2011 - Fellow of American Geophysical Union (AGU)
2010 - Geochemistry Fellow Honor, Geochemical Society and the European Association of Geochemistry
William E. Seyfried mostly deals with Hydrothermal circulation, Mineralogy, Seawater, Geochemistry and Basalt. The Hydrothermal circulation study combines topics in areas such as Hot spring, Metal, Mid-ocean ridge and Ultramafic rock. His Mineralogy research is multidisciplinary, relying on both Environmental chemistry, Magnetite, Peridotite and Dissolution.
The study incorporates disciplines such as Sulfide, Brucite, Clay minerals and Analytical chemistry in addition to Seawater. His biological study spans a wide range of topics, including Oceanography and Hydrothermal vent. As part of one scientific family, he deals mainly with the area of Basalt, narrowing it down to issues related to the Sulfate, and often Deep sea, Precambrian, Banded iron formation and Hematite.
William E. Seyfried spends much of his time researching Hydrothermal circulation, Mineralogy, Geochemistry, Seawater and Hydrothermal vent. His Hydrothermal circulation research is multidisciplinary, incorporating perspectives in Inorganic chemistry, Redox, Sulfide, Mid-ocean ridge and Isotope fractionation. His work carried out in the field of Mineralogy brings together such families of science as Analytical chemistry, Basalt, Quartz and Dissolution.
His work investigates the relationship between Geochemistry and topics such as Plagioclase that intersect with problems in Recrystallization. His studies deal with areas such as Sulfate, Clay minerals and Brine as well as Seawater. His Hydrothermal vent research incorporates themes from Seafloor spreading, Oceanography and Chloride.
The scientist’s investigation covers issues in Hydrothermal circulation, Hydrothermal vent, Geochemistry, Mineralogy and Dissolution. William E. Seyfried performs integrative Hydrothermal circulation and Anhydrite research in his work. His Hydrothermal vent study combines topics from a wide range of disciplines, such as Redox, Hydrology, Ridge and Seafloor spreading.
William E. Seyfried combines subjects such as Sediment and Sulfate with his study of Geochemistry. His biological study focuses on Dolomite. The various areas that William E. Seyfried examines in his Dissolution study include Magnetite, Siderite, Basalt and Volumetric flow rate.
William E. Seyfried focuses on Hydrothermal circulation, Mineralogy, Hydrothermal vent, Analytical chemistry and Olivine. Many of his studies on Hydrothermal circulation apply to Quartz as well. William E. Seyfried has included themes like In situ, Redox and Dissolution in his Mineralogy study.
His Dissolution study incorporates themes from Mineral alteration, Mineral, Basalt and Volumetric flow rate. His Hydrothermal vent study deals with Isotope fractionation intersecting with Recrystallization, Mid-ocean ridge and Ridge. His biological study spans a wide range of topics, including Chemical physics, Magnetite, Brucite and Chemical engineering.
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Reduction of CO2 during serpentinization of olivine at 300 °C and 500 bar
Michael E. Berndt;Douglas E. Allen;William E. Seyfried.
Hydrothermal alteration of basalt by seawater under seawater-dominated conditions
William E Seyfried;Michael J Mottl.
Geochimica et Cosmochimica Acta (1982)
Low temperature basalt alteration by sea water: an experimental study at 70°C and 150°C
W.E. Seyfried;J.L. Bischoff.
Geochimica et Cosmochimica Acta (1979)
Hydrothermal chemistry of seawater from 25 degrees to 350 degrees C
James L. Bischoff;William E. Seyfried.
American Journal of Science (1978)
Hydrocarbons in Hydrothermal Vent Fluids: The Role of Chromium-Bearing Catalysts
Dionysis I. Foustoukos;William E. Seyfried.
Alteration of the oceanic crust: Implications for geochemical cycles of lithium and boron
W.E. Seyfried;D.R. Janecky;M.J. Mottl.
Geochimica et Cosmochimica Acta (1984)
Compositional controls on vent fluids from ultramafic-hosted hydrothermal systems at mid-ocean ridges: An experimental study at 400°C, 500 bars
Douglas E. Allen;William E Seyfried.
Geochimica et Cosmochimica Acta (2003)
Hydrothermal serpentinization of peridotite within the oceanic crust: Experimental investigations of mineralogy and major element chemistry
D. R. Janecky;William E Seyfried.
Geochimica et Cosmochimica Acta (1986)
Experimental seawater-basalt interaction at 300°C, 500 bars, chemical exchange, secondary mineral formation and implications for the transport of heavy metals
W.E Seyfried;J.L Bischoff.
Geochimica et Cosmochimica Acta (1981)
Redox evolution and mass transfer during serpentinization : An experimental and theoretical study at 200 °C, 500 bar with implications for ultramafic-hosted hydrothermal systems at Mid-Ocean Ridges
William E Seyfried;D. I. Foustoukos;Qi Fu.
Geochimica et Cosmochimica Acta (2007)
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