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  • 2015-2019  (9)
  • 2018  (6)
  • 2015  (3)
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  • 2015-2019  (9)
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  • 1
    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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  • 2
    Publication Date: 2018-01-01
    Print ISSN: 1342-937X
    Electronic ISSN: 1878-0571
    Topics: Geosciences
    Published by Elsevier
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  • 3
    Publication Date: 2018-11-09
    Print ISSN: 1354-0793
    Electronic ISSN: 2041-496X
    Topics: Chemistry and Pharmacology , Geosciences
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  • 4
  • 5
    Publication Date: 2018-01-01
    Print ISSN: 0305-8719
    Electronic ISSN: 2041-4927
    Topics: Geosciences
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  • 6
    Publication Date: 2015-10-01
    Description: Paleoclimate reconstructions based on reef corals require precise detection of diagenetic alteration. Secondary calcite can significantly affect paleotemperature reconstructions at very low amounts of 1%. X-ray powder diffraction is routinely used to detect diagenetic calcite in aragonitic corals. This procedure has its limitations as single powder samples might not represent the entire coral heterogeneity. A conventional and a 2-D X-ray diffractometer were calibrated with gravimetric powder standards of high and low magnesium calcite (0.3% to 25% calcite). Calcite contents 〈1% can be recognized with both diffractometer setups based on the peak area of the calcite [104] reflection. An advantage of 2-D-XRD over convenient 1-D-XRD methods is the nondestructive and rapid detection of calcite with relatively high spatial resolution directly on coral slabs. The calcite detection performance of the 2-D-XRD setup was tested on thin sections from fossil Porites sp. samples that, based on powder XRD measurements, showed 〈1% calcite. Quantification of calcite contents for these thin sections based on 2-D-XRD and digital image analysis showed very similar results. This enables spot measurements with diameters of 4 mm, as well as systematic line scans along potential tracks previous to geochemical proxy sampling. In this way, areas affected by diagenetic calcite can be avoided and alternative sampling tracks can be defined. Alternatively, individual sampling positions that show dubious proxy results can later be checked for the presence of calcite. The presented calibration and quantification method can be transferred to any 2-D X-ray diffractometer. © 2015. American Geophysical Union. All Rights Reserved.
    Electronic ISSN: 1525-2027
    Topics: Chemistry and Pharmacology , Geosciences , Physics
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  • 7
  • 8
    Publication Date: 2015-05-05
    Description: After Mesozoic rifting, the Atlantic margin of Morocco has recorded the consequences of the continental collision between Africa and Europe and the relative northward motion of the African plate over the Canary Island hotspot during Cenozoic times. Interpretation of recently acquired 2D seismic reflection data (MIRROR 2011 experiment) presents new insights into the Late Cretaceous to recent geodynamic evolution of this margin. Crustal uplift presumably started during the Late Cretaceous and triggered regional tilting in the deep-water margin west of Essaouira and the formation of the Base Tertiary Unconformity (BTU). An associated hiatus in sedimentation is interpreted to have started earlier in the north (presumably in the Cenomanian at well location DSDP 416) and propagated to the south (presumably in the Coniacian at well location DSDP 415). The difference in the total duration of this hiatus is postulated to have controlled the extrusion of Late Triassic to Early Jurassic salt during the Late Cretaceous to Early Palaeocene non-depositional period, resulting in regional differences in the preservation of salt structures: the Agadir Basin in the south of the study area is dominated by salt diapirs, whereas massive canopies characterised the Ras Tafelnay Plateau farther north and salt-poor canopies and weld structures the northernmost offshore Essaouira and Safi Basins. Accompanied by volcanic intrusions, a presumably Early Palaeogene reactivation of previously existing basement faults is interpreted to have formed a series of deep-water anticlines with associated gravity deformation of shallow-seated sediments. The orientation of the fold axes is roughly perpendicular to the present day coast and the extensional fault direction; therefore, not a coast-line parallel pattern of extensional faults, related to the rifting and break-up of the margin, but rather a coast-line perpendicular oceanic fracture zone might have caused the basement faults associated with the deep-water folds. Both the volcanic intrusions and the formation of the deep-water anticlines show a comparable age trend which gets progressively younger towards the south. A potential tempo-spatial relationship of the BTU and the reactivation of basement faults can be explained by the relative northward motion of the African plate over the Canary Island hotspot. Regional uplift producing the BTU could have been the precursor of the approaching hotspot during the Late Cretaceous, followed during the Early Palaeogene by a locally more pronounced uplift above the hotspot centre. © 2015 The Authors. Basin Research © 2015 John Wiley & Sons Ltd, European Association of Geoscientists & Engineers and International Association of Sedimentologists
    Print ISSN: 0950-091X
    Electronic ISSN: 1365-2117
    Topics: Geosciences
    Published by Wiley
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  • 9
    Publication Date: 2018-01-10
    Description: 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
    Electronic ISSN: 1866-3516
    Topics: Geosciences
    Published by Copernicus
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