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Understanding Seismic Anisotropy in Exploration and Exploitation, Leon Thomsen


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Автор: Leon Thomsen
Название:  Understanding Seismic Anisotropy in Exploration and Exploitation
Перевод названия: Постижение и использование сейсмической анизотропии
ISBN: 9781560803263
Издательство: Mare Nostrum (Eurospan)
Классификация:

ISBN-10: 1560803266
Обложка/Формат: Paperback
Страницы: 304
Вес: 1.01 кг.
Дата издания: 30.12.2014
Серия: Distinguished instructor series
Язык: English
Издание: 2 revised edition
Размер: 279 x 216
Читательская аудитория: Primary and secondary/elementary and high school
Ключевые слова: Geophysics,Volcanology & seismology
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Поставляется из: Англии
Описание: Wide-azimuth surveying has shown that most rocks are azimuthally anisotropic, with P-wave velocities and P-AVO gradients varying with azimuth. Analysis with narrow-azimuth algorithms and concepts will necessarily fail to exploit this data. This book shows how to recognise anisotropy effects in data and provides intuitive concepts to analyse it.


Seismic Anisotropy in the Earth

Автор: V. Babuska; M Cara
Название: Seismic Anisotropy in the Earth
ISBN: 0792313216 ISBN-13(EAN): 9780792313212
Издательство: Springer
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Цена: 20896.00 р.
Наличие на складе: Есть у поставщика Поставка под заказ.

Описание: 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.

Seismic Anisotropy in the Earth

Автор: V. Babuska; M Cara
Название: Seismic Anisotropy in the Earth
ISBN: 9401055963 ISBN-13(EAN): 9789401055963
Издательство: Springer
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Цена: 15672.00 р.
Наличие на складе: Есть у поставщика Поставка под заказ.

Описание: 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.

Isotropic and Anisotropic Seismic Tomography Using Active Source and Earthquake Records

Автор: Yu-Pin Lin
Название: Isotropic and Anisotropic Seismic Tomography Using Active Source and Earthquake Records
ISBN: 9811050678 ISBN-13(EAN): 9789811050671
Издательство: Springer
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Цена: 16769.00 р.
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Описание:

Introduction.- Assessment of Tomography Models of Taiwan Using First-arrival Times from the TAIGER Active-source Experiment.- Crustal Velocity Variations in Taiwan Revealed by Active-source Seismic Observations.- Full-wave Effects on Shear-wave Splitting.- Full-wave Multiscale Anisotropy Tomography in Southern California.- Concluding Remarks.

Continuum Mechanics of Anisotropic Materials

Автор: Stephen C. Cowin
Название: Continuum Mechanics of Anisotropic Materials
ISBN: 1489990275 ISBN-13(EAN): 9781489990273
Издательство: Springer
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Цена: 10447.00 р.
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Описание: Continuum Mechanics of Anisotropic Materials presents an entirely new and unique development of material anisotropy in the context of an appropriate selection and organization of continuum mechanics topics.

Seismology of azimuthally anisotropic media and seismic fracture characterization

Автор: Tsvankin, Ilya Grechka, Vladimir
Название: Seismology of azimuthally anisotropic media and seismic fracture characterization
ISBN: 1560802286 ISBN-13(EAN): 9781560802280
Издательство: Mare Nostrum (Eurospan)
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Цена: 17932.00 р.
Наличие на складе: Нет в наличии.

Описание: Presents an analysis of seismic signatures for azimuthally anisotropic media and shows anisotropic inversion/processing methods for wide-azimuth reflection data and VSP surveys. The focus is kinematic parameter-estimation techniques; the prestack amplitudes section includes AVO and attenuation coefficients; field examples are included.


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