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  • 1
    Schlagwort(e): Permian Basin ; hydrocarbon ; geothermal energy
    Beschreibung / Inhaltsverzeichnis: 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
    Seiten: Online-Ressource (IX, 570 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 9781786203885
    Sprache: Englisch
    Standort Signatur Erwartet Verfügbarkeit
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  • 2
    Publikationsdatum: 2019-02-27
    Print ISSN: 2191-2203
    Digitale ISSN: 2191-2211
    Thema: Geologie und Paläontologie , Wirtschaftswissenschaften
    Publiziert von Springer
    Standort Signatur Erwartet Verfügbarkeit
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  • 3
    Publikationsdatum: 2017-07-06
    Beschreibung: This Article reports results from a field experiment investigating the influence of volcanic tephra coverage on glacier ablation. These influences are known to be significantly different from those of moraine debris on glaciers due to the contrasting grain size distribution and thermal conductivity. Influences of tephra deposits on glacier ablation have hardly been studied so far. For the experiment, artificial plots of two different tephra types from Eyjafjallajökull and Grimsvötn volcanoes were installed on a snow-covered glacier surface of Vatnajökull ice cap, Iceland.Ablation was automatically monitored along with atmospheric variables and ablation on a non-tephra covered reference site over the summer season 2015. For each of the two volcanic tephra types, three plots (~ 1.5 mm, ~ 8.5 mm and ~ 80 mm) were monitored. After limiting the records to a period of reliable measurements, a 50-days dataset of hourly records was obtained, which can be downloaded from the Pangaea data repository (https://www.pangaea.de; https://doi.org/10.1594/PANGAEA.876656). The experiment shows a substantial increase of ablation under the ~ 1.5 mm and ~ 8.5 mm tephra plots when compared to uncovered conditions. Only under the thick tephra cover some insulating effects could be observed. This result is in contrast to other studies which depicted insulating effects for much thinner tephra coverson bare-ice glacier surfaces. Differences between the influences of the two different petrological types of tephra exist but are small.
    Digitale ISSN: 1866-3591
    Thema: Geologie und Paläontologie
    Publiziert von Copernicus
    Standort Signatur Erwartet Verfügbarkeit
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  • 4
    Publikationsdatum: 2019-03-25
    Beschreibung: Layered evaporite sequences (LES) comprise interbedded weak layers (halite and, commonly, bittern salts) and strong layers (anhydrite and usually non-evaporite rocks such as carbonates and siliciclastics). This results in a strong rheological stratification, with a range of effective viscosity up to a factor of 105. We focus here on the deformation of competent intrasalt beds in different modes of salt tectonics using a combination of conceptual, numerical and analog models, and seismic data. In bedding-paralell extension, boudinage of the strong layers forms ruptured stringers, within a halite matrix, that become increasingly isolated with increasing strain. In bedding-parallel shortening, competent layers tend to maintain coherency while forming harmonic, disharmonic, and polyharmonic folds, with the rheological stratification leading to buckling and fold growth by bedding-parallel shear. In differential loading, extension and the resultant stringers dominate beneath suprasalt depocenters while folded competent beds characterize salt pillows. Finally, in tall passive diapirs, stringers generated by intrasalt extension are rotated to near vertical in tectonic melanges during upward flow of salt. In all cases, strong layers are progressively removed from areas of salt thinning and increasingly disrupted and folded in areas of salt growth as deformation intensifies. The varying styles of intrasalt deformation impact seismic imaging of LES and associated interpretations. Ruptured stringers are often visible where they have low dips, as in slightly extended salt layers or beneath depocenters, but are usually not imaged in tall passive diapirs due to steep dips. In contrast, areas of slightly to moderately shortened salt typically have well imaged, mostly continuous intrasalt reflectors, although seismic coherency decreases as deformation intensifies. Similarly, wells are most likely to penetrate strong layers in contractional structures and salt pillows, less likely in extended salt because they might drill between stringers, and unlikely in tall passive diapirs because the stringers are near-vertical. Thus, both seismic and well data may be interpreted to suggest that diapirs and other areas of more intense intrasalt deformation are more halite rich than is actually the case.
    Digitale ISSN: 1869-9537
    Thema: Geologie und Paläontologie
    Publiziert von Copernicus im Namen von European Geosciences Union.
    Standort Signatur Erwartet Verfügbarkeit
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  • 5
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  • 7
    Publikationsdatum: 2018-01-10
    Beschreibung: We report results from a field experiment investigating the influence of volcanic tephra coverage on glacier ablation. These influences are known to be significantly different from those of moraine debris on glaciers due to the contrasting grain size distribution and thermal conductivity. Thus far, the influences of tephra deposits on glacier ablation have rarely been studied. For the experiment, artificial plots of two different tephra types from Eyjafjallajökull and Grímsvötn volcanoes were installed on a snow-covered glacier surface of Vatnajökull ice cap, Iceland. Snow-surface lowering and atmospheric conditions were monitored in summer 2015 and compared to a tephra-free reference site. For each of the two volcanic tephra types, three plots of variable thickness (∼ 1.5, ∼ 8.5 and ∼ 80 mm) were monitored. After limiting the records to a period of reliable measurements, a 50-day data set of hourly records was obtained, which can be downloaded from the Pangaea data repository (https://www.pangaea.de; doi:10.1594/PANGAEA.876656). The experiment shows a substantial increase in snow-surface lowering rates under the ∼ 1.5 and ∼ 8.5 mm tephra plots when compared to uncovered conditions. Under the thick tephra cover some insulating effects could be observed. These results are in contrast to other studies which depicted insulating effects for much thinner tephra coverage on bare-ice glacier surfaces. Differences between the influences of the two different petrological types of tephra exist but are negligible compared to the effect of tephra coverage overall.
    Print ISSN: 1866-3508
    Digitale ISSN: 1866-3516
    Thema: Geologie und Paläontologie
    Publiziert von Copernicus
    Standort Signatur Erwartet Verfügbarkeit
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  • 8
    Publikationsdatum: 2019-06-28
    Beschreibung: Layered evaporite sequences (LESs) comprise interbedded weak layers (halite and, commonly, bittern salts) and strong layers (anhydrite and usually non-evaporite rocks such as carbonates and siliciclastics). This results in a strong rheological stratification, with a range of effective viscosity up to a factor of 105. We focus here on the deformation of competent intrasalt beds in different endmember modes of salt tectonics, even though combinations are common in nature, using a combination of conceptual, numerical, and analog models, and seismic data. In bedding-parallel extension, boudinage of the strong layers forms ruptured stringers, within a halite matrix, that become more isolated with increasing strain. In bedding-parallel shortening, competent layers tend to maintain coherency while forming harmonic, disharmonic, and polyharmonic folds, with the rheological stratification leading to buckling and fold growth by bedding-parallel shear. In differential loading, extension and the resultant stringers dominate beneath suprasalt depocenters, while folded competent beds characterize salt pillows. Finally, in passive diapirs, stringers generated by intrasalt extension are rotated to near vertical and encased in complex folds during upward flow of salt. In all cases, strong layers are progressively removed from areas of salt thinning and increasingly disrupted and folded in areas of salt growth as deformation intensifies. The varying styles of intrasalt deformation impact seismic imaging of LES and associated interpretations. Ruptured stringers are often visible where they have low dips, as in slightly extended salt layers or beneath depocenters, but are poorly imaged in passive diapirs due to steep dips. In contrast, areas of slightly to moderately shortened salt typically have well-imaged, mostly continuous intrasalt reflectors, although seismic coherency decreases as deformation intensifies. Similarly, wells are most likely to penetrate strong layers in contractional structures and salt pillows, less likely in extended salt because they might drill between stringers, and unlikely in tall passive diapirs because the stringers are near vertical. Thus, both seismic and well data may be interpreted to suggest that diapirs and other areas of more intense intrasalt deformation are more halite rich than is actually the case.
    Print ISSN: 1869-9510
    Digitale ISSN: 1869-9529
    Thema: Geologie und Paläontologie
    Publiziert von Copernicus im Namen von European Geosciences Union.
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 9
    Publikationsdatum: 2013-12-07
    Print ISSN: 1437-3254
    Digitale ISSN: 1437-3262
    Thema: Geologie und Paläontologie
    Publiziert von Springer
    Standort Signatur Erwartet Verfügbarkeit
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  • 10
    Publikationsdatum: 2009-05-06
    Print ISSN: 1437-3254
    Digitale ISSN: 1437-3262
    Thema: Geologie und Paläontologie
    Publiziert von Springer
    Standort Signatur Erwartet Verfügbarkeit
    BibTip Andere fanden auch interessant ...
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