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  • 1
    Call number: 9/M 04.0316
    In: Geological Society special publication
    Description / Table of Contents: Content: Exhumation of the North Atlantic margin: introduction and background, A G Dore, J A Cartwright, M S Stoker, J P Turner and N White • Present and past influence of the Iceland Plume on sedimentation, S M Jones, N White, B J Clarke, E Rowley and K Gallagher • Timing and mechanisms of North Atlantic Cenozoic uplift: evidence for mantle upwelling, M Rohrman, P A Van Der Beek, R D Van Der Hilst and P Reemst • Paleocene initiation of Cenozoic uplift in Norway, S B Nielsen, G E Paulsen, D L Hansen, L Gemmer, O R Clausen, B H Jacobsen, N Balling, M Huuse and K Gallagher • A structural transect between the central North Sea Dome and the South Swedish Dome: Middle Jurassic-Quaternary uplift-subsidence reversal and exhumation across the eastern North Sea Basin, O Graversen • Cenozoic inversion and uplift of southern Britain, D J Blundell • Landforms and uplift in Scandinavia, K Lidmar-Bergstrom and J O Naslund • Pattern and timing of the post-Caledonian denudation of northern Scandinavia constrained by apatite fission-track thermochronology, B W H Hendriks and P A M Andriessen • Along-slope variation in the late Neogene evolution of the mid-Norwegian margin in response to uplift and tectonism, D Evans, S McGiveron, Z Harrison, P Bryn and K Berg • Reconstructing the erosion history of glaciated passive margins: applications of in situ produced cosmogenic nuclide techniques, A P Stroeven, D Fabel, J Harbor, C Hattestrand and J Kleman • The thermotectonic development of southern Sweden during Mesozoic and Cenozoic time, C Cederbom • Neogene uplift and erosion of southern Scandinavia induced by the rise of the South Swedish Dome, P Japsen, T Bidstrup and K Lidmar-Bergstrom • Cenozoic uplift and denudation of southern Norway: insights from the North Sea Basin, M Huuse • Tectonic impact on sedimentary processes during Cenozoic evolution of the northern North Sea and surrounding areas, J I Faleide, R Kyrkjebo, T Kjennerud, R H Gabrielsen, H Jordt, S Fanavoll and M D Bjerke • Scotland's denudational history: an integrated view of erosion and sedimentation at an uplifted passive margin, A Hall and P Bishop • Cenozoic evolution of the Faroe Platform, comparing denudation and deposition, M S Andersen, A B Sorensen, L O Boldreel and T Nielsen • Late Neogene development of the UK Atlantic margin, M S Stoker • Quantifying exhumation from apatite fission-track analysis and vitrinite reflectance data: precision, accuracy and latest results from the Atlantic margin of NW Europe, P F Green, I R Duddy and K A Hegarty • Sonic velocity analysis of the Tertiary denudation of the Irish Sea basin, P D Ware and J P Turner • The Post-Variscan thermal and denudational history of Ireland, P A Allen, S D Bennett, M J M Cunningham, A Carter, K Gallagher, E Lazzaretti, J Galewsky, A L Densmore, W E A Phillips, D Naylor and C S Hach • Prediction of the hydrocarbon system in exhumed basins, and application to the NW European margin, A G Dore, D V Corcoran and I C Scotchman • Geological and geochemical consequences of basin exhumation, and commercial implications, L C Price • Diagenesis and fluid flow in response to uplift and exhumation, J Parnell • Uplift-related hydrocarbon accumulations: the release of natural gas from groundwater, B Cramer, S Schlomer and H S Poelchau • Depressurization of hydrocarbon-bearing reservoirs in exhumed basin settings: evidence from Atlantic margin and borderland basins, D V Corcoran and A G Dore
    Type of Medium: Monograph available for loan
    Pages: 494 S. , Ill., graph. Darst., Kt.
    ISBN: 1862391122
    Series Statement: Geological Society special publication 196
    Classification: A.3.7.
    Location: Reading room
    Branch Library: GFZ Library
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  • 2
    Call number: M 05.0239/1-2
    Pages: Vol. 1-2
    ISBN: 1862391645
    Classification: A.3.5.
    Branch Library: GFZ Library
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  • 3
    Unknown
    Weinheim [u.a.] : VCH
    Call number: 96.0485
    Pages: xvi, 161 S.
    ISBN: 3527293337
    Classification: E.7.
    Language: English
    Branch Library: GFZ Library
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  • 4
    Monograph available for loan
    Monograph available for loan
    London : The Geological Society
    Associated volumes
    Call number: 9/M 07.0421(306)
    In: Geological Society special publication
    Type of Medium: Monograph available for loan
    Pages: Auch online verfügbar
    ISBN: 1862392617 , 978-1-86239-261-8
    Series Statement: Geological Society special publication 306
    Classification: A.3.4.
    Location: Reading room
    Branch Library: GFZ Library
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  • 5
    Monograph available for loan
    Monograph available for loan
    Bologna : Zanichelli
    Call number: O 2113 / Regal 12
    Type of Medium: Monograph available for loan
    Pages: 387 S. : graph. Darst.
    Location: Magazine - must be ordered
    Branch Library: GFZ Library
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  • 6
    Call number: 9/M 07.0421(470)
    In: Geological Society Special Publication
    Description / Table of Contents: Fifty years ago, Tuzo Wilson published his paper asking ‘Did the Atlantic close and then re-open?’. This led to the ‘Wilson Cycle’ concept in which the repeated opening and closing of ocean basins along old orogenic belts is a key process in the assembly and breakup of supercontinents. The Wilson Cycle underlies much of what we know about the geological evolution of the Earth and its lithosphere, and will no doubt continue to be developed as we gain more understanding of the physical processes that control mantle convection, plate tectonics, and as more data become available from currently less accessible regions. This volume includes both thematic and review papers covering various aspects of the Wilson Cycle concept. Thematic sections include: (1) the Classic Wilson v. Supercontinent Cycles, (2) Mantle Dynamics in the Wilson Cycle, (3) Tectonic Inheritance in the Lithosphere, (4) Revisiting Tuzo's question on the Atlantic, (5) Opening and Closing of Oceans, and (6) Cratonic Basins and their place in the Wilson Cycle.
    Type of Medium: Monograph available for loan
    Pages: vi, 490 Seiten , Illustrationen, 1 Karte
    ISBN: 978-1-78620-383-0
    Series Statement: Geological Society Special Publication 470
    Language: English
    Location: Reading room
    Branch Library: GFZ Library
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  • 7
    Description / Table of Contents: Increasingly, researchers have reported that passive margins do not show a simple uninterrupted thermal sag pattern of post-rift subsidence following continental separation. Rather, the structural and stratigraphic development of such margins may record evidence of complex phases of differential subsidence, exhumation and fold development. Some of the fold structures observed on passive continental margins appear to be related to regional stresses transmitted through basement rocks, whereas others are related to gravitational sliding and toe-thrusting. This special publication concentrates on the first of these categories. The morphology and distribution of such folds, together with potential mechanisms for generation of regional stress, are described in a series of papers by authorities in the field. As well as being an enigmatic feature of passive margin geology, the compressive folds have significance in the exploration for petroleum.
    Pages: Online-Ressource (VIII, 220 Seiten)
    ISBN: 9781862392618
    Language: English
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  • 8
    Keywords: Wilson Cycle ; plate tectonics
    Description / Table of Contents: Introduction --- Fifty years of the Wilson Cycle concept in plate tectonics: an overview / R. W. Wilson, G. A. Houseman, S. J. H. Buiter, K. J. W. McCaffrey and A. G. Doré / Geological Society, London, Special Publications, 470, 1-17, 25 July 2019, https://doi.org/10.1144/SP470-2019-58 --- The Classic Wilson v. Supercontinent Cycles --- The classic Wilson cycle revisited / Ian W. D. Dalziel and John F. Dewey / Geological Society, London, Special Publications, 470, 19-38, 9 February 2018, https://doi.org/10.1144/SP470.1 --- Supercontinents: myths, mysteries, and milestones / Daniel Pastor-Galán, R. Damian Nance, J. Brendan Murphy and Christopher J. Spencer / Geological Society, London, Special Publications, 470, 39-64, 8 May 2018, https://doi.org/10.1144/SP470.16 --- Supercontinents and the case for Pannotia / R. Damian Nance and J. Brendan Murphy / Geological Society, London, Special Publications, 470, 65-86, 1 March 2018, https://doi.org/10.1144/SP470.5 --- Mantle Dynamics in the Wilson Cycle --- Mantle plumes and mantle dynamics in the Wilson cycle / Philip J. Heron / Geological Society, London, Special Publications, 470, 87-103, 19 November 2018, https://doi.org/10.1144/SP470-2018-97 --- Tectonic Inheritance in the Lithosphere --- Tectonic inheritance, structure reactivation and lithospheric strength: the relevance of geological history / A. M. C. Şengör, Nalan Lom and Nurbike G. Sağdıç / Geological Society, London, Special Publications, 470, 105-136, 15 March 2018, https://doi.org/10.1144/SP470.8 --- Exploring the theory of plate tectonics: the role of mantle lithosphere structure / Philip J. Heron, Russell N. Pysklywec and Randell Stephenson / Geological Society, London, Special Publications, 470, 137-155, 1 March 2018, https://doi.org/10.1144/SP470.7 --- Potential role of lithospheric mantle composition in the Wilson cycle: a North Atlantic perspective / Pauline Chenin, Suzanne Picazo, Suzon Jammes, Gianreto Manatschal, Othmar Müntener and Garry Karner / Geological Society, London, Special Publications, 470, 157-172, 6 March 2018, https://doi.org/10.1144/SP470.10 --- Rheological inheritance: lessons from the Death Valley region, US Basin and Range Province / Rodrigo D. Lima, Nicholas W. Hayman and Elena Miranda / Geological Society, London, Special Publications, 470, 173-204, 21 May 2018, https://doi.org/10.1144/SP470.14 --- Multi-phase reactivations and inversions of Paleozoic–Mesozoic extensional basins during the Wilson cycle: case studies from the North Sea (UK) and the Northern Apennines (Italy) / Vittorio Scisciani, Stefano Patruno, Enrico Tavarnelli, Fernando Calamita, Paolo Pace and David Iacopini / Geological Society, London, Special Publications, 470, 205-243, 3 May 2019, https://doi.org/10.1144/SP470-2017-232 --- Revisiting Tuzo's question on the Atlantic --- Examining the influence of tectonic inheritance on the evolution of the North Atlantic using a palinspastic deformable plate reconstruction / Bridget E. Ady and Richard C. Whittaker / Geological Society, London, Special Publications, 470, 245-264, 19 March 2018, https://doi.org/10.1144/SP470.9 --- Role of Avalonia in the development of tectonic paradigms / J. Brendan Murphy, R. Damian Nance, J. Duncan Keppie and Jaroslav Dostal / Geological Society, London, Special Publications, 470, 265-287, 23 March 2018, https://doi.org/10.1144/SP470.12 --- Diachronous Paleozoic accretion of peri-Gondwanan terranes at the Laurentian margin / John W. F. Waldron, David I. Schofield and J. Brendan Murphy / Geological Society, London, Special Publications, 470, 289-310, 29 March 2018, https://doi.org/10.1144/SP470.11 --- Inversion of Taconian extensional structures during Paleozoic orogenesis in western Newfoundland / Shawna E. White and John W. F. Waldron / Geological Society, London, Special Publications, 470, 311-336, 6 June 2018, https://doi.org/10.1144/SP470.17 --- Tectonic inheritance at multiple scales during more than two complete Wilson cycles recorded in eastern North America / William A. Thomas / Geological Society, London, Special Publications, 470, 337-352, 9 February 2018, https://doi.org/10.1144/SP470.4 --- Late Paleozoic extensional reactivation of the Rheic–Rhenohercynian suture zone in SW England, the English Channel and Western Approaches / Andrew C. Alexander, Robin K. Shail and Brian E. Leveridge / Geological Society, London, Special Publications, 470, 353-373, 4 January 2019, https://doi.org/10.1144/SP470.19 --- Opening and Closing of Oceans --- Non-Wilsonian break-up predisposed by transforms: examples from the North Atlantic and Arctic / E. R. Lundin and A. G. Doré / Geological Society, London, Special Publications, 470, 375-392, 21 February 2018, https://doi.org/10.1144/SP470.6 --- The Jan Mayen microplate complex and the Wilson cycle / Christian Schiffer, Alexander Peace, Jordan Phethean, Laurent Gernigon, Ken McCaffrey, Kenni D. Petersen and Gillian Foulger / Geological Society, London, Special Publications, 470, 393-414, 1 February 2018, https://doi.org/10.1144/SP470.2 --- The subduction initiation stage of the Wilson cycle / Robert Hall / Geological Society, London, Special Publications, 470, 415-437, 19 February 2018, https://doi.org/10.1144/SP470.3 --- 3D numerical modelling of the Wilson cycle: structural inheritance of alternating subduction polarity / Stéphane J. Beaussier, Taras V. Gerya and Jean-Pierre Burg / Geological Society, London, Special Publications, 470, 439-461, 2 May 2018, https://doi.org/10.1144/SP470.15 --- Cratonic Basins and their place in the Wilson Cycle --- Cratonic basins and the Wilson cycle: a perspective from the Parnaíba Basin, Brazil / M. C. Daly, B. Tozer and A. B. Watts / Geological Society, London, Special Publications, 470, 463-477, 3 May 2018, https://doi.org/10.1144/SP470.13
    Pages: Online-Ressource (VI, 490 Seiten) , Illustrationen, Diagramme
    ISBN: 9781786203830
    Language: English
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  • 9
    Publication Date: 2001-01-01
    Description: The Mesozoic history of a number of Atlantic borderland sedimentary basins can be related to the early opening history of the southern North Atlantic Ocean. Regional tectonic controls such as plate motion vectors and the pre-existing tectonic grain had an important role in basin development and are expressed as local tectonostratigraphic events. The evolving palaeogeographies for the region are demonstrated in a series of maps based on computer-generated plate reconstructions. The Porcupine Basin, centrally located in the study area, lay close to the intersection of three plate boundaries that separated Eurasia from North America and controlled opening of the Bay of Biscay. The south Porcupine Basin, where there is relatively poor data control, is considered in the context of broader platetectonic controls, which were also responsible for the development of contiguous and better understood basins during Mesozoic time. This approach provides new insight into the structural evolution and likely facies development in the south Porcupine Basin, allowing broad inferences for petroleum prospectivity to be made. Initial Permo-Triassic fault-controlled extension led to continental deposition, which, if associated with aeolian and/or fluvial reservoir rocks, will mostly be too deep to be prospective. Thermal subsidence during Early Jurassic time was associated with flooding and fine-grained clastic deposition with anticipated moderate source rock potential. Regional uplift of the northern Porcupine area during Mid-Jurassic time forced shorelines and shelves southwards and the south Porcupine Basin could contain good reservoir quality sandstones and possible waxy deltaic-type source rocks of this age. In Late Jurassic time, major crustal extension took place with potential for reservoir and source rocks in locally expanded footwall successions. Further extensional faulting occurred in earliest Cretaceous (Neocomian) time with further synrift plays possible at this level. Growth of the Porcupine Median Volcanic Ridge is attributed to Barremian-Aptian time and related to continuing extension associated with a northwesterly arm of a triple junction positioned to the south of the Porcupine area. Strong subsidence of the basin centre during this time will have a significant impact on source rock maturation and flank trap geometries in the south Porcupine Basin.
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  • 10
    Publication Date: 2002-01-01
    Description: Uplift, erosion and removal of overburden have profound effects on sedimentary basins and the hydrocarbon systems they contain. These effects are predictable from theory and from observation of explored exhumed basins. Exhumed basins are frequently evaluated in the same way as normal' subsiding basins, leading to errors and unrealistic expectations. In this paper we discuss the consequences of exhumation in terms of prospect risk analysis, resource estimation, and overall basin characteristics. Exhumation should be taken into account when assigning risk factors used to estimate the probability of discovery for a prospect. In general, exhumation reduces the probability of trapping or sealing hydrocarbons, except where highly ductile seals such as evaporites are present. Exhumation modifies the probability of reservoir in extreme cases; for example, where a unit may have been buried so deeply before uplift that it is no longer an effective reservoir, or where fracturing on uplift may have created an entirely new reservoir. The probability of sourcing or charging is affected by multiple factors, but primarily by the magnitude of the post-exhumation hydrocarbon budget and the efficiency of remigration. Generally gas will predominate as a result of methane liberation from oil, formation water and coal, and because of expansion of gas trapped before uplift. These factors in combination tend to result in gas flushing of exhumed hydrocarbon basins. Compared with a similar prospect in a non-exhumed basin, resource levels of a prospect in an exhumed basin are generally lower. Higher levels of reservoir diagenesis influence the standard parameters used to calculate prospect resources. Porosity, water saturation and net-to-gross ratio are adversely affected, and (as a consequence of all three) lower recovery factors are likely. Hydrostatic or near-hydrostatic fluid pressure gradients (as observed in exhumed NE Atlantic margin basins) will also reduce the recovery factor and, in the case of gas, will adversely affect the formation volume factor. Hydrocarbon systems in exhumed settings show a common set of characteristics. They can include: (1) large, basin-centred gas fields; (2) smaller, peripheral, remigrated oil accumulations; (3) two-phase accumulations; (4) residual oil columns; (5) biodegraded oils; (6) underfilled traps. Many basins on the NE Atlantic seaboard underwent kilometre-scale uplift during Cenozoic time and contain hydrocarbon systems showing the effects of exhumation. This knowledge can constrain risk and resource expectation in further evaluation of these basins, and in unexplored exhumed basins.
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