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  • 1
    Call number: M 08.0124
    In: Aachener geowissenschaftliche Beiträge
    Type of Medium: Monograph available for loan
    Pages: II, 26 S.
    ISBN: 3861309645
    Series Statement: Aachener geowissenschaftliche Beiträge 43
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 2
    Call number: S 00.0063(60)
    In: Schriftenreihe der Deutschen Gesellschaft für Geowissenschaften
    Type of Medium: Series available for loan
    Pages: 360 S.
    ISBN: 9783510492077
    Series Statement: Schriftenreihe der Deutschen Gesellschaft für Geowissenschaften 60
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 3
    Keywords: Permian Basin ; hydrocarbon ; geothermal energy
    Description / Table of Contents: Mesozoic resource potential in the Southern Permian Basin area: the geological key to exploiting remaining hydrocarbons whilst unlocking geothermal potential / Ben Kilhams, Peter A. Kukla, Stan Mazur, Tom McKie, Harmen F. Mijnlieff, Kees van Ojik and Eveline Rosendaal / Geological Society, London, Special Publications, 469, 1-18, 3 May 2018, https://doi.org/10.1144/SP469.26 --- Tectonic framework --- Timing and spatial patterns of Cretaceous and Cenozoic inversion in the Southern Permian Basin / Jonas Kley / Geological Society, London, Special Publications, 469, 19-31, 9 March 2018, https://doi.org/10.1144/SP469.12 --- The only way is up – on Mesozoic uplifts and basin inversion events in SE Poland / Piotr Krzywiec, Aleksandra Stachowska and Agata Stypa / Geological Society, London, Special Publications, 469, 33-57, 20 March 2018, https://doi.org/10.1144/SP469.14 --- The Wiek Fault System east of Rügen Island: origin, tectonic phases and its relationship to the Trans-European Suture Zone / Elisabeth Seidel, Martin Meschede and Karsten Obst / Geological Society, London, Special Publications, 469, 59-82, 24 January 2018, https://doi.org/10.1144/SP469.10 --- Fault system evolution in the Baltic Sea area west of Rügen, NE Germany / André Deutschmann, Martin Meschede and Karsten Obst / Geological Society, London, Special Publications, 469, 83-98, 9 March 2018, https://doi.org/10.1144/SP469.24 --- New insights into salt tectonics in the northern Dutch offshore: a framework for hydrocarbon exploration / Matthijs van Winden, Jan de Jager, Bastiaan Jaarsma and Renaud Bouroullec / Geological Society, London, Special Publications, 469, 99-117, 29 January 2018, https://doi.org/10.1144/SP469.9 --- Deriving relationships between diapir spacing and salt-layer thickness in the Southern North Sea / Karina Hernandez, Neil C. Mitchell and Mads Huuse / Geological Society, London, Special Publications, 469, 119-137, 26 February 2018, https://doi.org/10.1144/SP469.16 --- Triassic resources --- An introduction to the Triassic: current insights into the regional setting and energy resource potential of NW Europe / Mark Geluk, Tom McKie and Ben Kilhams / Geological Society, London, Special Publications, 469, 139-147, 26 January 2018, https://doi.org/10.1144/SP469.1 --- Lower Triassic reservoir development in the northern Dutch offshore / M. Kortekaas, U. Böker, C. van der Kooij and B. Jaarsma / Geological Society, London, Special Publications, 469, 149-168, 13 April 2018, https://doi.org/10.1144/SP469.19 --- The ‘Buntsandstein’ gas play of the Horn Graben (German and Danish offshore): dry well analysis and remaining hydrocarbon potential / Ben Kilhams, Snezana Stevanovic and Carlo Nicolai / Geological Society, London, Special Publications, 469, 169-192, 11 January 2018, https://doi.org/10.1144/SP469.5 --- Geothermal resources of the North German Basin: exploration strategy, development examples and remaining opportunities in Mesozoic hydrothermal reservoirs / Matthias Franz, Gregor Barth, Jens Zimmermann, Ingmar Budach, Kerstin Nowak and Markus Wolfgramm / Geological Society, London, Special Publications, 469, 193-222, 13 April 2018, https://doi.org/10.1144/SP469.11 --- Towards a better understanding of the highly overpressured Lower Triassic Bunter reservoir rocks in the Terschelling Basin / Stefan Peeters, Annemiek Asschert and Hanneke Verweij / Geological Society, London, Special Publications, 469, 223-236, 22 March 2018, https://doi.org/10.1144/SP469.13 --- Enhanced gas recovery of an ageing field utilizing N2 displacement: De Wijk Field, The Netherlands / Rajasmita Goswami, Fritz C. Seeberger and Geert Bosman / Geological Society, London, Special Publications, 469, 237-251, 16 January 2018, https://doi.org/10.1144/SP469.2 --- Data mining in the Dutch Oil and Gas Portal: a case study on the reservoir properties of the Volpriehausen Sandstone interval / B. M. M. van Kempen, H. F. Mijnlieff and J. van der Molen / Geological Society, London, Special Publications, 469, 253-267, 15 March 2018, https://doi.org/10.1144/SP469.15 --- Jurassic resources --- Tectonostratigraphy of a rift basin affected by salt tectonics: synrift Middle Jurassic–Lower Cretaceous Dutch Central Graben, Terschelling Basin and neighbouring platforms, Dutch offshore / R. Bouroullec, R. M. C. H. Verreussel, C. R. Geel, G. de Bruin, M. H. A. A. Zijp, D. Kőrösi, D. K. Munsterman, N. M. M. Janssen and S. J. Kerstholt-Boegehold / Geological Society, London, Special Publications, 469, 269-303, 15 March 2018, https://doi.org/10.1144/SP469.22 --- Stepwise basin evolution of the Middle Jurassic–Early Cretaceous rift phase in the Central Graben area of Denmark, Germany and The Netherlands / R. M. C. H. Verreussel, R. Bouroullec, D. K. Munsterman, K. Dybkjær, C. R. Geel, A. J. P. Houben, P. N. Johannessen and S. J. Kerstholt-Boegehold / Geological Society, London, Special Publications, 469, 305-340, 15 March 2018, https://doi.org/10.1144/SP469.23 --- Palaeogeographical evolution of the Lower Jurassic: high-resolution biostratigraphy and sequence stratigraphy in the Central European Basin / Gregor Barth, Grzegorz Pieńkowski, Jens Zimmermann, Matthias Franz and Gesa Kuhlmann / Geological Society, London, Special Publications, 469, 341-369, 4 January 2018, https://doi.org/10.1144/SP469.8 --- The impact of Quaternary glaciation on temperature and pore pressure in Jurassic troughs in the Southern Permian Basin, northern Germany / Victoria F. Sachse and Ralf Littke / Geological Society, London, Special Publications, 469, 371-398, 16 January 2018, https://doi.org/10.1144/SP469.7 --- The Posidonia Shale of northern Germany: unconventional oil and gas potential from high-resolution 3D numerical basin modelling of the cross-junction between the eastern Lower Saxony Basin, Pompeckj Block and Gifhorn Trough / Alexander T. Stock and Ralf Littke / Geological Society, London, Special Publications, 469, 399-421, 5 April 2018, https://doi.org/10.1144/SP469.21 --- Cretaceous resources --- Reservoir architecture model of the Nieuwerkerk Formation (Early Cretaceous, West Netherlands Basin): diachronous development of sand-prone fluvial deposits / A. G. Vondrak, M. E. Donselaar and D. K. Munsterman / Geological Society, London, Special Publications, 469, 423-434, 15 March 2018, https://doi.org/10.1144/SP469.18 --- Tectonic control on the Early Cretaceous Bentheim Sandstone sediments in the Schoonebeek oil field, The Netherlands / Geert-Jan Vis, Willem D. Smoor, Kees W. Rutten, Jan de Jager and Harmen F. Mijnlieff / Geological Society, London, Special Publications, 469, 435-455, 15 March 2018, https://doi.org/10.1144/SP469.25 --- The impact of heterogeneity on waterflood developments in clastic inner shelf reservoirs: an example from the Holland Greensand Member, Rotterdam Field, The Netherlands / Richard J. Porter, Alberto Muñoz Rojas and Malte Schlüter / Geological Society, London, Special Publications, 469, 457-477, 16 April 2018, https://doi.org/10.1144/SP469.20 --- Lower Cretaceous reservoir development in the North Sea Central Graben, and potential analogue settings in the Southern Permian Basin and South Viking Graben / Frank Zwaan / Geological Society, London, Special Publications, 469, 479-504, 4 January 2018, https://doi.org/10.1144/SP469.3 --- Erosional valleys at a major Late Jurassic–Early Cretaceous unconformity offshore Germany and The Netherlands: potential reservoirs or deteriorated seals? / Marco Wolf, Annelieke Vis and Annemiek Asschert / Geological Society, London, Special Publications, 469, 505-517, 25 January 2018, https://doi.org/10.1144/SP469.4 --- Giant pockmark formation from Cretaceous hydrocarbon expulsion in the western Lower Saxony Basin, The Netherlands / Frank Strozyk, Lars Reuning, Stefan Back and Peter Kukla / Geological Society, London, Special Publications, 469, 519-536, 11 January 2018, https://doi.org/10.1144/SP469.6 --- F17-Chalk: new insights in the tectonic history of the Dutch Central Graben / Henk van Lochem / Geological Society, London, Special Publications, 469, 537-558, 19 February 2018, https://doi.org/10.1144/SP469.17
    Pages: Online-Ressource (IX, 570 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 9781786203885
    Language: English
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  • 4
    Series available for loan
    Series available for loan
    Hannover : Deutsche Geologische Gesellschaft
    Associated volumes
    Call number: S 00.0063(33)
    In: Schriftenreihe der Deutschen Geologischen Gesellschaft
    Type of Medium: Series available for loan
    Pages: 283 S. , Ill., graph. Darst., Kt
    ISBN: 393253705X
    Series Statement: Schriftenreihe der Deutschen Geologischen Gesellschaft 33
    Classification: A.3.16.
    Note: Beitr. teilw. dt., teilw. engl
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 5
    Publication Date: 2012-02-13
    Description: Large rock inclusions are embedded in many salt bodies and these respond to the movements of the salt in a variety of ways including displacement, folding and fracturing. One mode of salt tectonics is downbuilding, whereby the top of a developing diapir remains in the same vertical position while the surrounding overburden sediments subside. We investigate how the differential displacement of the top salt surface caused by downbuilding induces ductile salt flow and the associated deformation of brittle stringers by an iterative procedure to detect and simulate conditions for the onset of localization of deformation in a finite element model, in combination with adaptive remeshing. The model set-up is constrained by observations from the South Oman Salt Basin, where large carbonate bodies encased in salt form substantial hydrocarbon plays. The model shows that, depending on the displacement of the top salt, the stringers can break very soon after the onset of salt tectonics and can deform in different ways. If extension along the inclusion dominates, stringers are broken by tensile fractures and boudinage at relatively shallow depth. Spacing of the boudin–bounding faults can be as close as 3–4 times the thickness of the stringer. In contrast, salt shortening along the inclusion may lead to folding or thrusting of stringers.
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  • 6
    Publication Date: 2012-12-11
    Description: Despite a long history of investigation, several critical issues regarding the glacial history of NW Europe, particularly in currently marine areas, remain unsolved. In this study, we present a comprehensive three-dimensional (3D) seismic interpretation of an area measuring 2000 km2 in the western part of the Danish North Sea that exhibits several buried Quaternary landforms. Well data are used to assign minimum and maximum ages for the studied sedimentary succession. The most prominent buried landforms are three large-scale tunnel valleys of probable Saalian age that extend over more than 20 km across the western and southern part of the study area. These valleys most probably formed through subglacial meltwater erosion close to the termination of a former ice sheet. In the southern part of the study area, an extensive network of small-scale, dendritic seismic lineations interpreted as a palaeo-drainage system characterizes the landward termination of one major tunnel valley. This drainage system was active either contemporaneously or shortly after the development of the tunnel valley. Interpretation of this system as contemporaneous to tunnel-valley formation suggests that steady-state subglacial meltwater discharge was funnelled through a drainage system into the main tunnel valley. In contrast, interpretation of the drainage network as post-incisional points to the development of a post-glacial river system re-using the pre-existing tunnel valley as a downstream fluvial pathway. This uncertainty in the interpretation has important consequences for prediction of the rock content and reservoir characteristics of the tunnel-valley infill, in that either meltwater deposits or fluvial sediments form a considerable part of the tunnel-valley infill.
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  • 7
    Publication Date: 2017-11-04
    Description: The causes of continental breakup are still poorly understood. More and more it becomes evident that classical concepts of deep-mantle versus intra-plate forces controlling continental breakup and shaping the subsequent evolution of the bordering passive margins, including associated vertical and horizontal movements, need to be revised. Instead of thinking in terms of active versus passive rift models or magma-poor versus magma-rich margins, concepts are needed that perceive these geodynamic processes in a three dimensional continuum evolving through time. The South Atlantic margins, often considered as a classical example for a plume related continental breakup, seem to be a perfect site to revisit and to test such new concepts. Traces of intense magmatism are present on both conjugate margins as well as aseismic ridges connecting them with a supposed current plume location below the island of Tristan da Cunha. Of these ridges, the Walvis Ridge has been interpreted as one of the major hotspot trails in the South Atlantic. The German priority program SAMPLE (DFG-SPP 1375: South Atlantic Margin Processes and Links with onshore Evolution), funded by the German Science Foundation (DFG) from 2008 to 2016, addressed a number of fundamental questions related to the processes responsible for opening of the South Atlantic and the subsequent evolution of both continental margins. This volume assembles new results emerging from multidisciplinary research in the SAMPLE projects and those of other groups working in the region.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , NonPeerReviewed
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  • 8
    Publication Date: 2017-06-10
    Description: The Aachen RWTH-1 well was drilled to 2544mTVD for geothermal purposes and gives substance to extensive geoscientific research. It is located in a hydrothermally and seismically active area of the Aachen Anticline, 500m NW of the Aachen Overthrust and 420m ENE of the Laurensberg Fault. The main focus of this PhD work is the structural and microtectonic analysis of the cores sampled. For 94% of the total well length the collected cuttings give information of the lithology and stratigraphy of the subsurface. A total of 145.5m was cored in three different intervals. A complete set of wireline measurements including high resolution borehole image allow mapping of fractures and folds, and linking the core to the logs. About 100 core samples were selected for detailed microstructural analysis.
    Description: conference
    Keywords: VBL 500 ; VAE 200 ; VKA 130 ; VKA 200 ; Geologische Bohrungen in einzelnen Regionen ; Geodynamik der Lithosphäre {Geologie} ; Optische Petrographie ; Gefügekunde der Gesteine ; Aachen 〈Region〉 ; Tiefbohrung ; Dünnschliff ; Gefüge 〈Gesteinskunde〉
    Language: German
    Type: anthologyArticle , publishedVersion
    Format: application/pdf
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  • 9
    Publication Date: 2017-06-10
    Description: Movement on fault planes causes a large amount of smaller-scale deformation, ductile or brittle, in the area surrounding the fault. Much of this deformation is below the resolution of reflection seismics (i.e. sub-seismic, 〈10m displacement), but it is important to determine this deformation, since it can make up a large portion of the total bulk strain, for instance in a developing sedimentary basin. Calculation of the amount of sub-seismic strain around a fault by 3-D geometrical kinematic retro-deformation can also be used to predict the orientation and magnitude of these smaller-scale structures. However, firstly a 3-D model of the fault and its faulted horizons must be constructed at a high enough resolution to be able to preserve fault and horizon morphology with a grid spacing of less than 10 m. Secondly, the kinematics of the fault need to be determined, and thirdly a suitable deformation algorithm chosen to fit the deformation style. Then by restoring the faulted horizons to their pre-deformation state (a ‘regional’), the moved horizons can be interrogated as to the strain they underwent. Since strain is commutative, the deformation demonstrated during this retro-deformation is equivalent to that during the natural, forward deformation...
    Description: conference
    Keywords: TQC 220 ; TSB 000 ; VAE 200 ; VAE 400 ; VBE 000 ; Reflexionsseismik {Geophysik} ; Mitteleuropa {Geophysik} ; Geodynamik der Lithosphäre {Geologie} ; Tektogenese {Geologie} ; Modellierung von Prozessen in der Geosphäre ; Niedersächsiches Becken ; Dreidimensionale Seismik ; Störung 〈Geologie〉 ; Kinematik ; Modell
    Language: German
    Type: anthologyArticle , publishedVersion
    Format: application/pdf
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  • 10
    Publication Date: 2012-07-01
    Description: The megacrack pattern of the ephemeral north Panamint dry lake, California, United States, is characterized by variably sized polygons with diameters ranging from hundreds of meters to meters. The evolution and subsurface extent of this polygonal pattern and a probable tectonic link are examined by ground resistivity measurements and surface mapping. Crack development is initiated by the shrinking of clays caused by changes in water content near the surface. For crack evolution, the following processes are proposed: Cavities develop at approximately 1-m (∼3-ft) depth during a subsurface phase, followed by the collapse of the overburden into the existing cavities to form the surface cracks. Cracks are filled by wind-blown sand and dried-out lake sediments from collapsing crack walls. Following burial, differences in competence between crack-fill and surrounding playa-lake sediments provide zones of structural weakness that might channelize stress release and faulting. Ground resistivity measurements confirmed the extent of the cracks to a depth of more than 3 m (〉9 ft). The megacrack pattern is compared to a Rotliegende (Upper Permian) tight gas field, located in the southern Permian Basin of northwestern Germany, situated in a comparable geologic setting. There, a multidirectional polygonal pattern is recorded on horizon slices of three-dimensional seismic data and compares well to our observations from the Panamint Valley. The Rotliegende pattern is associated with low-offset faults, which are proposed to be responsible for subtle reservoir compartmentalization.
    Print ISSN: 0149-1423
    Electronic ISSN: 0149-1423
    Topics: Geosciences
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