Corné Kreemer

TL;DR: The Global Strain Rate Model (GSRM v.2.1) as mentioned in this paper is a new global model of plate motions and strain rates in plate boundary zones constrained by horizontal geodetic velocities.

TL;DR: In this article, a global model (GSRM-1) of both horizontal velocities on the Earth's surface and horizontal strain rates for almost all deforming plate boundary zones is presented.

TL;DR: Development here of Median Interannual Difference Adjusted for Skewness (MIDAS), a variant of the Theil‐Sen median trend estimator, which computes a robust and realistic estimate of trend uncertainty and has the potential for broader application in the geosciences.

TL;DR: In this paper, the authors show that the true size and tsunami potential can be determined using Global Positioning System (GPS) data up to only 15 min after earthquake initiation, by tracking the mean displacement of the Earth's surface associated with the arrival of seismic waves.

TL;DR: In this article, the authors place the present kinematics in the eastern Mediterranean and Middle East in light of the post-Middle Miocene geological history and propose that in addition to the effects of the Hellenic subduction and Zagros collision-subduction zones on driving the surface motion, an underlying asthenospheric flow is also required.