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Mark van der Meijde

Researcher at University of Twente

Publications -  39
Citations -  2381

Mark van der Meijde is an academic researcher from University of Twente. The author has contributed to research in topics: Seismic wave & Advanced Spaceborne Thermal Emission and Reflection Radiometer. The author has an hindex of 21, co-authored 39 publications receiving 1953 citations. Previous affiliations of Mark van der Meijde include ETH Zurich & International Institute of Minnesota.

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Multi- and hyperspectral geologic remote sensing: A review

TL;DR: A review of multispectral and hyperspectral remote sensing data, products and applications in geology shows a unique opportunity to develop standardized protocols leading to validated and reproducible products from satellite remote sensing for the geology community.
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Seismic evidence for water deep in Earth's upper mantle.

TL;DR: Water in the deep upper mantle can influence the properties of seismic discontinuities in the mantle transition zone, and observations of converted seismic waves provide evidence of a 20- to 35-kilometer-thick discontinuity near a depth of 410 kilometers.
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Spatiotemporal landslide detection for the 2005 Kashmir earthquake region.

TL;DR: In this paper, an area of 36 km2 was selected in which changes in landslide activity, area, and types were quantified after each monsoon season for the following consecutive three years.
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Crustal structure beneath broad-band seismic stations in the Mediterranean region

TL;DR: In this paper, a grid search method was proposed to determine the best fitting receiver function for a given receiver function, containing both the direct conversion and reverberated phases, on a model grid of varying Moho depth and varying Poisson's ratio.
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Complex rupture mechanism and topography control symmetry of mass-wasting pattern, 2010 Haiti earthquake

TL;DR: In this paper, the authors conclude that a combined effect of complex rupture dynamics and topography primarily control this previously rarely documented landslide pattern, and they conclude that lower static stress drop, mean fault displacement, and blind ruptures of the 2010 Haiti earthquake resulted in fewer, smaller and more symmetrically distributed landslides than previous studies would suggest.