Name: Lattice-Preferred Orientation and Microstructures of Minerals and Their Implications for Seismic Anisotropy (en Inglés)
SKU: 57869362
Price: 64270.00 CLP
Availability: InStock
Author: Jung, Haemyeong ; Park, Munjae
ISBN: 9783036526423

portada Lattice-Preferred Orientation and Microstructures of Minerals and Their Implications for Seismic Anisotropy (en Inglés)

Lattice-Preferred Orientation and Microstructures of Minerals and Their Implications for Seismic Anisotropy (en Inglés)

Formato

Libro Físico

Editorial

Mdpi AG

Autor

Jung, Haemyeong ; Park, Munjae

Idioma

Inglés

N° páginas

204

Encuadernación

Tapa Dura

Dimensiones

24.4x17x1.8 cm

Peso

0.64 kg.

ISBN13

9783036526423

Categorías

Ciencia: cuestiones generales
Tecnología: cuestiones generales

Lattice-Preferred Orientation and Microstructures of Minerals and Their Implications for Seismic Anisotropy (en Inglés)

Jung, Haemyeong ; Park, Munjae (Autor) · Mdpi AG · Tapa Dura

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Reseña del libro "Lattice-Preferred Orientation and Microstructures of Minerals and Their Implications for Seismic Anisotropy (en Inglés)"

The lattice-preferred orientation (LPO) of minerals is important for interpreting seismic anisotropy, which occurs in the Earth's crust and mantle, and for understanding the internal structure of the deep interior of the Earth. The characterization of microstructures, including LPO, grain size, grain shape, and misorientation, is important to determine the deformation conditions, deformation histories, kinematics, and seismic anisotropies in the crust and mantle The articles in this Special Issue prove that studies of LPO and microstructures of minerals and rocks are a major research area and provide a foundation for interpreting seismic anisotropy in the crust, mantle, and subduction zones. Therefore, the authors hope that this Special Issue encompassing recent advances in the measurement of LPOs of different minerals under various tectonic settings will be a fundamental and valuable resource for the readers and researchers interested in exploring the deformation conditions of minerals and rocks, as well as the interpretation of seismic anisotropy in the crust, mantle, and subduction zones.