Global ETD Search
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Showing 1 to 5 of 5 for “"GPS Velocity Field"”.
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GPS Velocity Field In The Transition From Subduction To Collision Of The Eastern Sunda And Banda Arcs, Indonesia
Campaign GPS measurements during 2001-2003 in the transition between subduction and collision of the Banda arc reveal how strain is partitioned away from the trench and distributed to other parts of the arc-trench system. Genrich, et. al. (1996) conducted a GPS campaign (1992-1994) throughout the …
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Kinematically consistent, elastic block model for the eastern Mediterranean constrained by GPS measurements
I use a Global Positioning System (GPS) velocity field to constrain block models of the eastern Mediterranean and surrounding regions that account for the angular velocities of constituent blocks and elastic strain accumulation on block-bounding faults in the interseismic period. Kinematically …
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Present day plate boundary deformation in the Caribbean and crustal deformation on southern Haiti
… I use the available campaign and continuous GPS measurements in the Caribbean to derive a regional velocity field expressed in a consistent reference frame. I use this velocity field as input to a kinematic model where surface velocities result from the rotation of rigid blocks bounded by …
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Establishing the kinematics of the North East Region of South Africa with the use of GPS data
… data, supplemented with other available Nubian GPS data, to determine whether the North East Region of South Africa is segregated from the Nubian Plate. A ten year GPS time series (processed using the Bernese 5.0 precise GNSS software) is minimally constrained to the ITRF2008, using the …
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Kinematics and Dynamics of Continental Deformation
… Zagros mountains. Seismological, geodetic and field results are used to study the source parameters and slip distribution of this earthquake, and demonstrate that the earthquake was left-lateral and occurred on a fault striking ENE–WSW; approximately perpendicular to previously studied faults …