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LEADER 00000cam a2200601Ii 4500 
003    OCoLC 
005    20160311052453.3 
006    m     o  d         
007    cr cnu|||unuuu 
008    150813s2015    sz      ob    000 0 eng d 
019    SPRINGERocn918135875 
020    9783319215785 
020    3319215787 
020    |z9783319215778 
020    3319215779|q(print) 
020    9783319215778|q(print) 
024 7  10.1007/978-3-319-21578-5 
040    N$T|beng|erda|epn|cN$T|dN$T|dGW5XE|dYDXCP|dIDEBK|dSNK|dCDX
       |dWAU|dCOO|dOCLCF|dEBLCP|dDEBSZ 
043    x------ 
049    MAIN 
050  4 QE601.2|b.H35 2015eb 
082 04 551.13|223 
100 1  Haines, A. J.|q(A. John),|eauthor. 
245 10 Enhanced surface imaging of crustal deformation :
       |bobtaining tectonic force fields using GPS data /|cA. 
       John Haines, Lada L. Dimitrova, Laura M. Wallace, Charles 
       A. Williams. 
264  1 Cham :|bSpringer,|c2015. 
300    1 online resource. 
336    text|btxt|2rdacontent 
337    computer|bc|2rdamedia 
338    online resource|bcr|2rdacarrier 
490 1  SpringerBriefs in earth sciences 
504    Includes bibliographical references. 
505 0  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    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. 
650  0 Inversion (Geophysics) 
650  0 Faults (Geology) 
650  0 Rock deformation. 
650  0 Geology, Structural. 
651  0 Earth (Planet)|xSurface. 
651  0 Earth (Planet)|xCrust. 
655  0 Electronic books. 
655  4 Electronic books. 
700 1  Dimitrova, Lada L.,|eauthor. 
700 1  Wallace, Laura,|d1973-|eauthor. 
700 1  Williams, Charles A.|q(Charles Addison),|eauthor. 
710 2  SpringerLink|eissuing body. 
776 08 |iPrinted edition:|z9783319215778 
830  0 SpringerBriefs in earth sciences. 
830  0 Springer English/International eBooks 2015 - Full Set 
856 40 |uhttps://ezp.lib.unimelb.edu.au/login?url=http://
       link.springer.com/10.1007/978-3-319-21578-5|zConnect to 
       ebook (University of Melbourne only) 
990    Springer Full Set 2015 
990    Batch Ebook load (bud2) - do not edit, delete or attach 
       any records. 
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