- Pyrite (18.04%)
What were the highlights of his more recent work (between 2017-2021)?
- Geochemistry (66.30%)
- Pyrite (18.04%)
- δ34S (12.83%)
In recent papers he was focusing on the following fields of study:
His primary scientific interests are in Geochemistry, Pyrite, δ34S, Sedimentary rock and Hydrothermal circulation.
His studies deal with areas such as Dolomitization, Carbonate and Amphibole as well as Geochemistry.
His study on Pyrite also encompasses disciplines like
- Mineralization that intertwine with fields like Breccia,
- Chalcopyrite, which have a strong connection to Mineralogy.
His δ34S research is multidisciplinary, incorporating elements of Batholith, Evaporite, Environmental chemistry, Troodos Ophiolite and Galena.
He has researched Sedimentary rock in several fields, including Facies and Ultramafic rock.
His Hydrothermal circulation study frequently links to other fields, such as Mineral.
Between 2017 and 2021, his most popular works were:
- The evolution of magma during continental rifting : new constraints from the isotopic and trace element signatures of silicic magmas from Ethiopian volcanoes (25 citations)
- Delineating sources of groundwater recharge in an arsenic-affected Holocene aquifer in Cambodia using stable isotope-based mixing models (23 citations)
- Mixing of magmatic-hydrothermal and metamorphic fluids and the origin of peribatholitic Sn vein-type deposits in Rwanda (20 citations)
In his most recent research, the most cited papers focused on:
- Mineral
- Sedimentary rock
- Ecology
His primary areas of investigation include Geochemistry, Dolomitization, Pyrite, δ34S and Trace element.
His work carried out in the field of Geochemistry brings together such families of science as Carbonate and Hydrothermal circulation.
His Dolomitization study incorporates themes from Mineralization, Dolostone and Dolomite.
His Pyrite study combines topics from a wide range of disciplines, such as Snowball Earth, Anoxic sediments and Metallogeny.
His δ34S research incorporates elements of Chalcopyrite, Rhenium, Peridotite, Country rock and Pillow lava.
His Trace element study incorporates themes from Oil shale, Propylitic alteration, Weathering, Isotopes of strontium and Volcanogenic massive sulfide ore deposit.
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