Plate tectonics and magma genesis

Abstract The framework of plate tectonics, with active boundaries and stable plates, is the best yet devised for explaining the different types and styles of magmatic activity. The dynamic mechanisms of plate tectonics transport rock masses across fusion boundaries in three distinct types of environ...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Wyllie, P. J. [verfasserIn]

Format:	Artikel
Sprache:	Englisch

Erschienen:	1981

Schlagwörter:	Continental Crust Continental Margin Oceanic Crust Mantle Plume Plate Tectonic

Anmerkung:	© Ferdinand Enke Verlag Stuttgart 1981

Übergeordnetes Werk:	Enthalten in: Geologische Rundschau - Springer-Verlag, 1910, 70(1981), 1 vom: Feb., Seite 128-153
Übergeordnetes Werk:	volume:70 ; year:1981 ; number:1 ; month:02 ; pages:128-153

Links:	Volltext

DOI / URN:	10.1007/BF01764318

Katalog-ID:	OLC2070401278

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allfields	10.1007/BF01764318 doi (DE-627)OLC2070401278 (DE-He213)BF01764318-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Wyllie, P. J. verfasserin aut Plate tectonics and magma genesis 1981 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Ferdinand Enke Verlag Stuttgart 1981 Abstract The framework of plate tectonics, with active boundaries and stable plates, is the best yet devised for explaining the different types and styles of magmatic activity. The dynamic mechanisms of plate tectonics transport rock masses across fusion boundaries in three distinct types of environment and source material, associated with plate boundaries. These are divergent boundaries where mantle peridotite is transported upwards, melting to yield basalt, convergent boundaries where oceanic crust is transported downwards, melting to yield magma of intermediate $ SiO_{2} $ content, and ocean-continent convergent boundaries where the lower part of continental margins are melted to yield rhyolite magma. Hot spots beneath plates, possibly generated by mantle plumes, yield basaltic magma from mantle and rhyolite magma from overlying continental crust. Subducted $ H_{2} $O is involved in the generation of andesites and batholiths, and $ CO_{2} $ from uncertain sources is an influential component for the generation of kimberlite and other low $ SiO_{2} $, high alkali magmas below continental plates. The chemical differentiation of the earth is accomplished through magmatic processes which are a direct manifestation of convection within the mantle. Igneous petrology is now a study of processes and products firmly rooted in geophysics, and calibrated by laboratory experiments at high pressures and temperatures. Continental Crust Continental Margin Oceanic Crust Mantle Plume Plate Tectonic Enthalten in Geologische Rundschau Springer-Verlag, 1910 70(1981), 1 vom: Feb., Seite 128-153 (DE-627)129489441 (DE-600)205883-2 (DE-576)014883015 0016-7835 nnns volume:70 year:1981 number:1 month:02 pages:128-153 https://doi.org/10.1007/BF01764318 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_70 GBV_ILN_120 GBV_ILN_121 GBV_ILN_130 GBV_ILN_131 GBV_ILN_156 GBV_ILN_171 GBV_ILN_183 GBV_ILN_188 GBV_ILN_285 GBV_ILN_601 GBV_ILN_788 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_2057 GBV_ILN_2173 GBV_ILN_2315 GBV_ILN_2399 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4321 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4337 GBV_ILN_4700 AR 70 1981 1 02 128-153
spelling	10.1007/BF01764318 doi (DE-627)OLC2070401278 (DE-He213)BF01764318-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Wyllie, P. J. verfasserin aut Plate tectonics and magma genesis 1981 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Ferdinand Enke Verlag Stuttgart 1981 Abstract The framework of plate tectonics, with active boundaries and stable plates, is the best yet devised for explaining the different types and styles of magmatic activity. The dynamic mechanisms of plate tectonics transport rock masses across fusion boundaries in three distinct types of environment and source material, associated with plate boundaries. These are divergent boundaries where mantle peridotite is transported upwards, melting to yield basalt, convergent boundaries where oceanic crust is transported downwards, melting to yield magma of intermediate $ SiO_{2} $ content, and ocean-continent convergent boundaries where the lower part of continental margins are melted to yield rhyolite magma. Hot spots beneath plates, possibly generated by mantle plumes, yield basaltic magma from mantle and rhyolite magma from overlying continental crust. Subducted $ H_{2} $O is involved in the generation of andesites and batholiths, and $ CO_{2} $ from uncertain sources is an influential component for the generation of kimberlite and other low $ SiO_{2} $, high alkali magmas below continental plates. The chemical differentiation of the earth is accomplished through magmatic processes which are a direct manifestation of convection within the mantle. Igneous petrology is now a study of processes and products firmly rooted in geophysics, and calibrated by laboratory experiments at high pressures and temperatures. Continental Crust Continental Margin Oceanic Crust Mantle Plume Plate Tectonic Enthalten in Geologische Rundschau Springer-Verlag, 1910 70(1981), 1 vom: Feb., Seite 128-153 (DE-627)129489441 (DE-600)205883-2 (DE-576)014883015 0016-7835 nnns volume:70 year:1981 number:1 month:02 pages:128-153 https://doi.org/10.1007/BF01764318 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_70 GBV_ILN_120 GBV_ILN_121 GBV_ILN_130 GBV_ILN_131 GBV_ILN_156 GBV_ILN_171 GBV_ILN_183 GBV_ILN_188 GBV_ILN_285 GBV_ILN_601 GBV_ILN_788 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_2057 GBV_ILN_2173 GBV_ILN_2315 GBV_ILN_2399 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4321 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4337 GBV_ILN_4700 AR 70 1981 1 02 128-153
allfields_unstemmed	10.1007/BF01764318 doi (DE-627)OLC2070401278 (DE-He213)BF01764318-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Wyllie, P. J. verfasserin aut Plate tectonics and magma genesis 1981 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Ferdinand Enke Verlag Stuttgart 1981 Abstract The framework of plate tectonics, with active boundaries and stable plates, is the best yet devised for explaining the different types and styles of magmatic activity. The dynamic mechanisms of plate tectonics transport rock masses across fusion boundaries in three distinct types of environment and source material, associated with plate boundaries. These are divergent boundaries where mantle peridotite is transported upwards, melting to yield basalt, convergent boundaries where oceanic crust is transported downwards, melting to yield magma of intermediate $ SiO_{2} $ content, and ocean-continent convergent boundaries where the lower part of continental margins are melted to yield rhyolite magma. Hot spots beneath plates, possibly generated by mantle plumes, yield basaltic magma from mantle and rhyolite magma from overlying continental crust. Subducted $ H_{2} $O is involved in the generation of andesites and batholiths, and $ CO_{2} $ from uncertain sources is an influential component for the generation of kimberlite and other low $ SiO_{2} $, high alkali magmas below continental plates. The chemical differentiation of the earth is accomplished through magmatic processes which are a direct manifestation of convection within the mantle. Igneous petrology is now a study of processes and products firmly rooted in geophysics, and calibrated by laboratory experiments at high pressures and temperatures. Continental Crust Continental Margin Oceanic Crust Mantle Plume Plate Tectonic Enthalten in Geologische Rundschau Springer-Verlag, 1910 70(1981), 1 vom: Feb., Seite 128-153 (DE-627)129489441 (DE-600)205883-2 (DE-576)014883015 0016-7835 nnns volume:70 year:1981 number:1 month:02 pages:128-153 https://doi.org/10.1007/BF01764318 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_70 GBV_ILN_120 GBV_ILN_121 GBV_ILN_130 GBV_ILN_131 GBV_ILN_156 GBV_ILN_171 GBV_ILN_183 GBV_ILN_188 GBV_ILN_285 GBV_ILN_601 GBV_ILN_788 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_2057 GBV_ILN_2173 GBV_ILN_2315 GBV_ILN_2399 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4321 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4337 GBV_ILN_4700 AR 70 1981 1 02 128-153
allfieldsGer	10.1007/BF01764318 doi (DE-627)OLC2070401278 (DE-He213)BF01764318-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Wyllie, P. J. verfasserin aut Plate tectonics and magma genesis 1981 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Ferdinand Enke Verlag Stuttgart 1981 Abstract The framework of plate tectonics, with active boundaries and stable plates, is the best yet devised for explaining the different types and styles of magmatic activity. The dynamic mechanisms of plate tectonics transport rock masses across fusion boundaries in three distinct types of environment and source material, associated with plate boundaries. These are divergent boundaries where mantle peridotite is transported upwards, melting to yield basalt, convergent boundaries where oceanic crust is transported downwards, melting to yield magma of intermediate $ SiO_{2} $ content, and ocean-continent convergent boundaries where the lower part of continental margins are melted to yield rhyolite magma. Hot spots beneath plates, possibly generated by mantle plumes, yield basaltic magma from mantle and rhyolite magma from overlying continental crust. Subducted $ H_{2} $O is involved in the generation of andesites and batholiths, and $ CO_{2} $ from uncertain sources is an influential component for the generation of kimberlite and other low $ SiO_{2} $, high alkali magmas below continental plates. The chemical differentiation of the earth is accomplished through magmatic processes which are a direct manifestation of convection within the mantle. Igneous petrology is now a study of processes and products firmly rooted in geophysics, and calibrated by laboratory experiments at high pressures and temperatures. Continental Crust Continental Margin Oceanic Crust Mantle Plume Plate Tectonic Enthalten in Geologische Rundschau Springer-Verlag, 1910 70(1981), 1 vom: Feb., Seite 128-153 (DE-627)129489441 (DE-600)205883-2 (DE-576)014883015 0016-7835 nnns volume:70 year:1981 number:1 month:02 pages:128-153 https://doi.org/10.1007/BF01764318 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_70 GBV_ILN_120 GBV_ILN_121 GBV_ILN_130 GBV_ILN_131 GBV_ILN_156 GBV_ILN_171 GBV_ILN_183 GBV_ILN_188 GBV_ILN_285 GBV_ILN_601 GBV_ILN_788 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_2057 GBV_ILN_2173 GBV_ILN_2315 GBV_ILN_2399 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4321 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4337 GBV_ILN_4700 AR 70 1981 1 02 128-153
allfieldsSound	10.1007/BF01764318 doi (DE-627)OLC2070401278 (DE-He213)BF01764318-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn Wyllie, P. J. verfasserin aut Plate tectonics and magma genesis 1981 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Ferdinand Enke Verlag Stuttgart 1981 Abstract The framework of plate tectonics, with active boundaries and stable plates, is the best yet devised for explaining the different types and styles of magmatic activity. The dynamic mechanisms of plate tectonics transport rock masses across fusion boundaries in three distinct types of environment and source material, associated with plate boundaries. These are divergent boundaries where mantle peridotite is transported upwards, melting to yield basalt, convergent boundaries where oceanic crust is transported downwards, melting to yield magma of intermediate $ SiO_{2} $ content, and ocean-continent convergent boundaries where the lower part of continental margins are melted to yield rhyolite magma. Hot spots beneath plates, possibly generated by mantle plumes, yield basaltic magma from mantle and rhyolite magma from overlying continental crust. Subducted $ H_{2} $O is involved in the generation of andesites and batholiths, and $ CO_{2} $ from uncertain sources is an influential component for the generation of kimberlite and other low $ SiO_{2} $, high alkali magmas below continental plates. The chemical differentiation of the earth is accomplished through magmatic processes which are a direct manifestation of convection within the mantle. Igneous petrology is now a study of processes and products firmly rooted in geophysics, and calibrated by laboratory experiments at high pressures and temperatures. Continental Crust Continental Margin Oceanic Crust Mantle Plume Plate Tectonic Enthalten in Geologische Rundschau Springer-Verlag, 1910 70(1981), 1 vom: Feb., Seite 128-153 (DE-627)129489441 (DE-600)205883-2 (DE-576)014883015 0016-7835 nnns volume:70 year:1981 number:1 month:02 pages:128-153 https://doi.org/10.1007/BF01764318 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_70 GBV_ILN_120 GBV_ILN_121 GBV_ILN_130 GBV_ILN_131 GBV_ILN_156 GBV_ILN_171 GBV_ILN_183 GBV_ILN_188 GBV_ILN_285 GBV_ILN_601 GBV_ILN_788 GBV_ILN_2002 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_2057 GBV_ILN_2173 GBV_ILN_2315 GBV_ILN_2399 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4251 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4309 GBV_ILN_4311 GBV_ILN_4313 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4321 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4337 GBV_ILN_4700 AR 70 1981 1 02 128-153
language	English
source	Enthalten in Geologische Rundschau 70(1981), 1 vom: Feb., Seite 128-153 volume:70 year:1981 number:1 month:02 pages:128-153
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topic_facet	Continental Crust Continental Margin Oceanic Crust Mantle Plume Plate Tectonic
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author	Wyllie, P. J.
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title	Plate tectonics and magma genesis
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title_sort	plate tectonics and magma genesis
title_auth	Plate tectonics and magma genesis
abstract	Abstract The framework of plate tectonics, with active boundaries and stable plates, is the best yet devised for explaining the different types and styles of magmatic activity. The dynamic mechanisms of plate tectonics transport rock masses across fusion boundaries in three distinct types of environment and source material, associated with plate boundaries. These are divergent boundaries where mantle peridotite is transported upwards, melting to yield basalt, convergent boundaries where oceanic crust is transported downwards, melting to yield magma of intermediate $ SiO_{2} $ content, and ocean-continent convergent boundaries where the lower part of continental margins are melted to yield rhyolite magma. Hot spots beneath plates, possibly generated by mantle plumes, yield basaltic magma from mantle and rhyolite magma from overlying continental crust. Subducted $ H_{2} $O is involved in the generation of andesites and batholiths, and $ CO_{2} $ from uncertain sources is an influential component for the generation of kimberlite and other low $ SiO_{2} $, high alkali magmas below continental plates. The chemical differentiation of the earth is accomplished through magmatic processes which are a direct manifestation of convection within the mantle. Igneous petrology is now a study of processes and products firmly rooted in geophysics, and calibrated by laboratory experiments at high pressures and temperatures. © Ferdinand Enke Verlag Stuttgart 1981
abstractGer	Abstract The framework of plate tectonics, with active boundaries and stable plates, is the best yet devised for explaining the different types and styles of magmatic activity. The dynamic mechanisms of plate tectonics transport rock masses across fusion boundaries in three distinct types of environment and source material, associated with plate boundaries. These are divergent boundaries where mantle peridotite is transported upwards, melting to yield basalt, convergent boundaries where oceanic crust is transported downwards, melting to yield magma of intermediate $ SiO_{2} $ content, and ocean-continent convergent boundaries where the lower part of continental margins are melted to yield rhyolite magma. Hot spots beneath plates, possibly generated by mantle plumes, yield basaltic magma from mantle and rhyolite magma from overlying continental crust. Subducted $ H_{2} $O is involved in the generation of andesites and batholiths, and $ CO_{2} $ from uncertain sources is an influential component for the generation of kimberlite and other low $ SiO_{2} $, high alkali magmas below continental plates. The chemical differentiation of the earth is accomplished through magmatic processes which are a direct manifestation of convection within the mantle. Igneous petrology is now a study of processes and products firmly rooted in geophysics, and calibrated by laboratory experiments at high pressures and temperatures. © Ferdinand Enke Verlag Stuttgart 1981
abstract_unstemmed	Abstract The framework of plate tectonics, with active boundaries and stable plates, is the best yet devised for explaining the different types and styles of magmatic activity. The dynamic mechanisms of plate tectonics transport rock masses across fusion boundaries in three distinct types of environment and source material, associated with plate boundaries. These are divergent boundaries where mantle peridotite is transported upwards, melting to yield basalt, convergent boundaries where oceanic crust is transported downwards, melting to yield magma of intermediate $ SiO_{2} $ content, and ocean-continent convergent boundaries where the lower part of continental margins are melted to yield rhyolite magma. Hot spots beneath plates, possibly generated by mantle plumes, yield basaltic magma from mantle and rhyolite magma from overlying continental crust. Subducted $ H_{2} $O is involved in the generation of andesites and batholiths, and $ CO_{2} $ from uncertain sources is an influential component for the generation of kimberlite and other low $ SiO_{2} $, high alkali magmas below continental plates. The chemical differentiation of the earth is accomplished through magmatic processes which are a direct manifestation of convection within the mantle. Igneous petrology is now a study of processes and products firmly rooted in geophysics, and calibrated by laboratory experiments at high pressures and temperatures. © Ferdinand Enke Verlag Stuttgart 1981
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