What is he best known for?
The fields of study he is best known for:
- Volcano
- Oceanography
- Basalt
His scientific interests lie mostly in Hydrothermal circulation, Oceanography, Geochemistry, Mineralogy and Seawater.
His Hydrothermal circulation research is multidisciplinary, incorporating perspectives in Abiogenic petroleum origin, Tectonics and Oceanic crust.
His Oceanography research is multidisciplinary, relying on both Helium and Hydrothermal vent.
His Geochemistry study combines topics in areas such as Lau Basin and Chimney.
The study incorporates disciplines such as Environmental chemistry, Lost City Hydrothermal Field, Ultramafic rock and Mantle in addition to Mineralogy.
John E. Lupton interconnects Subduction and Volcanic arc in the investigation of issues within Volcano.
His most cited work include:
- Abiogenic hydrocarbon production at lost city hydrothermal field. (520 citations)
- A Major Helium-3 Source at 15°S on the East Pacific Rise (300 citations)
- Geochemistry of hydrothermal fluids from Axial Seamount hydrothermal emissions study vent field, Juan de Fuca Ridge: Subseafloor boiling and subsequent fluid‐rock interaction (295 citations)
What are the main themes of his work throughout his whole career to date?
Hydrothermal circulation, Geochemistry, Volcano, Oceanography and Mineralogy are his primary areas of study.
His Hydrothermal circulation research integrates issues from Seawater, Seafloor spreading, Submarine and Ridge.
His Seafloor spreading research focuses on Mid-ocean ridge and how it relates to Petrology and Oceanic crust.
His study explores the link between Geochemistry and topics such as Lau Basin that cross with problems in Rift zone and Back-arc basin.
The Volcano study combines topics in areas such as Subduction and Volcanic arc.
His Oceanography research incorporates themes from Paleontology and Rift.
He most often published in these fields:
- Hydrothermal circulation (52.54%)
- Geochemistry (47.46%)
- Volcano (33.33%)
What were the highlights of his more recent work (between 2010-2020)?
- Geochemistry (47.46%)
- Hydrothermal circulation (52.54%)
- Volcano (33.33%)
In recent papers he was focusing on the following fields of study:
John E. Lupton mainly investigates Geochemistry, Hydrothermal circulation, Volcano, Oceanography and Mantle.
John E. Lupton combines subjects such as Lau Basin, Subduction and Seawater with his study of Geochemistry.
In the subject of general Hydrothermal circulation, his work in Hydrothermal vent is often linked to Autotrophic Processes, thereby combining diverse domains of study.
His Volcano research includes themes of Rift and Subaerial.
When carried out as part of a general Oceanography research project, his work on Water column and Ridge is frequently linked to work in Hydrogen, therefore connecting diverse disciplines of study.
His Mantle study incorporates themes from Deep sea, Earth science, Helium, Petrology and Mantle plume.
Between 2010 and 2020, his most popular works were:
- Submarine hydrothermal activity and gold-rich mineralization at Brothers Volcano, Kermadec Arc, New Zealand (143 citations)
- Active submarine eruption of boninite in the northeastern Lau Basin (104 citations)
- Hydrothermal Plumes: Near and Far Field (95 citations)
In his most recent research, the most cited papers focused on:
- Volcano
- Basalt
- Oceanography
John E. Lupton spends much of his time researching Volcano, Geochemistry, Hydrothermal circulation, Basalt and Caldera.
His Volcano research is multidisciplinary, incorporating elements of Seawater, Hydrothermal vent, Lau Basin and Seamount.
His Geochemistry research integrates issues from Subduction, Rift and Seafloor spreading, Oceanography, Water column.
In most of his Hydrothermal circulation studies, his work intersects topics such as Mineralogy.
In his study, Mafic and Volcanogenic massive sulfide ore deposit is inextricably linked to Volcanic rock, which falls within the broad field of Basalt.
In Caldera, John E. Lupton works on issues like Chimney, which are connected to δ34S, Dacite, Pyrite and Volcanic cone.
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