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  • 1
    Call number: 9/M 02.0230
    In: Geological Society special publication
    Type of Medium: Monograph available for loan
    Pages: 473 S.
    ISBN: 1862390878
    Series Statement: Geological Society special publication 188
    Classification:
    A. 3.7.
    Location: Reading room
    Branch Library: GFZ Library
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  • 2
    Description / Table of Contents: Ireland is virtually encircled by sedimentary basins which developed in response to periods of rifting and thermal subsidence. These offshore basins have been the focus of intermittent phases of exploration since drilling of the first well in 1970 and, to date, 136 wells have been drilled. Most of the drilling so far has concentrated on structural traps, but recent exploration has begun to focus on a variety of stratigraphic traps, with greater emphasis on results obtained from studies of the Atlantic margin basins. The Petroleum Exploration of Ireland's Offshore Basins contains a set of 27 papers on a wide range of topics relating to recent exploration of the Irish offshore sedimentary basins. These papers address aspects of the structural and stratigraphic evolution, thermal history, petroleum systems, reservoir geology and sea-bed processes in the Irish offshore area. Although the main focus is on petroleum systems and those issues bearing on exploration risk, the exploration effort has yielded fundamental new insight into the wider development of starved passive continental margins. The volume will be of interest to oil industry explorationists and researchers focusing on NW European sedimentary basins and the evolution of the Irish Atlantic margin.
    Pages: Online-Ressource (473 Seiten)
    ISBN: 1862390878
    Language: English
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  • 3
    Publication Date: 2001-01-01
    Description: Regional structural synthesis together with 2D forward and reverse flexural isostatic basin modelling techniques have been used to investigate the extensional and subsidence history of the southern part of the Porcupine Basin. Two structural interpretations of seismic line GSP97-19 have been considered: (1) a Mid-Late Jurassic rift basin based upon seismic interpretation of well-defined tilted fault blocks, with subsidence modelling of the thick overlying sediment section predicting high lithosphere stretching factors of up to {beta} = 6; (2) a Mid-Jurassic-Early Cretaceous rift responsible for a thick Barremian-Aptian synrift sequence within the basin centre resulting in reduced maximum lithospheric stretching factors of {beta} = 2.3. The variance in published estimates of crustal thickness beneath the basin cannot distinguish between these scenarios. A comparison between stretching factors and the amount of observable upper-crustal faulting suggests that depth-dependent lithospheric stretching may be a feature of the basin, as in other sedimentary basins along the Atlantic margin, and is directly associated with the onset of Cretaceous plate break-up in the Atlantic.
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  • 4
    Publication Date: 2002-01-01
    Description: Depressurization of reservoirs in petroliferous basins commonly occurs through cap-rocks at structural crests where pore pressures are locally elevated because of either the presence of a hydrocarbon column or the redistribution of overpressures by water flow along laterally extensive inclined permeable aquifers. In exhumed petroliferous basins this deflation of excess pore pressures is enhanced by the denudation process, which results in the large-scale removal of overburden during regional uplift. Evidence from the exhumed basins of the Atlantic margin indicates that hydrocarbon accumulations in these basins are commonly characterized by underfilled traps and hydrostatically pressured or modestly overpressured reservoirs. These observations are reviewed in the context of the generic mechanisms by which top-seals leak, the properties of cap-rocks and the physical processes that occur during exhumation. Water-wet shaly cap-rocks can form a capillary seal to a hydrocarbon column while simultaneously accommodating brine flow and equilibration of pressures between the reservoir and the top-seal. In contrast, thick, low-permeability shale or evaporite sequences may form pressure seals that restrict vertical brine and hydrocarbon flow and prevent the equilibration of aquifer pressures above and below the seal. In any sedimentary basin, the presence of regional pressure seals can result in a layered hydrogeological regime with hydrostatically pressured strata decoupled from over- or underpressured cells. Recently exhumed basins typically show limited overpressuring and in a number of these basins underpressured reservoirs have been described. Post-exhumation overpressure generation is primarily driven by tectonic compression, aquathermal pressuring and hydraulic head. The fluid retention capacity of any cap-rock lithology during exhumation is dependent upon the physical and mechanical characteristics of the cap-rock at the time of exhumation and the timing and conditions of the associated deformation relative to the timing of hydrocarbon emplacement. The permeability and deformational characteristics of halite render it an excellent cap-rock with a high retention capacity, even under conditions of exhumation. However, mudrocks may also form effective cap-rocks in exhumed basins when the deformation associated with exhumation occurs before embrittlement and the shale cap-rock exhibits ductile behaviour. Shale and evaporite cap-rocks form the main regional seals to hydrocarbon accumulations in exhumed basins of the Atlantic margin and borderlands. Syn-exhumation top-seal efficiency (fluid retention capacity) is a major exploration risk in these basins, although post-exhumation top-seal integrity in these basins may be relatively high under certain conditions. Consequently, a major exploration risk factor in exhumed basin settings pertains to the limited hydrocarbon budget available post-regional uplift and the efficiency of the remigration process.
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  • 5
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    In:  Geological Society Special Publication 188: 1-8.
    Publication Date: 2001-01-01
    Description: Ireland is virtually encircled by sedimentary basins (Fig. 1) that developed in response to a series of rift episodes interspersed with periods of thermal subsidence. A number of inversion episodes also played a role in the development of sediment source areas and in the structuring of the basins. These basins can be categorized into two groups. The first comprises the basins of Northern Ireland, the Irish Sea and Celtic Sea areas, and the inboard basins (Slyne, Erris and Donegal basins) of the Atlantic margin. They generally have a NE-SW elongate morphology and typically lie within 100km of the shore. Their sedimentary fill is predominantly of pre-Tertiary age and they have no major bathymetric expression. The second group, comprising the outboard basins of the Atlantic margin (Goban Spur, Porcupine, Rockall and Hatton basins), lies in deep water. These basins are characterized by having an extensive surface area, typically containing a predominantly Cretaceous and Tertiary succession and having an underfilled sedimentary character. The Irish offshore basins have been the focus of intermittent phases of exploration since the first well was drilled in 1970. To date, a total of 136 wells has been drilled (Fig. 2) with 37 of these in the basins west of Ireland. The total cost of wells in the Irish offshore, in 2001 prices, is approximately IR {pound}1500 million. A significant amount of 2D reflection seismic data has been acquired (Fig. 3), both as speculative and proprietary surveys. Two commercial gas fields (Kinsale Head and Ballycotton) are currently in ... This 250-word extract was created in the absence of an abstract.
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  • 6
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    In:  Geological Society Special Publication 188: 61-90.
    Publication Date: 2001-01-01
    Description: Vitrinite reflectance (VR) data (Rm%) have been compiled from 77 Irish offshore wells and 17 onshore boreholes. This database has facilitated the analysis of vitrinite reflectance v. depth relationships by both basin and stratigraphic interval. In general, VR gradients from the Carboniferous sections are defined by less scattered trends than those from Mesozoic and Cenozoic sections, reflecting the less complex vitrinite populations within Carboniferous coals and shales. A composite approach (display of profiles from a number of wells together) to the interpretation of vitrinite reflectance profiles has been utilized to characterize the thermal history and the prevalent heat transfer mechanisms within the various basins. Calculated peak palaeotemperatures from the wells are used to compute palaeogeothermal gradients and to estimate the magnitude of net exhumation at selected locations. Average palaeogeothermal gradients in the onshore Carboniferous basins range from less than 3{degrees}C km-1 at well IIP-2 in the Clare Basin to 119{degrees}C km-1 at well N998 in the Navan area of the Dublin Basin. Lateral variations in palaeogeothermal gradients recorded in the Carboniferous sections are consistent with a gravity-driven hydrothermal system discharging heated fluids, along fault systems, in a foreland platform area. In general, palaeogeothermal gradients are substantially higher in the Carboniferous sections (mean 60{degrees}C km-1) than in the Mesozoic or Cenozoic sections (mean 32{degrees}C km-1). Maturation levels in many of the Carboniferous sections are considered to be the consequence of burial, elevated heat flows and a regional advective system during late Carboniferous to early Permian times rather than Mesozoic or Cenozoic processes. Empirically derived methods of calculating peak palaeotemperature from VR are compared with kinetic models and, although differing in detail, within the resolution of this dataset are shown to produce similar trends. There is a considerable body of evidence to suggest that the extensional evolution of Ireland's Late Palaeozoic to Cenozoic sedimentary basins has been punctuated by a multiphase inversion history. Regional stratigraphic evidence, combined with VR and apatite fission-track data, suggests at least two periods of pervasive exhumation occurred; one during Late Carboniferous-Late Permian time and another during Tertiary time. Both of these phases are characterized by a component of compressional inversion and the widespread occurrence of extrusive and intrusive igneous rocks. However, the contrasting thermal signature of these regional uplift events suggests that both the basin setting and the mechanism of regional exhumation exerted a fundamental control on processes that determined heat flow distribution within a basin. In terms of the hydrocarbon exploration of Ireland's sedimentary basins the model presented here has important implications for the timing of maturation of Carboniferous source rocks in these basins. Where Carboniferous source rocks are present, they will make a significant contribution to the hydrocarbon budget only in those basins that experienced relatively low heat flow during Late Carboniferous-Early Permian time and where sufficient Mesozoic burial has occurred to subsequently expose the kerogen to higher temperatures. This observation is consistent with the presence of gas accumulations, which are postulated to have been derived from Carboniferous source rocks, in both the Slyne Basin and the Northwest Carboniferous Basin.
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  • 7
    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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  • 8
    Publication Date: 2016-01-27
    Description: Petroleum (oil and gas) forms from the bacterial or thermal breakdown of kerogen during progressive burial in sedimentary basins. During times of petroleum generation, kerogens in organic-rich source rocks expel petroleum to form a fluid phase in the pore system, capable of migrating under hydrodynamic and buoyancy forces to ultimately escape to the surface or accumulate within petroleum traps in the subsurface. The relative timing of petroleum charge and trap formation is a vital component in the accumulation of petroleum deposits. Exhumed basins have been historically viewed as higher-risk targets for conventional petroleum exploration because of, inter alia, the switch-off of petroleum generation in the source rock at the commencement of cooling during exhumation. However, even at the switch-off point, the source rock may retain a significant volume of petroleum sorbed in kerogen and within its pore system. Herein we demonstrate that if the source rock is exhumed to shallower depths after peak burial, pore pressure reduction and the associated volumetric expansion of the petroleum—particularly of the gaseous—phase in the pore system will result in the discharge of additional petroleum into the adjacent carrier bed or reservoir formations. Because most onshore sedimentary basins are characterized by major exhumation events at some point in their history, this represents an additional and underappreciated mechanism for a late-stage petroleum charge in exhumed sedimentary basins. The modeling also indicates that both the initial, pre-exhumation, total gas storage capacity and the exhumation gas charge are likely to be volumetrically more significant for gas-bearing source rocks that have been exposed to higher initial pressures and lower thermal gradients. The concepts presented here also have implications for petroleum resources retained within unconventional shale reservoirs because high-graded shale plays may be associated with systems where the magnitude or rate of relative overpressure dissipation has limited exhumation charge from the unconventional to conventional reservoirs within the basin.
    Print ISSN: 0149-1423
    Electronic ISSN: 0149-1423
    Topics: Geosciences
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  • 9
    Publication Date: 2016-04-21
    Description: Intracratonic sag basins commonly have relatively simple tectonic histories; however, later tectonic activity involving exhumation can make reconstructing the burial history a challenging task. This is important because the relative timing of hydrocarbon generation and trap formation can be a key factor in risk assessment. If trap formation postdates peak hydrocarbon generation, exploration plays are typically downgraded. Mechanisms for charge in such exhumed basins are critical factors for understanding exploration risk. This study uses data collected from an Ordovician gas-condensate field in the Illizi Basin of Algeria to document the charging of a trap formed, or modified, during exhumation of the basin following maximum burial. Integrated analysis of sonic compaction data, thermal history indicators, and stratigraphic well data was used to constrain the burial and thermal history of the region. Hydrocarbon generation in the lower Silurian source rock is interpreted to have occurred during the Carboniferous (prior to Hercynian exhumation) and during the Late Cretaceous–early Eocene maximum burial (prior to Eocene exhumation). Structural reconstructions indicate that the field was initially located on the southern flank of a long-lived, intrabasinal, Paleozoic paleohigh. The large, low-relief structural closure that defines the present-day accumulation formed as a result of northward tilting of the Illizi Basin during Eocene uplift of the Hoggar massif. The study demonstrates that the timing of trap formation at the Ordovician field postdates the main local hydrocarbon generation events within the basin, suggesting that alternative hydrocarbon charge mechanisms are required. This study indicates considerable potential to charge updip traps on the flanks of exhumed petroliferous basins via redistribution of the preexisting hydrocarbons within the basin.
    Print ISSN: 0149-1423
    Electronic ISSN: 0149-1423
    Topics: Geosciences
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  • 10
    Publication Date: 2005-03-01
    Print ISSN: 1354-0793
    Electronic ISSN: 2041-496X
    Topics: Chemistry and Pharmacology , Geosciences
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