John A. Percival mostly deals with Geochemistry, Gneiss, Archean, Mafic and Crust. Geochemistry is frequently linked to Geomorphology in his study. His biological study spans a wide range of topics, including Granulite and Terrane.
His Archean research is multidisciplinary, relying on both Metamorphism, Subduction, Rift and Craton. His work in Mafic addresses subjects such as Geochronology, which are connected to disciplines such as Ophiolite, MINTO, Sill and Block. His research integrates issues of Greenstone belt and Zircon in his study of Crust.
John A. Percival spends much of his time researching Geochemistry, Archean, Crust, Craton and Seismology. His Geochemistry study frequently links to other fields, such as Terrane. His Archean research includes elements of Suture, Pluton and Continental margin.
His studies in Crust integrate themes in fields like Precambrian and Lithosphere. His Craton research incorporates elements of Transpression, Subduction, Thermal subsidence and Tectonic zone. The various areas that John A. Percival examines in his Gneiss study include Proterozoic, Granulite and Lithology.
John A. Percival mainly investigates Geochemistry, Craton, Geochronology, Tectonic zone and Paleontology. His work on Crust as part of general Geochemistry research is frequently linked to Mineral potential, thereby connecting diverse disciplines of science. His Crust study combines topics from a wide range of disciplines, such as Natural, Precambrian and Lithosphere.
His research in Craton intersects with topics in Bedrock and Quaternary. The concepts of his Geochronology study are interwoven with issues in Orogeny and Zircon, Monazite. His work on Greenstone belt as part of general Archean study is frequently linked to Base metal, therefore connecting diverse disciplines of science.
His primary areas of investigation include Geochemistry, Geochronology, Zircon, Transect and Craton. His studies deal with areas such as Structural basin and Basement as well as Geochemistry. His Geochronology study combines topics in areas such as Greenstone belt, Archean, Metallogeny and Volcanogenic massive sulfide ore deposit.
His study in Zircon is interdisciplinary in nature, drawing from both Sedimentary depositional environment, Tectonics, Shield and Group. His Transect investigation overlaps with other disciplines such as Tectonic zone and Queen.
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Tectonic evolution of the western Superior Province from NATMAP and Lithoprobe studies
J.A. Percival;M. Sanborn-Barrie;T. Skulski;G.M. Stott.
Canadian Journal of Earth Sciences (2006)
Archean crust as revealed in the Kapuskasing uplift, Superior province, Canada
J. A. Percival;K. D. Card.
Geology (1983)
The Kapuskasing uplift: a geological and geophysical synthesis
John A. Percival;Gordon F. West.
Canadian Journal of Earth Sciences (1994)
Paleomagnetism and U-Pb geochronology of diabase dyke swarms of Minto block, Superior Province, Quebec, Canada
Kenneth L Buchan;James K Mortensen;Kenneth D Card;John A Percival.
Canadian Journal of Earth Sciences (1998)
Heat production in an Archean crustal profile and implications for heat flow and mobilization of heat-producing elements
L.D. Ashwal;P. Morgan;S.A. Kelley;J.A. Percival.
Earth and Planetary Science Letters (1987)
Late Archean Quetico accretionary complex, Superior province, Canada
John A. Percival;Howard R. Williams.
Geology (1989)
Minto block, Superior province: Missing link in deciphering assembly of the craton at 2.7 Ga
J. A. Percival;R. A. Stern;T. Skulski;K. D. Card.
Geology (1994)
A Mainly Crustal Origin for Tonalitic Granitoid Rocks, Superior Province, Canada: Implications for Late Archean Tectonomagmatic Processes
Joseph B. Whalen;John A. Percival;Vicki J. McNICOLL;Frederick J. Longstaffe.
Journal of Petrology (2002)
A regional perspective of the Quetico metasedimentary belt, Superior Province, Canada
John A. Percival.
Canadian Journal of Earth Sciences (1989)
High-grade metamorphism in the Chapleau-Foleyet area, Ontario
John A. Percival.
American Mineralogist (1983)
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