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Charlotte M. Krawczyk

Researcher at Technical University of Berlin

Publications -  151
Citations -  3069

Charlotte M. Krawczyk is an academic researcher from Technical University of Berlin. The author has contributed to research in topics: Geology & Distributed acoustic sensing. The author has an hindex of 29, co-authored 132 publications receiving 2518 citations. Previous affiliations of Charlotte M. Krawczyk include University of Potsdam & Leibniz Association.

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Dynamic strain determination using fibre-optic cables allows imaging of seismological and structural features

TL;DR: F fibre-optic cables used for telecommunications are used to obtain strain data and identify faults and volcanic dykes in Iceland and it is suggested that fibre- Optic cables could be used for hazard assessment.
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The S reflector west of Galicia (Spain): Evidence from prestack depth migration for detachment faulting during continental breakup

TL;DR: In this article, the S reflector is shown as an undulating (in time), locally discontinuous reflection on existing seismic profiles west of Iberia, and it is interpreted as a brittle detachment fault which controlled the final breakup of the continent west of Galicia.
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Post-Variscan (end Carboniferous-Early Permian) basin evolution in Western and Central Europe

TL;DR: In this article, the authors provide an overview of a variety of basin types, to more fully explore the controls upon the tectonomagmatic-sedimentary evolution of these important basins.
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Estimation of depth to the bottom of magnetic sources by a modified centroid method for fractal distribution of sources: An application to aeromagnetic data in Germany

TL;DR: In this paper, a modified centroid method was proposed to compute the depth to the bottom of magnetic sources (DBMS) based on a fractal source distribution, which provides better estimates than the assumption of an uncorrelated source distribution.
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An integrated study of the NE German Basin

TL;DR: In this paper, the authors integrated a variety of geological and geophysical data in order to reveal the present day deep crustal structure of the NE German Basin, where a thick high-velocity lower crustal layer is present below the basin centre.