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000733598 020__ $$a9783319215785$$qelectronic book
000733598 020__ $$a3319215787$$qelectronic book
000733598 020__ $$z9783319215778
000733598 0247_ $$a10.1007/978-3-319-21578-5$$2doi
000733598 035__ $$aSP(OCoLC)ocn918135875
000733598 035__ $$aSP(OCoLC)918135875
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000733598 050_4 $$aQE601.2$$b.H35 2015eb
000733598 08204 $$a551.13$$223
000733598 1001_ $$aHaines, A. J.$$q(A. John),$$eauthor.
000733598 24510 $$aEnhanced surface imaging of crustal deformation$$h[electronic resource] :$$bobtaining tectonic force fields using GPS data /$$cA. John Haines, Lada L. Dimitrova, Laura M. Wallace, Charles A. Williams.
000733598 264_1 $$aCham :$$bSpringer,$$c2015.
000733598 300__ $$a1 online resource.
000733598 336__ $$atext$$btxt$$2rdacontent
000733598 337__ $$acomputer$$bc$$2rdamedia
000733598 338__ $$aonline resource$$bcr$$2rdacarrier
000733598 4901_ $$aSpringerBriefs in earth sciences
000733598 504__ $$aIncludes bibliographical references.
000733598 5050_ $$a1. 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.
000733598 506__ $$aAccess limited to authorized users.
000733598 520__ $$aThis 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.
000733598 650_0 $$aInversion (Geophysics)
000733598 650_0 $$aFaults (Geology)
000733598 650_0 $$aRock deformation.
000733598 650_0 $$aGeology, Structural.
000733598 651_0 $$aEarth (Planet)$$xSurface.
000733598 651_0 $$aEarth (Planet)$$xCrust.
000733598 7001_ $$aDimitrova, Lada L.,$$eauthor.
000733598 7001_ $$aWallace, Laura,$$d1973-$$eauthor.
000733598 7001_ $$aWilliams, Charles A.$$q(Charles Addison),$$eauthor.
000733598 77608 $$iPrint version:$$z9783319215778
000733598 830_0 $$aSpringerBriefs in earth sciences.
000733598 85280 $$bebk$$hSpringerLink
000733598 85640 $$3SpringerLink$$uhttps://univsouthin.idm.oclc.org/login?url=http://link.springer.com/10.1007/978-3-319-21578-5$$zOnline Access$$91397441.1
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000733598 980__ $$aEBOOK
000733598 980__ $$aBIB
000733598 982__ $$aEbook
000733598 983__ $$aOnline
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