Plate Deformation from Cradle to Grave : Seismic Anisotropy and Deformation at Mid-Ocean Ridges and in the Lowermost Mantle (Springer Theses)

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Plate Deformation from Cradle to Grave : Seismic Anisotropy and Deformation at Mid-Ocean Ridges and in the Lowermost Mantle (Springer Theses)

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  • 製本 Hardcover:ハードカバー版/ページ数 162 p./サイズ 70 illus., 61 in color
  • 商品コード 9783642348419

Full Description

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.

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