What is he best known for?
The fields of study he is best known for:
- Basalt
- Igneous rock
- Volcano
Mary R. Reid mainly focuses on Geochemistry, Silicic, Zircon, Magma chamber and Magma.
His Geochemistry research focuses on Partial melting, Trace element, Basalt and Mantle.
His work investigates the relationship between Silicic and topics such as Porphyritic that intersect with problems in Alkali feldspar, Hydrothermal circulation, Peralkaline rock and Lava.
His work is dedicated to discovering how Zircon, Rhyolite are connected with Phenocryst and Mineralogy and other disciplines.
He interconnects Supervolcano and Mineral resource classification in the investigation of issues within Magma chamber.
His research brings together the fields of Caldera and Magma.
His most cited work include:
- Bedrock incision, rock uplift and threshold hillslopes in the northwestern Himalayas (849 citations)
- Prolonged residence times for the youngest rhyolites associated with Long Valley Caldera:230Th—238U ion microprobe dating of young zircons (263 citations)
- Geochemistry of primary and least fractionated lavas from Okmok Volcano, Central Aleutians: Implications for arc magmagenesis (177 citations)
What are the main themes of his work throughout his whole career to date?
His scientific interests lie mostly in Geochemistry, Basalt, Magma, Mantle and Zircon.
His study in Silicic, Caldera, Rhyolite, Mafic and Magma chamber is carried out as part of his Geochemistry studies.
His research in Caldera intersects with topics in Igneous rock, Igneous differentiation and Volcanic rock.
His work carried out in the field of Basalt brings together such families of science as Basin and Range Province, Plagioclase, Olivine and Asthenosphere.
His biological study spans a wide range of topics, including Tectonics, Lithosphere, Petrology and Crust.
As part of the same scientific family, Mary R. Reid usually focuses on Zircon, concentrating on Supervolcano and intersecting with Mineral resource classification.
He most often published in these fields:
- Geochemistry (88.06%)
- Basalt (29.85%)
- Magma (34.33%)
What were the highlights of his more recent work (between 2011-2021)?
- Geochemistry (88.06%)
- Mantle (26.87%)
- Basalt (29.85%)
In recent papers he was focusing on the following fields of study:
The scientist’s investigation covers issues in Geochemistry, Mantle, Basalt, Lithosphere and Zircon.
In his study, which falls under the umbrella issue of Geochemistry, Volcano and Sanidine is strongly linked to Volcanism.
Mary R. Reid has researched Basalt in several fields, including Petrology and Asthenosphere.
His Lithosphere research incorporates themes from Xenolith and Mafic.
He performs multidisciplinary study in Zircon and Allanite in his work.
His Silicic study incorporates themes from Rhyolite and Igneous differentiation.
Between 2011 and 2021, his most popular works were:
- Shallow melting of MORB‐like mantle under hot continental lithosphere, Central Anatolia (39 citations)
- Magma mixing and the generation of isotopically juvenile silicic magma at Yellowstone caldera inferred from coupling 238 U– 230 Th ages with trace elements and Hf and O isotopes in zircon and Pb isotopes in sanidine (33 citations)
- Melting under the Colorado Plateau, USA (27 citations)
In his most recent research, the most cited papers focused on:
- Basalt
- Igneous rock
- Volcano
Mary R. Reid spends much of his time researching Geochemistry, Lithosphere, Mantle, Zircon and Basalt.
His work on Caldera and Igneous differentiation as part of general Geochemistry research is often related to Population, thus linking different fields of science.
His work deals with themes such as Earth science and Mafic, which intersect with Lithosphere.
The various areas that Mary R. Reid examines in his Mafic study include Crust, Xenolith, Magmatism, Peridotite and Geochemical cycle.
Mary R. Reid has included themes like Quartz, Magma and Silicic in his Zircon study.
In his study, Metasomatism, Basin and Range Province, Transition zone and Geophysics is strongly linked to Asthenosphere, which falls under the umbrella field of Basalt.
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