Enhanced Surface Imaging of Crustal Deformation Obtaining Tectonic Force Fields Using GPS Data /

This book takes an in depth look at a novel methodology for analyzing Global Positioning System (GPS) data to obtain the highest possible resolution surface imaging of tectonic deformation sources without prescribing the nature of either the sources or the subsurface medium. GPS methods are widely u...

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Detalles Bibliográficos
Clasificación:Libro Electrónico
Autores principales: Haines, A. John (Autor), Dimitrova, Lada L. (Autor), Wallace, Laura M. (Autor), Williams, Charles A. (Autor)
Autor Corporativo: SpringerLink (Online service)
Formato: Electrónico eBook
Idioma:Inglés
Publicado: Cham : Springer International Publishing : Imprint: Springer, 2015.
Edición:1st ed. 2015.
Colección:SpringerBriefs in Earth Sciences,
Temas:
Geophysics.
Natural disasters.
Mathematical physics.
Natural Hazards.
Mathematical Physics.
Acceso en línea:Texto Completo

MARC

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100 1 |a Haines, A. John.  |e author.  |4 aut  |4 http://id.loc.gov/vocabulary/relators/aut 
245 1 0 |a Enhanced Surface Imaging of Crustal Deformation  |h [electronic resource] :  |b Obtaining Tectonic Force Fields Using GPS Data /  |c by A. John Haines, Lada L. Dimitrova, Laura M. Wallace, Charles A. Williams. 
250 |a 1st ed. 2015. 
264 1 |a Cham :  |b Springer International Publishing :  |b Imprint: Springer,  |c 2015. 
300 |a X, 99 p. 50 illus., 37 illus. in color.  |b online resource. 
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505 0 |a 1. Introduction.- 2. Introduction to the Vertical Derivatives of Horizontal Stress (VDoHS) Rates -- 3. Inversion Methodology -- 4. 1-Dimensional Synthetic Examples -- 5. Application to Central South Island, New Zealand -- 6. 2-Dimensional Examples -- 7. Concluding Remarks. 
520 |a This book takes an in depth look at a novel methodology for analyzing Global Positioning System (GPS) data to obtain the highest possible resolution surface imaging of tectonic deformation sources without prescribing the nature of either the sources or the subsurface medium. GPS methods are widely used to track the surface expression of crustal deformation at tectonic plate boundaries, and are typically expressed in terms of velocity fields or strain rate fields. Vertical derivatives of horizontal stress (VDoHS) rates at the Earth's surface can also be derived from GPS velocities, and VDoHS rates provide much higher resolution information about subsurface deformation sources than velocities or strain rates. In particular, VDoHS rates allow for high precision estimates of fault dips, slip rates and locking depths, as well as objective characterization of previously unknown (or hidden) tectonic deformation zones. 
650 0 |a Geophysics. 
650 0 |a Natural disasters. 
650 0 |a Mathematical physics. 
650 1 4 |a Geophysics. 
650 2 4 |a Natural Hazards. 
650 2 4 |a Mathematical Physics. 
700 1 |a Dimitrova, Lada L.  |e author.  |4 aut  |4 http://id.loc.gov/vocabulary/relators/aut 
700 1 |a Wallace, Laura M.  |e author.  |4 aut  |4 http://id.loc.gov/vocabulary/relators/aut 
700 1 |a Williams, Charles A.  |e author.  |4 aut  |4 http://id.loc.gov/vocabulary/relators/aut 
710 2 |a SpringerLink (Online service) 
773 0 |t Springer Nature eBook 
776 0 8 |i Printed edition:  |z 9783319215778 
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830 0 |a SpringerBriefs in Earth Sciences,  |x 2191-5377 
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912 |a ZDB-2-SXEE 
950 |a Earth and Environmental Science (SpringerNature-11646) 
950 |a Earth and Environmental Science (R0) (SpringerNature-43711) 

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