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Journal articles on the topic 'North German Basin'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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1

Lerche, I. "The North German Basin: Some Unresolved Problems." Energy Exploration & Exploitation 17, no. 5 (1999): 277–86. http://dx.doi.org/10.1177/014459879901700506.

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2

Röhling, Heinz-Gerd. "Regional characteristics of the Buntsandstein of the North German Basin (Germany)." Schriftenreihe der Deutschen Gesellschaft für Geowissenschaften 69 (August 31, 2014): 269–384. http://dx.doi.org/10.1127/sdgg/69/2014/269.

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3

McCann, T. "Pre-Permian of the north-east German Basin." Geological Journal 31, no. 2 (1996): 159–77. http://dx.doi.org/10.1002/(sici)1099-1034(199606)31:2<159::aid-gj705>3.0.co;2-8.

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4

SACHS, SVEN, MARKUS WILMSEN, JOSCHUA KNÜPPE, JAHN J. HORNUNG, and BENJAMIN P. KEAR. "Cenomanian–Turonian marine amniote remains from the Saxonian Cretaceous Basin of Germany." Geological Magazine 154, no. 2 (2016): 237–46. http://dx.doi.org/10.1017/s0016756815001004.

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AbstractThe Saxonian Cretaceous Basin constitutes an important source of rare Late Cretaceous marine amniote fossils from Germany. It is also historically famous, having been documented in a series of monographic works published by the distinguished German palaeontologist Hanns Bruno Geinitz in the nineteenth century. The most productive rock units include the upper Cenomanian Dölzschen Formation and upper Turonian Strehlen and Weinböhla limestones (lower Strehlen Formation). A survey of curated specimens recovered from these deposits has now identified isolated teeth of probable polycotylid a

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5

Scheibe, Reiner, Knut Seidel, Mario Vormbaum, and Norbert Hoffmann. "Magnetic and gravity modelling of the crystalline basement in the North German Basin." Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 156, no. 2 (2005): 291–98. http://dx.doi.org/10.1127/1860-1804/2005/0156-0291.

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6

Lempp, Christof, and Ian Lerche. "Correlation of stress directions across the North German Basin: suprasalt and subsalt differences." Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 157, no. 2 (2006): 279–97. http://dx.doi.org/10.1127/1860-1804/2006/0157-0279.

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7

Bansal, A. R., G. Gabriel, V. P. Dimri, and C. M. Krawczyk. "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." GEOPHYSICS 76, no. 3 (2011): L11—L22. http://dx.doi.org/10.1190/1.3560017.

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We propose a modified centroid method to compute the depth to the bottom of magnetic sources (DBMS) based on a fractal source distribution. This approach provides better estimates than the assumption of an uncorrelated source distribution. We apply our approach to a recently compiled homogeneous set of aeromagnetic data from Germany. The deepest DBMS values are found for some large basin areas, i.e., the Molasse basin and parts of the North German basin. Smaller DBMS were estimated for the Moldanubian region in southern Germany and the northern part of the North German basin. A comparison of D

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8

Kockel, F. "Rifting processes in NW-Germany and the German North Sea Sector." Netherlands Journal of Geosciences - Geologie en Mijnbouw 81, no. 2 (2002): 149–58. http://dx.doi.org/10.1017/s0016774600022381.

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AbstractSince the beginning of the development of the North German Basin in Stephanien to Early Rotliegend times, rifting played a major role. Nearly all structures in NW-Germany and the German North Sea - (more than 800) - salt diapirs, grabens, inverted grabens and inversion structures - are genetically related to rifting. Today, the rifting periods are well dated. We find signs of dilatation at all times except from the Late Aptian to the end of the Turonian. To the contrary, the period of the Coniacian and Santonian, lasting only five million years was a time of compression, transpression,

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9

Mingram, Birgit, Peer Hoth, and Daniel E. Harlov. "Nitrogen potential of Namurian shales in the North German Basin." Journal of Geochemical Exploration 78-79 (May 2003): 405–8. http://dx.doi.org/10.1016/s0375-6742(03)00044-x.

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10

Kohnen, Oliver. "Palaeotemperatures from the Upper Oligocene of the North German Basin." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 198, no. 1-2 (1995): 233–41. http://dx.doi.org/10.1127/njgpa/198/1995/233.

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11

Erbacher, Jochen, André Bornemann, Maria Rose Petrizzo, and Stefan Huck. "Chemostratigraphy and stratigraphic distribution of keeled planktonic foraminifera in the Cenomanian of the North German Basin." Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 171, no. 2 (2020): 149–61. http://dx.doi.org/10.1127/zdgg/2020/0211.

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12

Hiete, Michael, Ulrich Berner, Carmen Heunisch, and Heinz-Gerd Röhling. "A high-resolution inorganic geochemical profile across the Zechstein-Buntsandstein boundary in the North German Basin." Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 157, no. 1 (2006): 77–105. http://dx.doi.org/10.1127/1860-1804/2006/0157-0077.

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13

Schmidt Mumm, A., and M. Wolfgramm. "Fluid systems and mineralization in the north German and Polish basin." Geofluids 4, no. 4 (2004): 315–28. http://dx.doi.org/10.1111/j.1468-8123.2004.00090.x.

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14

Hjuler, Morten Leth, Mette Olivarius, Lars Ole Boldreel, et al. "Multidisciplinary approach to assess geothermal potential, Tønder area, North German Basin." Geothermics 78 (March 2019): 211–23. http://dx.doi.org/10.1016/j.geothermics.2018.12.001.

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15

Magri, Fabien, Ulf Bayer, Christoph Jahnke, et al. "Fluid-dynamics driving saline water in the North East German Basin." International Journal of Earth Sciences 94, no. 5-6 (2005): 1056–69. http://dx.doi.org/10.1007/s00531-005-0497-9.

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16

Kaiser, Arne. "Neotectonic modelling of the North German Basin and adjacent areas a tool to understand postglacial landscape evolution?" Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 156, no. 2 (2005): 357–66. http://dx.doi.org/10.1127/1860-1804/2005/0156-0357.

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17

Franz, Matthias, Kerstin Nowak, Sebastian Niegel, Elisabeth Seidel, Marco Wolf, and Markus Wolfgramm. "Deep geothermal resources of the North German Basin: The hydrothermal reservoirs of the Stuttgart Formation (Schilfsandstein, Upper Triassic)." Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 169, no. 3 (2018): 353–87. http://dx.doi.org/10.1127/zdgg/2018/0164.

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18

Fischer, Cornelius. "Carboniferous and Rotliegend sedimentation in the Flechtingen High area (North German Basin)." Jahresberichte und Mitteilungen des Oberrheinischen Geologischen Vereins 95 (April 1, 2013): 107–30. http://dx.doi.org/10.1127/jmogv/95/2013/107.

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19

Feldbusch, Elvira, Thomas Wiersberg, Martin Zimmer, and Simona Regenspurg. "Origin of gases from the geothermal reservoir Groß Schönebeck (North German Basin)." Geothermics 71 (January 2018): 357–68. http://dx.doi.org/10.1016/j.geothermics.2017.09.007.

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20

Diechmann, R., and H. W. Partenscky. "A NEW EQUILIBRIUM ANALYSIS FOR NEARSHORE TIDAL BASINS." Coastal Engineering Proceedings 1, no. 20 (1986): 80. http://dx.doi.org/10.9753/icce.v20.80.

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A large tidal flat area of about 40 tidal basins with catchment areas of between 10 and 790 km2 exists along the coast of the German Bight. Not all of these tidal basins are morphologically stable. The main parameter necessary for determining the state of equilibrium is the volumetric capacity of the concave portions of the tidal basin. In order to examine the equilibrium state it is necessary to compare the volumetric capacity of the tidal basin determined from hydrographic charts (measured volume) with a theoretical volume given by newly developed stability criteria representing averaged con

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21

Köthe, Angelika. "A revised Cenozoic dinoflagellate cyst and calcareous nannoplankton zonation for the German sector of the southeastern North Sea Basin." Newsletters on Stratigraphy 45, no. 3 (2012): 189–220. http://dx.doi.org/10.1127/0078-0421/2012/0021.

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22

Kloppmann, W., L. Dever, and W. M. Edmunds. "Residence time of Chalk groundwaters in the Paris Basin and the North German Basin: a geochemical approach." Applied Geochemistry 13, no. 5 (1998): 593–606. http://dx.doi.org/10.1016/s0883-2927(97)00110-8.

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23

Hoffmann, N., H. Jödicke, and P. Gerling. "The distribution of Pre-Westphalian source rocks in the North German Basin – Evidence from magnetotelluric and geochemical data." Netherlands Journal of Geosciences - Geologie en Mijnbouw 80, no. 1 (2001): 71–84. http://dx.doi.org/10.1017/s0016774600022174.

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AbstractFor the first time this project attempts to directly correlate magnetotelluric and geochemical data with the aim of creating a model on the regional distribution of potential pre-Westphalian source rocks deposited in marine environments in the North German basin.Analysis of the magnetotelluric data shows, that there is a deep good conductor at the north-eastern fringe of the North German basin around the islands of Rügen and Usedom and on the mainland north east of the Anklam Fault. Through integration with seismic data and the offshore well G14 the conductor can be correlated with the

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24

Franz, Matthias, Gerhard H. Bachmann, Jens Barnasch, Carmen Heunisch, and Heinz-Gerd Röhling. "Der Keuper in der Stratigraphischen Tabelle von Deutschland 2016 – kontinuierliche Sedimentation in der norddeutschen Beckenfazies (Variante B)." Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 169, no. 2 (2018): 203–24. http://dx.doi.org/10.1127/zdgg/2018/0114.

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25

Arfai, Jashar, and Rüdiger Lutz. "3D basin and petroleum system modelling of the NW German North Sea (Entenschnabel)." Geological Society, London, Petroleum Geology Conference series 8, no. 1 (2017): 67–86. http://dx.doi.org/10.1144/pgc8.35.

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Abstract3D basin and petroleum system modelling covering the NW German North Sea (Entenschnabel) was performed to reconstruct the thermal history, maturity and petroleum generation of three potential source rocks, namely the Namurian–Visean coals, the Lower Jurassic Posidonia Shale and the Upper Jurassic Hot Shale.Modelling results indicate that the NW study area did not experience the Late Jurassic heat flow peak of rifting as in the Central Graben. Therefore, two distinct heat flow histories are needed since the Late Jurassic to achieve a match between measured and calculated vitrinite refle

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26

Rabbel, W., K. Förste, A. Schulze, R. Bittner, J. Röhl, and J. C. Reichert. "A high‐velocity layer in the lower crust of the North German Basin." Terra Nova 7, no. 3 (1995): 327–37. http://dx.doi.org/10.1111/j.1365-3121.1995.tb00802.x.

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27

Regenspurg, Simona, Elvira Feldbusch, Ben Norden, and Marion Tichomirowa. "Fluid-rock interactions in a geothermal Rotliegend/Permo-Carboniferous reservoir (North German Basin)." Applied Geochemistry 69 (June 2016): 12–27. http://dx.doi.org/10.1016/j.apgeochem.2016.03.010.

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28

Wolf, Marco, Stephan Steuer, Heinz-Gerd Röhling, Dorothee Rebscher, and Fabian Jähne-Klingberg. "Lithofacies distribution in the Central European Basin: a 3D model of the Buntsandstein facies in the central German North Sea." Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 166, no. 4 (2015): 341–59. http://dx.doi.org/10.1127/zdgg/2015/0039.

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29

Hoffmann, Norbert, Hartmut Jödicke, and Laska Horejschi. "Regional distribution of the Lower Carboniferous Culm and Carboniferous limestone facies in the North German Basin derived from magnetotelluric soundings." Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 156, no. 2 (2005): 323–40. http://dx.doi.org/10.1127/1860-1804/2005/0156-0323.

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30

Hattermann, F. F., H. Gömann, T. Conradt, M. Kaltofen, P. Kreins, and F. Wechsung. "Impacts of global change on water-related sectors and society in a trans-boundary central European river basin – Part 1: project framework and impacts on agriculture." Advances in Geosciences 11 (June 15, 2007): 85–92. http://dx.doi.org/10.5194/adgeo-11-85-2007.

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Abstract. Central Europe, the focus region of this study, is a region in transition, climatically from maritime to continental and politically from formerly more planning-oriented to more market-oriented management regimes, and in terms of climate change from regions of increasing precipitation in the west and north of Europe to regions of decreasing precipitation in central and southern Europe. The Elbe basin, a trans-boundary catchment flowing from the Czech Republic through Germany into the North Sea, was selected to investigate the possible impacts of global change on crop yields and water

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31

Barth, G., M. Franz, C. Heunisch, W. Ernst, J. Zimmermann, and M. Wolfgramm. "Marine and terrestrial sedimentation across the T–J transition in the North German Basin." Palaeogeography, Palaeoclimatology, Palaeoecology 489 (January 2018): 74–94. http://dx.doi.org/10.1016/j.palaeo.2017.09.029.

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32

Marotta, A. M., U. Bayer, H. Thybo, and M. Scheck. "Origin of the regional stress in the North German basin: results from numerical modelling." Tectonophysics 360, no. 1-4 (2002): 245–64. http://dx.doi.org/10.1016/s0040-1951(02)00358-x.

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33

Baykulov, Mikhail, Heinz-Jürgen Brink, Dirk Gajewski, and Mi-Kyung Yoon. "Revisiting the structural setting of the Glueckstadt Graben salt stock family, North German Basin." Tectonophysics 470, no. 1-2 (2009): 162–72. http://dx.doi.org/10.1016/j.tecto.2008.05.027.

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34

Sindern, S., V. Havenith, A. Gerdes, F. M. Meyer, D. Adelmann, and A. Hellmann. "Dating of anatase-forming diagenetic reactions in Rotliegend sandstones of the North German Basin." International Journal of Earth Sciences 108, no. 4 (2019): 1275–92. http://dx.doi.org/10.1007/s00531-019-01705-x.

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35

Brink, Heinz-Juergen. "The evolution of the North German Basin and the metamorphism of the lower crust." International Journal of Earth Sciences 94, no. 5-6 (2005): 1103–16. http://dx.doi.org/10.1007/s00531-005-0037-7.

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36

Hübner, Wiete, Matthias Wellbrink, Thomas Röckel, Stephan Steuer, Stefanie Krug, and Torsten Tischner. "Stress rotation in the suprasalt beneath Hanover (North German Basin) derived from image logs of the deep well Groß Buchholz Gt1." Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 166, no. 4 (2015): 361–73. http://dx.doi.org/10.1127/zdgg/2015/0038.

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37

Schaumann, Gerlinde, and Michael Grinat. "Electrical conductivity as an indication for potential geothermal target layers within the North German Basin with respect to local geological conditions." Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 167, no. 2-3 (2016): 121–30. http://dx.doi.org/10.1127/zdgg/2016/0057.

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38

Hoffmann, Norbert, Laska Hengesbach, Bernhard Friedrichs, and Heinz-Jürgen Brink. "The contribution of magnetotellurics to an improved understanding of the geological evolution of the North German Basin review and new results." Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 159, no. 4 (2008): 591–606. http://dx.doi.org/10.1127/1860-1804/2008/0159-0591.

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39

Arfai, Jashar, Fabian Jähne, Rüdiger Lutz, Dieter Franke, Christoph Gaedicke, and Jonas Kley. "Late Palaeozoic to Early Cenozoic geological evolution of the northwestern German North Sea (Entenschnabel): New results and insights." Netherlands Journal of Geosciences - Geologie en Mijnbouw 93, no. 4 (2014): 147–74. http://dx.doi.org/10.1017/njg.2014.22.

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AbstractThe results of a detailed seismic mapping campaign of 13 horizons in the northwestern German North Sea, covering Late Permian to Palaeogene sedimentary successions, are presented. Based on the interpretation of four 3D and two 2D seismic surveys, thickness and depth maps of prominent stratigraphic units were constructed. These maps provide an overview of key structural elements, the sedimentation and erosion, and give insights into the evolution of the German Central Graben. The base of the Zechstein Group reaches a maximum depth of 7800 m within the German Central Graben. Lateral thic

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40

Ahlers, Steffen, Tobias Hergert, and Andreas Henk. "Numerical Modelling of Salt-Related Stress Decoupling in Sedimentary Basins–Motivated by Observational Data from the North German Basin." Geosciences 9, no. 1 (2018): 19. http://dx.doi.org/10.3390/geosciences9010019.

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A three dimensional (3D) finite element model is used to study the conditions leading to mechanical decoupling at a salt layer and vertically varying stress fields in salt-bearing sedimentary basins. The study was inspired by observational data from northern Germany showing stress orientations varying up to 90° between the subsalt and the suprasalt layers. Parameter studies address the role of salt viscosity and salt topology on how the plate boundary forces acting at the basement level affect the stresses in the sedimentary cover above the salt layer. Modelling results indicate that mechanica

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41

Obst, Karsten. "From salt mining and hydrocarbon exploration towards geothermal use and natural gas storage in the eastern part of the North German Basin." Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 170, no. 3-4 (2019): 357–80. http://dx.doi.org/10.1127/zdgg/2019/0207.

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42

Prieto, Jérôme, Lars W. van den Hoek Ostende, Madelaine Böhme, and M. Braze. "Reappearance of Galerix (Erinaceomorpha, Mammalia) at the Middle to Late Miocene transition in South Germany: biostratigraphic and palaeoecologic implications." Contributions to Zoology 80, no. 3 (2011): 179–89. http://dx.doi.org/10.1163/18759866-08003002.

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The presence of Galerix molars in the South German fossil locality Hammerschmiede 3 is interpreted as evidence for a reimmigration of West European origin into the North Alpine Foreland Basin at the transition of the Middle to Late Miocene. The brief re-appearence of Galerix in southern Germany can be used as a biostratigraphic marker that allows promising correlations between local biostratigraphic subdivisions from Spain and Germany, suggesting that, contrary to previous thought, the Hammerschmiede locality may antedate the hipparionine horses’ appearance event. Based on the supposed climati

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43

Nielsen, Lars, Hans Thybo, and Martin Glendrup. "Seismic tomographic interpretation of Paleozoic sedimentary sequences in the southeastern North Sea." GEOPHYSICS 70, no. 4 (2005): R45—R56. http://dx.doi.org/10.1190/1.1996908.

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Seismic wide-angle data were recorded to more than 300-km offset from powerful airgun sources during the MONA LISA experiments in 1993 and 1995 to determine the seismic-velocity structure of the crust and uppermost mantle along three lines in the southeastern North Sea with a total length of 850 km. We use the first arrivals observed out to an offset of 90 km to obtain high-resolution models of the velocity structure of the sedimentary layers and the upper part of the crystalline crust. Seismic tomographic traveltime inversion reveals 2–8-km-thick Paleozoic sedimentary sequences with P-wave ve

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44

Klapper, H. S., R. Baessler, K. Weidauer, and D. Stuerzbecher. "Evaluation of Suitability of High-Alloyed Materials for Geothermal Applications in the North German Basin." CORROSION 68, no. 1 (2012): 016001–1. http://dx.doi.org/10.5006/1.3676631.

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45

Prokoph, A., and J. Thurow. "Diachronous pattern of Milankovitch cyclicity in late Albian pelagic marlstones of the North German Basin." Sedimentary Geology 134, no. 3-4 (2000): 287–303. http://dx.doi.org/10.1016/s0037-0738(00)00050-6.

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46

Alber, M., and C. Solibida. "Geomechanical Characterization of a Host Rock for Enhanced Geothermal System in the North-German Basin." Procedia Engineering 191 (2017): 158–63. http://dx.doi.org/10.1016/j.proeng.2017.05.167.

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47

Gemmer, Lykke, Søren B. Nielsen, and Ulf Bayer. "Late Cretaceous–Cenozoic evolution of the North German Basin—results from 3-D geodynamic modelling." Tectonophysics 373, no. 1-4 (2003): 39–54. http://dx.doi.org/10.1016/s0040-1951(03)00282-8.

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48

Otto, Volker. "Inversion-related features along the southeastern margin of the North German Basin (Elbe Fault System)." Tectonophysics 373, no. 1-4 (2003): 107–23. http://dx.doi.org/10.1016/s0040-1951(03)00287-7.

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49

Jahne, Fabian, and Jonas Kley. "Structural balancing at the southern border of the North East German basin: results and challenges." Geotectonic Research 95 (June 1, 2008): 69–71. http://dx.doi.org/10.1127/1864-5658/08/9501-0069.

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50

Blöcher, Guido, Mauro Cacace, Thomas Reinsch, and Norihiro Watanabe. "Evaluation of three exploitation concepts for a deep geothermal system in the North German Basin." Computers & Geosciences 82 (September 2015): 120–29. http://dx.doi.org/10.1016/j.cageo.2015.06.005.

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