Enhanced surface imaging of crustal deformation [electronic resource] : obtaining tectonic force fields using GPS data / A. John Haines, Lada L. Dimitrova, Laura M. Wallace, Charles A. Williams.
2015
QE601.2 .H35 2015eb
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Title
Enhanced surface imaging of crustal deformation [electronic resource] : obtaining tectonic force fields using GPS data / A. John Haines, Lada L. Dimitrova, Laura M. Wallace, Charles A. Williams.
ISBN
9783319215785 electronic book
3319215787 electronic book
9783319215778
3319215787 electronic book
9783319215778
Published
Cham : Springer, 2015.
Language
English
Description
1 online resource.
Item Number
10.1007/978-3-319-21578-5 doi
Call Number
QE601.2 .H35 2015eb
Dewey Decimal Classification
551.13
Summary
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 Earthℓ́ℓs 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.
Bibliography, etc. Note
Includes bibliographical references.
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Access limited to authorized users.
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Series
SpringerBriefs in earth sciences.
Available in Other Form
Print version: 9783319215778
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Table of Contents
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.
3. Inversion Methodology
4. 1-Dimensional Synthetic Examples
5. Application to Central South Island, New Zealand
6. 2-Dimensional Examples
7. Concluding Remarks.