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Enhanced surface imaging of crustal deformation = obtaining tectonic force fields using GPS data /

Record Type:	Electronic resources : Monograph/item
Title/Author:	Enhanced surface imaging of crustal deformation/ by A. John Haines ... [et al.].
Reminder of title:	obtaining tectonic force fields using GPS data /
other author:	Haines, A. John.
Published:	Cham :Springer International Publishing : : 2015.,
Description:	x, 99 p. :ill., digital ;24 cm.
[NT 15003449]:	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.
Contained By:	Springer eBooks
Subject:	Inversion (Geophysics) -
Subject:	Earth (Planet) - Internal structure. -
Online resource:	http://dx.doi.org/10.1007/978-3-319-21578-5
ISBN:	9783319215785

Enhanced surface imaging of crustal deformation = obtaining tectonic force fields using GPS data /
Enhanced surface imaging of crustal deformationobtaining tectonic force fields using GPS data /[electronic resource] :by A. John Haines ... [et al.]. - Cham :Springer International Publishing :2015. - x, 99 p. :ill., digital ;24 cm. - SpringerBriefs in earth sciences,2191-5369. - SpringerBriefs in earth sciences..

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.

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.

ISBN: 9783319215785

Standard No.: 10.1007/978-3-319-21578-5doiSubjects--Topical Terms:

588077
Inversion (Geophysics)
Subjects--Geographical Terms:

1640405
Earth (Planet)
--Internal structure.

LC Class. No.: QE601.2 / .H35 2015

Dewey Class. No.: 551.13

Enhanced surface imaging of crustal deformation = obtaining tectonic force fields using GPS data /
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245 0 0 $a Enhanced surface imaging of crustal deformation $h [electronic resource] : $b obtaining tectonic force fields using GPS data / $c by A. John Haines ... [et al.].
260 $a Cham : $b Springer International Publishing : $b Imprint: Springer, $c 2015.
300 $a x, 99 p. : $b ill., digital ; $c 24 cm.
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 Inversion (Geophysics) $3 588077
650 0 $a Faults (Geology) $3 542838
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700 1 $a Haines, A. John. $3 2160192
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