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Enhanced surface imaging of crustal ...

Earth (Planet)

Enhanced surface imaging of crustal deformationobtaining tectonic force fields using GPS data /

Record Type:	Electronic resources : Monograph/item
Title/Author:	Enhanced surface imaging of crustal deformationby 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.
Contained By:	Springer eBooks
Subject:	Inversion (Geophysics)
Subject:	Earth (Planet)Rotation.
Online resource:	http://dx.doi.org/10.1007/978-3-319-21578-5
ISBN:	9783319215785$q(electronic bk.)

Enhanced surface imaging of crustal deformationobtaining 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$q(electronic bk.)

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

405222
Inversion (Geophysics)
Subjects--Geographical Terms:

611612
Earth (Planet)
--Rotation.

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

Dewey Class. No.: 551.13

Enhanced surface imaging of crustal deformationobtaining tectonic force fields using GPS data /
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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.
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