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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Λεπτομέρειες βιβλιογραφικής εγγραφής
Κύριοι συγγραφείς: Haines, A. John (Συγγραφέας), Dimitrova, Lada L. (Συγγραφέας), Wallace, Laura M. (Συγγραφέας), Williams, Charles A. (Συγγραφέας)
Συγγραφή απο Οργανισμό/Αρχή: SpringerLink (Online service)
Μορφή: Ηλεκτρονική πηγή Ηλ. βιβλίο
Γλώσσα:English
Έκδοση: Cham : Springer International Publishing : Imprint: Springer, 2015.
Έκδοση:1st ed. 2015.
Σειρά:SpringerBriefs in Earth Sciences,
Θέματα:
Διαθέσιμο Online:Full Text via HEAL-Link
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100 1 |a Haines, A. John.  |e author. 
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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490 1 |a SpringerBriefs in Earth Sciences,  |x 2191-5369 
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 Earth sciences. 
650 0 |a Geophysics. 
650 0 |a Natural disasters. 
650 0 |a Mathematical physics. 
650 1 4 |a Earth Sciences. 
650 2 4 |a Geophysics/Geodesy. 
650 2 4 |a Natural Hazards. 
650 2 4 |a Mathematical Applications in the Physical Sciences. 
700 1 |a Dimitrova, Lada L.  |e author. 
700 1 |a Wallace, Laura M.  |e author. 
700 1 |a Williams, Charles A.  |e author. 
710 2 |a SpringerLink (Online service) 
773 0 |t Springer eBooks 
776 0 8 |i Printed edition:  |z 9783319215778 
830 0 |a SpringerBriefs in Earth Sciences,  |x 2191-5369 
856 4 0 |u http://dx.doi.org/10.1007/978-3-319-21578-5  |z Full Text via HEAL-Link 
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950 |a Earth and Environmental Science (Springer-11646)