Theoretical Mantle Dynamics [PDF]
Geodynamics is the study of the deformation and flow of the solid Earth and other planetary interiors. Focusing on the Earth's mantle, this book provides a comprehensive, mathematically advanced treatment of the continuum mechanics of mantle processes and the craft of formulating geodynamical models to approximate them.
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On November 20 and 21, 1984, the Geophysical Laboratory and the Department of Terrestrial Magnetism of the Carnegie Institution sponsored a workshop on the structure and dynamics of the mantle. The participants represented several academic institutions and a wide range of disciplines within the earth and planetary sciences.
Paul G. Silver +3 more
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Global observations of reflectors in the mid-mantle with implications for mantle structure and dynamics [PDF]
AbstractSeismic tomography indicates that flow is commonly deflected in the mid-mantle. However, without a candidate mineral phase change, causative mechanisms remain controversial. Deflection of flow has been linked to radial changes in viscosity and/or composition, but a lack of global observations precludes comprehensive tests by seismically ...
Lauren Waszek +2 more
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Mantle flow through a tear in the Nazca slab inferred from shear wave splitting
A tear in the subducting Nazca slab is located between the end of the Pampean flat slab and normally subducting oceanic lithosphere. Tomographic studies suggest mantle material flows through this opening.
Colton Lynner +4 more
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Multi‐Layer Seismic Anisotropy Beneath Greenland
Seismic anisotropy provides insight into past episodes of lithospheric deformation and the orientations of strain in the underlying asthenosphere. The Greenland mantle has played host to a rich history of tectonic processes, including multiple orogenies ...
Erica M. Nathan +3 more
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Pressure‐Induced sp 2 ‐sp 3 Transitions in Carbon‐Bearing Phases
This book is Open Access. A digital copy can be downloaded for free from Wiley Online Library.
Explores the behavior of carbon in minerals, melts, and fluids under extreme conditions
Carbon trapped in diamonds and carbonate-bearing rocks in subduction zones are examples of the continuing exchange of substantial carbon ...
Sergey S. Lobanov +1 more
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Ultralow velocity zones (ULVZs) and seismic anisotropy are both commonly detected in the lowermost mantle at the edges of the two antipodal large low velocity provinces (LLVPs).
Jonathan Wolf, Maureen D. Long
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Geochemical and geophysical observations for large-scale structures in the Earth’s interior, particularly horizontal variations of long wavelengths such as degree-1 and degree-2 structures, are reviewed with special attention to the cause of ...
Hikaru Iwamori +2 more
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Large polar motions are observed in the apparent polar wander paths of several continents during the Ediacaran. Among various hypotheses proposed in the literature, one consists of the occurrence of two successive fast and large true polar wander (TPW ...
Boris Robert +2 more
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: The ultramafic massif of Feragen, which belongs to the eastern ophiolitic belt of Norway, has abundant amounts of chromite ores. Recent studies have revealed a complex melt evolution in a supra-subduction zone (SSZ) environment. This study presents new
Tian Qiu +4 more
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