Stefano Mancuso: Mantle Plumes : A Multidisciplinary Approach - neues Buch
ISBN: 9783540680468
The concept of mantle plumes, originally suggested by Morgan (1971), is widely but not unequivocally accepted as the cause for hotspot volcanism.Plumes are thought of as deep-rooted, appr… Mehr…
The concept of mantle plumes, originally suggested by Morgan (1971), is widely but not unequivocally accepted as the cause for hotspot volcanism.Plumes are thought of as deep-rooted, approximately cylindrical regions of hot rising mantle rock with a typical diameter of 100-200 km.Pressure-release melting near the b- tom of the lithosphere produces magmas that rise to the surface and lead, when the plate moves relative to the plume, to a chain of volcanic edifices whose age p- gresses with increasing distance from the plume.For a long time, the evidence for mantle plumes has been largely circumstantial.Laboratory and computer models of mantle convection show that under certain conditions plume-like structures can be found, and these simulations have been used to characterise their properties.Geodetic signals, such as topographic swells and associated geoid anomalies which surround the volcanic hotspots, support the plume hypothesis.They are best identified in an oceanic environment where the plume signal is usually less s- ceptible to be masked by effects of crustal or lithospheric heterogeneities.The i- topic and trace element composition of hotspot lavas differs from those of m- oceanic ridge basalts which is interpreted as indication for a source reservoir d- ferent from average upper mantle rock.The idea of mantle plumes has gained widespread popularity in various disciplines of Earth science and has been used, sometimes perhaps excessively, to explain volcanic and other phenomena.; PDF; Scientific, Technical and Medical > Physics > Applied physics > Geophysics, Springer Berlin Heidelberg<
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Clark A. Rosen: Mantle Plumes : A Multidisciplinary Approach - neues Buch
ISBN: 9783540680468
The concept of mantle plumes, originally suggested by Morgan (1971), is widely but not unequivocally accepted as the cause for hotspot volcanism.Plumes are thought of as deep-rooted, appr… Mehr…
The concept of mantle plumes, originally suggested by Morgan (1971), is widely but not unequivocally accepted as the cause for hotspot volcanism.Plumes are thought of as deep-rooted, approximately cylindrical regions of hot rising mantle rock with a typical diameter of 100-200 km.Pressure-release melting near the b- tom of the lithosphere produces magmas that rise to the surface and lead, when the plate moves relative to the plume, to a chain of volcanic edifices whose age p- gresses with increasing distance from the plume.For a long time, the evidence for mantle plumes has been largely circumstantial.Laboratory and computer models of mantle convection show that under certain conditions plume-like structures can be found, and these simulations have been used to characterise their properties.Geodetic signals, such as topographic swells and associated geoid anomalies which surround the volcanic hotspots, support the plume hypothesis.They are best identified in an oceanic environment where the plume signal is usually less s- ceptible to be masked by effects of crustal or lithospheric heterogeneities.The i- topic and trace element composition of hotspot lavas differs from those of m- oceanic ridge basalts which is interpreted as indication for a source reservoir d- ferent from average upper mantle rock.The idea of mantle plumes has gained widespread popularity in various disciplines of Earth science and has been used, sometimes perhaps excessively, to explain volcanic and other phenomena.; PDF; Scientific, Technical and Medical > Physics > Applied physics > Geophysics, Springer Berlin Heidelberg<
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No. 9783540680468. Versandkosten:Instock, Despatched same working day before 3pm, zzgl. Versandkosten. Details...
(*) Derzeit vergriffen bedeutet, dass dieser Titel momentan auf keiner der angeschlossenen Plattform verfügbar ist.
The concept of mantle plumes, originally suggested by Morgan (1971), is widely but not unequivocally accepted as the cause for hotspot volcanism. Plumes are thought of as deep-rooted, app… Mehr…
The concept of mantle plumes, originally suggested by Morgan (1971), is widely but not unequivocally accepted as the cause for hotspot volcanism. Plumes are thought of as deep-rooted, approximately cylindrical regions of hot rising mantle rock with a typical diameter of 100-200 km. Pressure-release melting near the b- tom of the lithosphere produces magmas that rise to the surface and lead, when the plate moves relative to the plume, to a chain of volcanic edifices whose age p- gresses with increasing distance from the plume. For a long time, the evidence for mantle plumes has been largely circumstantial. Laboratory and computer models of mantle convection show that under certain conditions plume-like structures can be found, and these simulations have been used to characterise their properties. Geodetic signals, such as topographic swells and associated geoid anomalies which surround the volcanic hotspots, support the plume hypothesis. They are best identified in an oceanic environment where the plume signal is usually less s- ceptible to be masked by effects of crustal or lithospheric heterogeneities. The i- topic and trace element composition of hotspot lavas differs from those of m- oceanic ridge basalts which is interpreted as indication for a source reservoir d- ferent from average upper mantle rock. The idea of mantle plumes has gained widespread popularity in various disciplines of Earth science and has been used, sometimes perhaps excessively, to explain volcanic and other phenomena., Springer<
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The concept of mantle plumes is a key to understanding intraplate volcanism in the framework of modern plate tectonics. Recent progress in instrumental, analytical and satellite technolog… Mehr…
The concept of mantle plumes is a key to understanding intraplate volcanism in the framework of modern plate tectonics. Recent progress in instrumental, analytical and satellite technology enables scientists to verify the plume hypothesis with seismic tomography, isotope geochemistry and other sophisticated techniques. In this book, a group of experts review these advances in plume research and present a general overview on recent plume studies. eBooks > Fremdsprachige eBooks > Englische eBooks > Sach- & Fachthemen > Chemie; eBooks > Fachbücher > Geowissenschaften; eBooks > Fachbücher > Physik & Astronomie; eBooks > Fremdsprachige eBooks > Englische eBooks > Sach- & Fachthemen > Physik; eBooks > , Springer, Springer<
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Mantle Plumes : A Multidisciplinary Approach - neues Buch
ISBN: 9783540680468
The concept of mantle plumes, originally suggested by Morgan (1971), is widely but not unequivocally accepted as the cause for hotspot volcanism.Plumes are thought of as deep-rooted, appr… Mehr…
The concept of mantle plumes, originally suggested by Morgan (1971), is widely but not unequivocally accepted as the cause for hotspot volcanism.Plumes are thought of as deep-rooted, approximately cylindrical regions of hot rising mantle rock with a typical diameter of 100-200 km.Pressure-release melting near the b- tom of the lithosphere produces magmas that rise to the surface and lead, when the plate moves relative to the plume, to a chain of volcanic edifices whose age p- gresses with increasing distance from the plume.For a long time, the evidence for mantle plumes has been largely circumstantial.Laboratory and computer models of mantle convection show that under certain conditions plume-like structures can be found, and these simulations have been used to characterise their properties.Geodetic signals, such as topographic swells and associated geoid anomalies which surround the volcanic hotspots, support the plume hypothesis.They are best identified in an oceanic environment where the plume signal is usually less s- ceptible to be masked by effects of crustal or lithospheric heterogeneities.The i- topic and trace element composition of hotspot lavas differs from those of m- oceanic ridge basalts which is interpreted as indication for a source reservoir d- ferent from average upper mantle rock.The idea of mantle plumes has gained widespread popularity in various disciplines of Earth science and has been used, sometimes perhaps excessively, to explain volcanic and other phenomena.; PDF; Scientific, Technical and Medical > Physics > Applied physics > Geophysics, Springer Berlin Heidelberg<
No. 9783540680468. Versandkosten:Instock, Despatched same working day before 3pm, zzgl. Versandkosten.
Mantle Plumes : A Multidisciplinary Approach - neues Buch
ISBN: 9783540680468
The concept of mantle plumes, originally suggested by Morgan (1971), is widely but not unequivocally accepted as the cause for hotspot volcanism.Plumes are thought of as deep-rooted, appr… Mehr…
The concept of mantle plumes, originally suggested by Morgan (1971), is widely but not unequivocally accepted as the cause for hotspot volcanism.Plumes are thought of as deep-rooted, approximately cylindrical regions of hot rising mantle rock with a typical diameter of 100-200 km.Pressure-release melting near the b- tom of the lithosphere produces magmas that rise to the surface and lead, when the plate moves relative to the plume, to a chain of volcanic edifices whose age p- gresses with increasing distance from the plume.For a long time, the evidence for mantle plumes has been largely circumstantial.Laboratory and computer models of mantle convection show that under certain conditions plume-like structures can be found, and these simulations have been used to characterise their properties.Geodetic signals, such as topographic swells and associated geoid anomalies which surround the volcanic hotspots, support the plume hypothesis.They are best identified in an oceanic environment where the plume signal is usually less s- ceptible to be masked by effects of crustal or lithospheric heterogeneities.The i- topic and trace element composition of hotspot lavas differs from those of m- oceanic ridge basalts which is interpreted as indication for a source reservoir d- ferent from average upper mantle rock.The idea of mantle plumes has gained widespread popularity in various disciplines of Earth science and has been used, sometimes perhaps excessively, to explain volcanic and other phenomena.; PDF; Scientific, Technical and Medical > Physics > Applied physics > Geophysics, Springer Berlin Heidelberg<
No. 9783540680468. Versandkosten:Instock, Despatched same working day before 3pm, zzgl. Versandkosten.
The concept of mantle plumes, originally suggested by Morgan (1971), is widely but not unequivocally accepted as the cause for hotspot volcanism. Plumes are thought of as deep-rooted, app… Mehr…
The concept of mantle plumes, originally suggested by Morgan (1971), is widely but not unequivocally accepted as the cause for hotspot volcanism. Plumes are thought of as deep-rooted, approximately cylindrical regions of hot rising mantle rock with a typical diameter of 100-200 km. Pressure-release melting near the b- tom of the lithosphere produces magmas that rise to the surface and lead, when the plate moves relative to the plume, to a chain of volcanic edifices whose age p- gresses with increasing distance from the plume. For a long time, the evidence for mantle plumes has been largely circumstantial. Laboratory and computer models of mantle convection show that under certain conditions plume-like structures can be found, and these simulations have been used to characterise their properties. Geodetic signals, such as topographic swells and associated geoid anomalies which surround the volcanic hotspots, support the plume hypothesis. They are best identified in an oceanic environment where the plume signal is usually less s- ceptible to be masked by effects of crustal or lithospheric heterogeneities. The i- topic and trace element composition of hotspot lavas differs from those of m- oceanic ridge basalts which is interpreted as indication for a source reservoir d- ferent from average upper mantle rock. The idea of mantle plumes has gained widespread popularity in various disciplines of Earth science and has been used, sometimes perhaps excessively, to explain volcanic and other phenomena., Springer<
Nr. 978-3-540-68046-8. Versandkosten:Worldwide free shipping, , DE. (EUR 0.00)
The concept of mantle plumes is a key to understanding intraplate volcanism in the framework of modern plate tectonics. Recent progress in instrumental, analytical and satellite technolog… Mehr…
The concept of mantle plumes is a key to understanding intraplate volcanism in the framework of modern plate tectonics. Recent progress in instrumental, analytical and satellite technology enables scientists to verify the plume hypothesis with seismic tomography, isotope geochemistry and other sophisticated techniques. In this book, a group of experts review these advances in plume research and present a general overview on recent plume studies. eBooks > Fremdsprachige eBooks > Englische eBooks > Sach- & Fachthemen > Chemie; eBooks > Fachbücher > Geowissenschaften; eBooks > Fachbücher > Physik & Astronomie; eBooks > Fremdsprachige eBooks > Englische eBooks > Sach- & Fachthemen > Physik; eBooks > , Springer, Springer<
Nr. A1031487384. Versandkosten:Lieferzeiten außerhalb der Schweiz 3 bis 21 Werktage, , Sofort per Download lieferbar, zzgl. Versandkosten. (EUR 17.51)
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Buch in der Datenbank seit 2009-07-29T15:28:14+02:00 (Vienna) Detailseite zuletzt geändert am 2024-01-25T14:15:47+01:00 (Vienna) ISBN/EAN: 9783540680468
ISBN - alternative Schreibweisen: 3-540-68046-2, 978-3-540-68046-8 Alternative Schreibweisen und verwandte Suchbegriffe: Autor des Buches: joachim ritter, christensen, takahashi, stefano mancuso Titel des Buches: plume
Daten vom Verlag:
Autor/in: Joachim R. R. Ritter; U.R. Christensen Titel: Mantle Plumes - A Multidisciplinary Approach Verlag: Springer; Springer Berlin 502 Seiten Erscheinungsjahr: 2007-04-27 Berlin; Heidelberg; DE Gedruckt / Hergestellt in Deutschland. Sprache: Englisch 213,99 € (DE) 220,00 € (AT) 236,00 CHF (CH) Available VIII, 502 p. 157 illus., 31 illus. in color.
EA; E107; eBook; Nonbooks, PBS / Geowissenschaften/Geologie; Geophysik; Verstehen; Geodynamics; Volcanism; geochemistry; plate tectonics; satellite; C; Geophysics/Geodesy; Inorganic Chemistry; Geology; Theoretical, Mathematical and Computational Physics; Geophysics; Inorganic Chemistry; Geology; Theoretical, Mathematical and Computational Physics; Earth and Environmental Science; Anorganische Chemie; Geologie und die Lithosphäre; Mathematische Physik; BB
Basic Properties of Mantle Plumes.- Fluid Dynamics of Mantle Plumes.- Case studies.- Tracing the Hawaiian Mantle Plume by Converted Seismic Waves.- Iceland: The current picture of a ridge-centred mantle plume.- Combined Gas-geochemical and Receiver Function Studies of the Vogtland/NW Bohemia Intraplate Mantle Degassing Field, Central Europe.- Crustal and Upper Mantle Structure of the French Massif Central Plume.- Eifel Region.- Geodynamic Setting of the Tertiary Hocheifel Volcanism (Germany), Part I: 40Ar/39Ar geochronology.- Geodynamic Setting of the Tertiary Hocheifel Volcanism (Germany), Part II: Geochemistry and Sr, Nd and Pb Isotopic Compositions.- The Quaternary Volcanic Fields of the East and West Eifel (Germany).- Thermal and Geochemical Evolution of the Shallow Subcontinental Lithospheric Mantle Beneath the Eifel: Constraints from Mantle Xenoliths, a Review.- He-Ne-Ar Isotope Systematics of Eifel and Pannonian Basin Mantle Xenoliths Trace Deep Mantle Plume-Lithosphere Interaction Beneath the European Continent.- Quaternary Uplift in the Eifel Area.- The Seismic Signature of the Eifel Plume.- Upper Mantle Structure Beneath the Eifel from Receiver Functions.- Rayleigh Wave Dispersion in the Eifel Region.- Seismic Anisotropy in the Asthenosphere Beneath the Eifel Region, Western Germany.- Gravity Observations in the Western Rhenish Massif and Forward Modelling of the Eifel Plume Bouguer Anomaly.
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