2013 - Fellow of American Geophysical Union (AGU)
Fellow of the Geological Society of America
Michael R. Perfit spends much of his time researching Basalt, Geochemistry, Mid-ocean ridge, Mantle and Mineralogy. In his study, Polybaric melting and Magma is strongly linked to Lava, which falls under the umbrella field of Basalt. The concepts of his Mid-ocean ridge study are interwoven with issues in Seafloor spreading and Petrology.
Michael R. Perfit works mostly in the field of Mantle, limiting it down to concerns involving Mantle wedge and, occasionally, Mantle convection, Transition zone, Hotspot and Mantle plume. His work in the fields of Volatiles overlaps with other areas such as Sulfur, Chlorine and Carbon dioxide. As part of the same scientific family, Michael R. Perfit usually focuses on Partial melting, concentrating on Volcanic rock and intersecting with Igneous rock.
Michael R. Perfit mostly deals with Geochemistry, Basalt, Mid-ocean ridge, Lava and Mantle. The various areas that he examines in his Geochemistry study include Ridge and Oceanic crust. Michael R. Perfit interconnects Ridge, Igneous rock and Andesites in the investigation of issues within Basalt.
His work is dedicated to discovering how Mid-ocean ridge, Earth science are connected with Lithosphere and other disciplines. His Lava study integrates concerns from other disciplines, such as Seafloor spreading, Petrology, Geomorphology and Dense-rock equivalent. His research integrates issues of Mantle wedge, Mineralogy, Olivine, Trace element and Transition zone in his study of Mantle.
Geochemistry, Mid-ocean ridge, Petrology, Basalt and Mantle are his primary areas of study. As part of his studies on Geochemistry, Michael R. Perfit often connects relevant areas like Ridge. His research integrates issues of Earth science, Igneous rock, Seafloor spreading, Oceanography and Crustal assimilation in his study of Mid-ocean ridge.
His Petrology research incorporates themes from Lava and Magma. His Basalt study incorporates themes from Ridge, Trace element, Plagioclase and Oceanic crust. Michael R. Perfit usually deals with Mantle and limits it to topics linked to Transition zone and Mantle plume and Planetary science.
The scientist’s investigation covers issues in Geochemistry, Basalt, Mid-ocean ridge, Petrology and Volcano. His Geochemistry research includes elements of Arc system and Ridge. The concepts of his Basalt study are interwoven with issues in Ridge and Crust.
His study in Crust is interdisciplinary in nature, drawing from both Mineralogy, Transition zone, Mantle and Oceanic crust. In his study, which falls under the umbrella issue of Mid-ocean ridge, Mid-Atlantic Ridge is strongly linked to Oceanography. He works mostly in the field of Petrology, limiting it down to topics relating to Lava and, in certain cases, Seafloor spreading, Magma and Geophysics.
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Chemical characteristics of island-arc basalts: Implications for mantle sources
M.R. Perfit;D.A. Gust;A.E. Bence;R.J. Arculus.
Chemical Geology (1980)
Vapour undersaturation in primitive mid-ocean-ridge basalt and the volatile content of Earth's upper mantle
Alberto E. Saal;Erik H. Hauri;Charles H. Langmuir;Michael R. Perfit.
Nature (2002)
Volcanic eruption of the mid-ocean ridge along the East Pacific Rise crest at 9°45-52'N: Direct submersible observations of seafloor phenomena associated with an eruption event in April, 1991
R.M. Haymon;D.J. Fornari;K. L. Von Damm;M.D. Lilley.
Earth and Planetary Science Letters (1993)
Ambient and excess mantle temperatures, olivine thermometry, and active vs. passive upwelling
Keith D. Putirka;Michael Perfit;F.J. Ryerson;Matthew G. Jackson.
Chemical Geology (2007)
Magmatism at Mid‐Ocean Ridges: Constraints from Volcanological and Geochemical Investigations
Michael R. Perfit;William W. Chadwick.
Geophysical monograph (2013)
Experimental constraints on the generation of FeTi basalts, andesites, and rhyodacites at the Galapagos Spreading Center, 85°W and 95°W
Thomas C. Juster;Timothy L. Grove;Michael R. Perfit.
Journal of Geophysical Research (1989)
Axial summit trough of the East Pacific Rice 9°–10°N: Geological characteristics and evolution of the axial zone on fast spreading mid‐ocean ridge
Daniel J. Fornari;Rachel M. Haymon;Michael R. Perfit;Tracy K. P. Gregg.
Journal of Geophysical Research (1998)
Small-scale spatial and temporal variations in mid-ocean ridge crest magmatic processes
M. R. Perfit;D. J. Fornari;M. C. Smith;J. F. Bender.
Geology (1994)
143Nd/144Nd,87Sr/86Sr and trace element constraints on the petrogenesis of Aleutian island arc magmas
Malcolm T. McCulloch;Michael R. Perfit.
Earth and Planetary Science Letters (1981)
Chemical and isotopic constraints on the generation and transport of magma beneath the East Pacific Rise
K.W.W Sims;K.W.W Sims;S.J Goldstein;J Blichert-toft;M.R Perfit.
Geochimica et Cosmochimica Acta (2002)
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