2020 - Fellow of American Geophysical Union (AGU)
2003 - Distinguished Scientist Award, American Heart Association
Fellow of the Geological Society of America
Geochemistry, Crust, Migmatite, Petrology and Metamorphism are his primary areas of study. His Geochemistry research is multidisciplinary, incorporating perspectives in Subduction and Granulite. His Subduction research integrates issues from Proterozoic, Mantle and Plate tectonics.
His Migmatite study incorporates themes from Quartz, Feldspar and Pluton. His work carried out in the field of Petrology brings together such families of science as Anatexis, Shear zone and Geomorphology. His research in Metamorphism intersects with topics in Fission track dating and Paragenesis.
Michael Brown spends much of his time researching Geochemistry, Metamorphism, Metamorphic rock, Migmatite and Petrology. Michael Brown interconnects Subduction, Eclogite and Granulite in the investigation of issues within Geochemistry. His Metamorphism research focuses on subjects like Plate tectonics, which are linked to Lithosphere.
His Metamorphic rock research is multidisciplinary, incorporating elements of Metamorphic facies, Igneous rock and Monazite. The Migmatite study combines topics in areas such as Anatexis, Biotite and Pluton. His Petrology study frequently intersects with other fields, such as Shear zone.
Michael Brown mostly deals with Geochemistry, Subduction, Eclogite, Plate tectonics and Metamorphism. His Geochemistry research includes elements of Blueschist and Eastern china. His studies deal with areas such as Earth, Geophysics and Continental crust as well as Subduction.
The concepts of his Continental crust study are interwoven with issues in Lithosphere, Petrology and Archean. His Metamorphism research is multidisciplinary, relying on both Metamorphic rock, Earth science, Devonian and Pluton. His Crust study combines topics in areas such as Migmatite and Monazite.
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The generation, segregation, ascent and emplacement of granite magma: the migmatite-to-crustally-derived granite connection in thickened orogens
Michael Brown.
Earth-Science Reviews (1994)
Metamorphic Conditions in Orogenic Belts: A Record of Secular Change
M. Brown.
International Geology Review (2007)
Duality of thermal regimes is the distinctive characteristic of plate tectonics since the Neoarchean
Michael Brown.
Geology (2006)
Granite: From genesis to emplacement
Michael Brown.
Geological Society of America Bulletin (2013)
Shear-zone systems and melts: feedback relations and self-organization in orogenic belts
Michael Brown;Gary S. Solar.
Journal of Structural Geology (1998)
Subduction styles in the Precambrian: Insight from numerical experiments
E. Sizova;T. Gerya;T. Gerya;M. Brown;L.L. Perchuk;L.L. Perchuk.
Lithos (2010)
Granite magma generation, ascent and emplacement within a transpressional orogen
R. S. D’Lemos;M. Brown;R. A. Strachan.
Journal of the Geological Society (1992)
Crustal melting and melt extraction, ascent and emplacement in orogens: mechanisms and consequences
Michael Brown.
Journal of the Geological Society (2007)
Granite ascent and emplacement during contractional deformation in convergent orogens
Michael Brown;Gary S. Solar.
Journal of Structural Geology (1998)
Delamination and recycling of Archaean crust caused by gravitational instabilities
Tim E. Johnson;Michael Brown;Boris J. P. Kaus;Boris J. P. Kaus;Jill A. VanTongeren.
Nature Geoscience (2014)
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