SEISMISCHE OBERFLÄCHENWELLEN IN EINER LATERAL INHOMOGENEN ERDE von V I Keilis-borok
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eBay-Artikelnr.:187660616166
Artikelmerkmale
- Artikelzustand
- ISBN-10
- 9401068852
- Book Title
- Seismic Surface Waves in a Laterally Inhomogeneous Earth (Modern
- Item Height
- 9.25 inches
- ISBN
- 9789401068857
Über dieses Produkt
Product Identifiers
Publisher
Springer Netherlands
ISBN-10
9401068852
ISBN-13
9789401068857
eBay Product ID (ePID)
175979338
Product Key Features
Number of Pages
304 Pages
Publication Name
Seismic Surface Waves in a Laterally Inhomogeneous Earth
Language
English
Publication Year
2011
Subject
Physics / Geophysics, Earth Sciences / Geology
Type
Textbook
Subject Area
Science
Series
Modern Approaches in Geophysics Ser.
Format
Trade Paperback
Dimensions
Item Weight
16.7 Oz
Item Length
9.3 in
Item Width
6.1 in
Additional Product Features
Intended Audience
Scholarly & Professional
Preface by
Its, E. N., Yanovskaya, T., Lander, A. V.
Dewey Edition
19
Series Volume Number
9
Number of Volumes
1 vol.
Illustrated
Yes
Dewey Decimal
551.2/2
Table Of Content
1. Theory.- 1. Surface waves in vertically inhomogeneous media.- 2. Surface waves in media with weak lateral inhomogeneity.- 3. Surface waves in media involving vertical contacts.- 4. Computation techniques for surface waves.- 2. Interpretation of Surface Wave Observations.- 5. Recording, identification, and measurement of surface wave parameters.- 6. Methods for quantitative interpretation of observations.- 7. Some results from studies of regional lithospheric structure by surface waves.- References.
Synopsis
Surface waves form the longest and strongest portion of a seismic record excited by explosions and shallow earthquakes. Traversing areas with diverse geologic structures, they 'absorb' information on the properties of these areas which is best retlected in dispersion, the dependence of velocity on frequency. The other prop erties of these waves - polarization, frequency content, attenuation, azimuthal variation of the amplitude and phase - arc also controlled by the medium between the source and the recording station; some of these are affected by the properties of the source itself and by the conditions around it. In recent years surface wave seismology has become an indispensable part of seismological practice. The maximum amplitude in the surface wave train of virtually every earthquake or major explosion is being measured and used by all national and international seismological surveys in the determination of the most important energy parameter of a seismic source, namely, the magnitude M,. The relationship between M, and the body wave magnitude fI1t, is routinely employed in identification of underground nuclear explosions. Surface waves of hundreds of earthquakes recorded every year are being analysed to estimate the seismic moment tensor of earthquake sources, to determine the periods of free oscillations of the Earth, to construct regional dispersion curves from which in turn the crustal and upper mantle structure in various areas is derived, and to evaluate the dissipative parameters of the mantle material., Surface waves form the longest and strongest portion of a seismic record excited by explosions and shallow earthquakes. Traversing areas with diverse geologic structures, they 'absorb' information on the properties of these areas which is best retlected in dispersion, the dependence of velocity on frequency. The other prop- erties of these waves - polarization, frequency content, attenuation, azimuthal variation of the amplitude and phase - arc also controlled by the medium between the source and the recording station; some of these are affected by the properties of the source itself and by the conditions around it. In recent years surface wave seismology has become an indispensable part of seismological practice. The maximum amplitude in the surface wave train of virtually every earthquake or major explosion is being measured and used by all national and international seismological surveys in the determination of the most important energy parameter of a seismic source, namely, the magnitude M, . The relationship between M, and the body wave magnitude fI1t, is routinely employed in identification of underground nuclear explosions. Surface waves of hundreds of earthquakes recorded every year are being analysed to estimate the seismic moment tensor of earthquake sources, to determine the periods of free oscillations of the Earth, to construct regional dispersion curves from which in turn the crustal and upper mantle structure in various areas is derived, and to evaluate the dissipative parameters of the mantle material.
LC Classification Number
QC801-809
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- 1***0 (1563)- Bewertung vom Käufer.Letzter MonatBestätigter KaufAS SHOWN/DESCRIBED. IT IS A GREAT BOOK WITH COLORED INSTRUCTIONS WITHIN. I ONLY SUGGEST THAT ALL SELLERS OF BOOKS WOULD SHOW 2-3 PHOTOS OF ITS CONTENTS. IN DOING SO IT MAY HELP WITH ANY QUESTIONS BUYERS MIGHT HAVE. SECURED PKG, SUPER FAST FREE SHIPPING, SUPER FAST DELIVERY. BOUGHT ITEM, IMMEDIATELY PAID FOR IT, WAS SHIPPED AND DELIVERED WITHIN 24 HOURS VIA AMAZON! I COULD NOT BE HAPPIER. AND I HIGHLY RECOMMEND THIS OUTSTANDING SELLER! THANK YOU FOR EVERYTHING!
- 0***t (10)- Bewertung vom Käufer.Letzte 6 MonateBestätigter KaufItem was exactly as described and packaged to protect it. Seller’s pricing was spot on and when I received it, it was in good condition. Seller actually messaged me when they shipped it (I really appreciated that). Overall I’m happy doing business with them!
- 8***g (254)- Bewertung vom Käufer.Letzte 6 MonateBestätigter KaufA smooth and professional transaction throughout. The item was exactly as described, clearly listed, and fairly priced. Communication from the seller was prompt, polite, and helpful, with dispatch confirmed quickly. The parcel was securely packaged and arrived in excellent condition, ahead of the expected delivery date. Care was taken at every stage of the process. I would be happy to buy from this seller again—many thanks for a reliable and well-handled sale.FINLAND AND EUROPE: INTERNATIONAL CRISES IN THE PERIOD OF By Juhani Paasivirta (Nr. 335694307643)