Gray E. Bebout focuses on Geochemistry, Subduction, Metamorphism, Metamorphic rock and Schist. His research on Geochemistry frequently links to adjacent areas such as Mineralogy. In his research, Volcano is intimately related to Mantle, which falls under the overarching field of Subduction.
A large part of his Metamorphism studies is devoted to Greenschist. His research in Metamorphic rock focuses on subjects like Sedimentary rock, which are connected to Tourmaline and Isotopes of oxygen. Gray E. Bebout combines subjects such as Mantle wedge and Subduction zone metamorphism with his study of Forearc.
His primary scientific interests are in Geochemistry, Subduction, Metamorphic rock, Metamorphism and Metasomatism. Gray E. Bebout has researched Geochemistry in several fields, including Forearc and Oceanic crust. His Subduction research is multidisciplinary, incorporating perspectives in Sedimentary rock, Basalt and Petrology.
In general Metamorphic rock study, his work on Protolith often relates to the realm of Metamorphic facies, thereby connecting several areas of interest. Gray E. Bebout interconnects Eclogite, Subduction zone metamorphism, Igneous rock, Partial melting and Lithology in the investigation of issues within Metamorphism. He has included themes like Trace element and Mafic in his Metasomatism study.
His main research concerns Subduction, Geochemistry, Petrology, Metamorphic rock and Seismology. As part of the same scientific family, he usually focuses on Subduction, concentrating on Sedimentary rock and intersecting with Tectonics. His study looks at the intersection of Geochemistry and topics like Chlorite with Mica and Schist.
His work investigates the relationship between Petrology and topics such as Deformation that intersect with problems in Geomorphology, Carbon cycle, Ophiolite and Boudinage. Gray E. Bebout studied Metamorphic rock and Metamorphism that intersect with Pressure solution. His Ultramafic rock research includes themes of Accretionary wedge, Blueschist, Metasomatism and Underplating.
Gray E. Bebout spends much of his time researching Subduction, Geochemistry, Petrology, Deformation and Metamorphic rock. His Subduction study frequently draws connections to other fields, such as Trace element. His Geochemistry research is multidisciplinary, relying on both Seafloor spreading, Volcanic arc and Earth science.
His Petrology research incorporates themes from Boudinage, Ophiolite, Carbon cycle and Geomorphology. His work carried out in the field of Deformation brings together such families of science as Sedimentary rock, Stratigraphic unit and Tectonics. His Metamorphic rock research incorporates themes from Blueschist, Mafic, Ultramafic rock and Underplating.
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Metamorphic chemical geodynamics of subduction zones
Gray E. Bebout.
Earth and Planetary Science Letters (2007)
Nitrogen-isotope compositions of metasedimentary rocks in the Catalina Schist, California: Implications for metamorphic devolatilization history
Gray E. Bebout;Marilyn L. Fogel.
Geochimica et Cosmochimica Acta (1992)
FRACTIONATION OF TRACE ELEMENTS BY SUBDUCTION-ZONE METAMORPHISM : EFFECT OF CONVERGENT-MARGIN THERMAL EVOLUTION
Gray E. Bebout;Jeffrey G. Ryan;William P. Leeman;Ann E. Bebout.
Earth and Planetary Science Letters (1999)
Volcanic arcs fed by rapid pulsed fluid flow through subducting slabs
Timm John;Nikolaus Gussone;Yuri Y. Podladchikov;Gray E. Bebout.
Nature Geoscience (2012)
Fluid flow and metasomatism in a subduction zone hydrothermal system: Catalina Schist terrane, California
Gray E. Bebout;Mark D. Barton.
BBe systematics in subduction-related metamorphic rocks: Characterization of the subducted component
Gray E Bebout;Jeffrey G Ryan;William P Leeman.
Geochimica et Cosmochimica Acta (1993)
Metasomatism during subduction: products and possible paths in the Catalina Schist, California
Gray E. Bebout;Mark D. Barton.
Chemical Geology (1993)
The impact of subduction-zone metamorphism on mantle-ocean chemical cycling
Gray E. Bebout.
Chemical Geology (1995)
Tectonic and metasomatic mixing in a high-T, subduction-zone mélange—insights into the geochemical evolution of the slab–mantle interface
Gray E Bebout;Mark D Barton.
Chemical Geology (2002)
Fluid and mass transfer at subduction interfaces-The field metamorphic record
Gray E. Bebout;Sarah C. Penniston-Dorland.
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