The Experts below are selected from a list of 327 Experts worldwide ranked by ideXlab platform
Yoshinobu, Aaron S - One of the best experts on this subject based on the ideXlab platform.
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Ordovician and Silurian Magmatism in the Upper Nappe, Uppermost Allochthon, Helgeland Nappe Complex, North-Central Norway
Geological Society Norway, 2016Co-Authors: Barnes, Calvin G., Reid Kristin, Frost, Carol D., Barnes Melanie, Allen, Charlotte M, Yoshinobu, Aaron SAbstract:The structurally lowest parts of the Upper Nappe of the Helgeland Nappe Complex consist primarily of migmatitic quartzofeldspathic Gneiss with intercalated calc-silicate Gneiss. Detrital zircons in the Gneiss indicate an Ordovician depositional age. Migmatization via biotite dehydration reactions occurred at ~480 Ma at pressures of ~700 MPa; some migmatites were mobilized into cross-cutting diatexites. Diverse gabbroic to granitic plutons and dikes of the Bindal Batholith were emplaced from 448-424 Ma. They range from calc-alkaline to alkalic and most have initial 87Sr/86Sr
Barnes, Calvin G. - One of the best experts on this subject based on the ideXlab platform.
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Ordovician and Silurian Magmatism in the Upper Nappe, Uppermost Allochthon, Helgeland Nappe Complex, North-Central Norway
Geological Society Norway, 2016Co-Authors: Barnes, Calvin G., Reid Kristin, Frost, Carol D., Barnes Melanie, Allen, Charlotte M, Yoshinobu, Aaron SAbstract:The structurally lowest parts of the Upper Nappe of the Helgeland Nappe Complex consist primarily of migmatitic quartzofeldspathic Gneiss with intercalated calc-silicate Gneiss. Detrital zircons in the Gneiss indicate an Ordovician depositional age. Migmatization via biotite dehydration reactions occurred at ~480 Ma at pressures of ~700 MPa; some migmatites were mobilized into cross-cutting diatexites. Diverse gabbroic to granitic plutons and dikes of the Bindal Batholith were emplaced from 448-424 Ma. They range from calc-alkaline to alkalic and most have initial 87Sr/86Sr
Barnes Melanie - One of the best experts on this subject based on the ideXlab platform.
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Ordovician and Silurian Magmatism in the Upper Nappe, Uppermost Allochthon, Helgeland Nappe Complex, North-Central Norway
Geological Society Norway, 2016Co-Authors: Barnes, Calvin G., Reid Kristin, Frost, Carol D., Barnes Melanie, Allen, Charlotte M, Yoshinobu, Aaron SAbstract:The structurally lowest parts of the Upper Nappe of the Helgeland Nappe Complex consist primarily of migmatitic quartzofeldspathic Gneiss with intercalated calc-silicate Gneiss. Detrital zircons in the Gneiss indicate an Ordovician depositional age. Migmatization via biotite dehydration reactions occurred at ~480 Ma at pressures of ~700 MPa; some migmatites were mobilized into cross-cutting diatexites. Diverse gabbroic to granitic plutons and dikes of the Bindal Batholith were emplaced from 448-424 Ma. They range from calc-alkaline to alkalic and most have initial 87Sr/86Sr
Reid Kristin - One of the best experts on this subject based on the ideXlab platform.
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Ordovician and Silurian Magmatism in the Upper Nappe, Uppermost Allochthon, Helgeland Nappe Complex, North-Central Norway
Geological Society Norway, 2016Co-Authors: Barnes, Calvin G., Reid Kristin, Frost, Carol D., Barnes Melanie, Allen, Charlotte M, Yoshinobu, Aaron SAbstract:The structurally lowest parts of the Upper Nappe of the Helgeland Nappe Complex consist primarily of migmatitic quartzofeldspathic Gneiss with intercalated calc-silicate Gneiss. Detrital zircons in the Gneiss indicate an Ordovician depositional age. Migmatization via biotite dehydration reactions occurred at ~480 Ma at pressures of ~700 MPa; some migmatites were mobilized into cross-cutting diatexites. Diverse gabbroic to granitic plutons and dikes of the Bindal Batholith were emplaced from 448-424 Ma. They range from calc-alkaline to alkalic and most have initial 87Sr/86Sr
Frost, Carol D. - One of the best experts on this subject based on the ideXlab platform.
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Ordovician and Silurian Magmatism in the Upper Nappe, Uppermost Allochthon, Helgeland Nappe Complex, North-Central Norway
Geological Society Norway, 2016Co-Authors: Barnes, Calvin G., Reid Kristin, Frost, Carol D., Barnes Melanie, Allen, Charlotte M, Yoshinobu, Aaron SAbstract:The structurally lowest parts of the Upper Nappe of the Helgeland Nappe Complex consist primarily of migmatitic quartzofeldspathic Gneiss with intercalated calc-silicate Gneiss. Detrital zircons in the Gneiss indicate an Ordovician depositional age. Migmatization via biotite dehydration reactions occurred at ~480 Ma at pressures of ~700 MPa; some migmatites were mobilized into cross-cutting diatexites. Diverse gabbroic to granitic plutons and dikes of the Bindal Batholith were emplaced from 448-424 Ma. They range from calc-alkaline to alkalic and most have initial 87Sr/86Sr