portada Seismic Anisotropy in the Earth (en Inglés)

Seismic Anisotropy in the Earth (en Inglés)

Formato

Libro Físico

Autor

V. Babuska

M. Cara

Editorial

Springer

Idioma

Inglés

N° páginas

219

Encuadernación

Tapa Blanda

Dimensiones

23.4x15.6x1.2 cm

Peso

0.33 kg.

ISBN13

9789401055963

Categorías

Geofísica
Geología, geomorfología y la litosfera
La tierra: historia natural general. interés general

Seismic Anisotropy in the Earth (en Inglés)

V. Babuska (Autor) · M. Cara (Autor) · Springer · Tapa Blanda

Libro Nuevo Importado

Envío: 17 a 24 días háb.

$ 189.32$ 94.66

-50%

Costos de importación incluídos en el precio ✅

Libro Nuevo

Quedan más de 100 unidades

$ 94.66

Llega entre el 22 Sep y el 05 Oct a Quito, Pichincha. Seleccionar ubicación

Agregar a lista de deseos

Reseña del libro "Seismic Anisotropy in the Earth (en Inglés)"

Structural geologists are well aware of the fact that isotropic rocks are quite exceptional in nature. Whicheverorigin, sedimentary, metamorphicormagmatic, rocks are shaped with a plane of mineral flattening, the foliation in geologists' jargon, and with a line ofmineral elongation, the lineation. Just like a good quarryman, a trained structural geologistwill detectapreferredorientationin an apparently isotropic granite. Preferred mineral orientation and thus structural anisotropy are the rule in nature. Consideringthe largevariationsinelasticcoefficientsofrock-forming minerals, itcould be predicted that, in turn, seismic anisotropy should exist and be important, provided thatdomains withasimilarstructural signatureare largeenough to affectseismic waves. This is why, in 1982 at a conference held in Frankfurt, which was oneofthe fIrst meetings devoted to the subject of seismic anisotropy, I asked Don Anderson the question of why seismologists had not considered earlier in their models the obvious constraint of anisotropy. I still remember Don's answer: "Adolphe, we knew that our isotropic models were not very good but we had no other choice. It is simply that, so far, computerswere not largeenough tointegrate the anisotropy parameter". Changingisotropic glassesfor anisotropic ones permits us to obtain betterand more realistic seismic modelsofthe Earth's interior, but, maybe more importantly, it has, for a seismologist, the farreaching consequenceofsteppinginto the fIeld ofgeodynamics.