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Plate Deformation from Cradle to Grave - Seismic Anisotropy and Deformation at Mid-Ocean Ridges and in the Lowermost Mantle (Paperback, Softcover reprint of the original 1st ed. 2013)
Loot Price: R3,416
Discovery Miles 34 160
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Plate Deformation from Cradle to Grave - Seismic Anisotropy and Deformation at Mid-Ocean Ridges and in the Lowermost Mantle (Paperback, Softcover reprint of the original 1st ed. 2013)
Series: Springer Theses
Expected to ship within 10 - 15 working days
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The Earth's rocky mantle convects to lose heat, which comes from
the liquid iron core below. The mantle's interfaces - the
core-mantle boundary, and the lithosphere - may hold the key to
understanding mantle motion because of the seismic anisotropy
present in these parts of the Earth. In this thesis, Andy Nowacki
presents a precise but comprehensive review of the current state of
the art in studying flow with anisotropy, mineral physics and
geodynamics. New measurements of shear wave anisotropy in the
lowermost mantle and at mid-ocean ridges are used to constrain
mechanisms of creep and melt extraction in the mantle. A model of
global flow is used to predict anisotropy in the deep Earth, and
novel methods to forward model shear wave splitting are described.
Future studies of mantle flow must incorporate the understanding
gained in this thesis. The thesis contains a substantive
introduction to the structure of the Earth, seismic anisotropy in
general and in the core-mantle boundary region, and mid-ocean ridge
processes. It also describes novel methods for forward modelling
and interpreting shear wave splitting data. Three chapters present
timely research into dynamics at divergent plate boundaries and at
the core-mantle boundary.
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