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Publications
Helmholtz Centre Potsdam
GFZ German Research Centre for Geosciences
(Co) Author: Krawczyk, C.
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Krawczyk, C. M.; Prolom, U.; Trabs, S.; Dahm, T. (2011): Suffosion and collapse sinkholes in the city of Hamburg - High-resolution imaging of subrosion structures by urban shear-wave reflection seismics. Journal of Applied Geophysics, 78, 133-143.
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Endres, H.; Samiee, R.; Lohr, T.; Krawczyk, C. M.; Tanner, D. C.; Trappe, H.; Thierer, P. O.; Oncken, O.; Kukla, P. A. (2008): Quantitative fracture prediction from seismic data. Petroleum Geoscience, 14, 4, 369-377.
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Groß, K.; Micksch, U.; and TIPTEQ Research Group, Seismics Team; Araneda, M.; Bataille, K.; Bribach, J.; Buske, S.; Krawczyk, C. M.; Lüth, S.; Mechie, J.; Schulze, A.; Shapiro, S. A.; Stiller, M.; Wigger, P.; Ziegenhagen, T. (2008): The reflection seismic survey of project TIPTEQ - the inventory of the Chilean subduction zone at 38.2° S. Geophysical Journal International, 172, 2, 565-571.
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Lohr, T.; Krawczyk, C. M.; Tanner, D. C.; Samiee, R.; Endres, H.; Thierer, P. O.; Oncken, O.; Trappe, H.; Bachmann, R.; Kukla, P. A. (2008): Prediction of subseismic faults and fractures: Integration of three-dimensional seismic data, three-dimensional retrodeformation, and well data on an example of deformation around an inverted fault. AAPG Bulletin, 92, 4, 473-485.
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Lohr, T.; Krawczyk, C. M.; Tanner, D. C.; Samiee, R.; Endres, H.; Trappe, H.; Oncken, O.; Kukla, P. A. (2007): Strain partitioning due to salt: insights from interpretation of a 3D seismic data set in the NW German Basin. Basin Research, 19, 4, 579-597.
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Franke, D.; Neben, S.; Schreckenberger, B.; Schulze, A.; Stiller, M.; Krawczyk, C. M. (2006): Crustal structure across the Colorado Basin, offshore Argentina. Geophysical Journal International, 165, 3, 850-864.
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Kossow, D.; Krawczyk, C. M. (2002): Structure and quantification of processes controlling the evolution of the inverted NE-German Basin. Marine and Petroleum Geology, 19, 5, 601-618.
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Krawczyk, C. M.; Eilts, F.; Lassen, A.; & Thybo, H. (2002): Seismic evidence of Caledonian deformed crust and uppermost mantle structures in the northern part of the Trans-European Suture Zone (TESZ), SW Baltic Sea.. Tectonophysics, 360, 1-4, 215-244.
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