Enhanced surface imaging of crustal ...
Earth (Planet)

 

  • Enhanced surface imaging of crustal deformation[electronic resource] :obtaining tectonic force fields using GPS data /
  • 紀錄類型: 書目-語言資料,印刷品 : Monograph/item
    杜威分類號: 551.13
    書名/作者: Enhanced surface imaging of crustal deformation : obtaining tectonic force fields using GPS data // by A. John Haines ... [et al.].
    其他作者: Haines, A. John.
    出版者: Cham : : Springer International Publishing :, 2015.
    面頁冊數: x, 99 p. : : ill., digital ;; 24 cm.
    Contained By: Springer eBooks
    標題: Inversion (Geophysics)
    標題: Faults (Geology)
    標題: Rock deformation.
    標題: Geology, Structural.
    標題: Earth Sciences.
    標題: Geophysics/Geodesy.
    標題: Natural Hazards.
    標題: Mathematical Applications in the Physical Sciences.
    標題: Earth (Planet) - Rotation.
    ISBN: 9783319215785
    ISBN: 9783319215778
    內容註: 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.
    摘要、提要註: 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.
    電子資源: http://dx.doi.org/10.1007/978-3-319-21578-5
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