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  • 1
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: The Campanian Cliff House Formation represents a series of individually progradational shoreface tongues preserved in an overall landward-stepping system. In the Mancos Canyon area, the formation consists of four, 50- to 55-m-thick and 10- to 20-km-wide sandstone tongues, which pinch out landwards into lower coastal plain and lagoonal deposits of the Upper Menefee Formation and seawards into offshore shales of the Lewis Shale Formation. Photogrammetric mapping of lithofacies along the steep and well-exposed canyon walls was combined with sedimentary facies analysis and mapping of the detailed facies architecture. Two major facies associations have been identified, one comprising the mostly muddy and organic-rich facies of lagoonal and lower coastal plain origin and one comprising the sandstone-dominated facies of shoreface origin. Key stratigraphic surfaces were identified by combining the mapped geometry of the lithofacies units with the interpretation of depositional processes. The stratigraphic surfaces (master ravinement surface, shoreface/coastal plain contact, transgressive surface, maximum flooding surface and the sequence boundary) allow each major sandstone tongue to be divided into a simple sequence, consisting of a basal transgressive system tract (TST) overlain by a highstand system tract (HST). Within each sandstone tongue, a higher frequency cyclicity is evident. The high-frequency cycles show a complex stacking pattern development and are commonly truncated in the downdip direction by surfaces of regressive marine erosion. The complexities of the Cliff House sandstone tongues are believed to reflect changes in the rate of sea-level rise combined with the responses of the depositional system to these changes. Synsedimentary compaction, causing a thickness increase in the sandstone tongues above intervals of previously uncompacted lagoonal/coastal plain sediments, also played a role. This study of the facies architecture, geometry and sequence stratigraphy of the Cliff House Formation highlights the fact that there may be some problems in applying conventional sequence stratigraphical methods to landward-stepping systems in general. These difficulties stem from the fact that no single stratigraphic surface can easily be identified and followed from the non-marine to the fully marine realm (i.e. from the landward to the basinward pinch-out of the sandstone tongues). In addition, the effects of synsedimentary compaction and changes in the shoreface dynamics are not easily recognized in limited data sets such as from the subsurface.
    Type of Medium: Electronic Resource
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  • 2
    Publication Date: 2005-07-01
    Description: This article illustrates a successful methodology used to screen a series of deep-marine depositional systems in the gigantic (〉180,000-km2; 〉69,500-mi2) Vøring and Møre basins, offshore mid-Norway. Seismic and well data have been integrated with architectural information from selected outcrop analogs from the Delaware basin in United States and the Ainsa basin in Spain to describe the three-dimensional depositional geometries of the deep-water sedimentary systems. The examples presented document the large variability in geometry and size by illustrating seismic facies and sequences of deep-marine fan systems in the Vøring and Møre basins. The main architectural elements are (1) basin-floor deposits characterized by constructional processes such as sheet sands and lobe forms; (2) canyons and channels with several phases of infill; and (3) slope accommodation deposits governed by the topography with a variety of infilling stratigraphic architectures. Offshore mid-Norway, the distance to sediment provenance area varies between tens and hundreds of kilometers for the deep-marine systems, and the basin-floor deposits cover up to several thousands of square kilometers. However, insight into the lithofacies distribution and architectural features of different scales seen in outcrop and subsurface data suggest that common depositional processes may be involved regardless of scale differences across a deep-water profile. In frontier basins, sand prediction will be regional in scale, and the applied methodology is a very useful screening tool to predict what part of the deep-water basin is most likely to be sand prone and also the ultimate reservoir quality. Edith M. G. Fugelli received an M.Sc. degree in sedimentology from the University of Oslo, Norway, in 1987. She has worked for the Norwegian Petroleum Directorate and Statoil and joined BP Norway in 2001, where she is currently working as a senior regional geologist. Her interests are sequence and seismic stratigraphy, paleotectonic influences on depositional systems, and outcrop to seismic-defined reservoir characterization.Tina R. Olsen received her M.Sc. degree from the University of Copenhagen, Denmark, in 1993 and her Ph.D. from the University of Bergen, Norway, in 1996. She joined Amoco in 1996 and is currently working as a senior reservoir geologist with BP Norge in Stavanger, Norway. Olsen specializes in sedimentology and stratigraphy and her areas of expertise cover exploration, development, and production geology on the Norwegian continental shelf.
    Print ISSN: 0149-1423
    Electronic ISSN: 1943-2674
    Topics: Geosciences
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  • 3
    Publication Date: 2005-07-01
    Description: This article documents the methodology and results of a risk analysis for seven plays in the frontier Møre and Vøring basins. The play types represent different deep-marine systems and span a complete transect from upper slope to basin floor. Because of the sparse well data coverage typical of frontier basins, the play models are seismically driven, resulting in high-level qualitative risk assessments, dividing the plays into low-, medium-, and high-risk categories. The objectives of the risk assessment were both to develop an understanding of the distribution of promising reservoir thickness, architecture, and net to gross in each play type and, further, to evaluate the range of uncertainties of the depositional model and the quality of the available database. We demonstrate here how the effect of perceptions of risk in constituting a valid play can be evaluated during the ranking process and how the process can be used to systematically screen for future exploration opportunities. The workflow is rooted in a risk analysis of the geological models because this represents an integrated interpretation of the geology with respect to reservoir distribution, architecture, and presence of seal. In conclusion, the prerequisites for proper qualitative risk assessment of geological models are an awareness of reservoir variability and the range of depositional attributes. Play risk consists of regional risk elements, determined by regional depositional models. Equally important is the uncertainty introduced by poor or lacking data. Differentiating between play risk and lack of data improved decision making, i.e., whether to acquire acreage, data, or both. Edith M. G. Fugelli received an M.Sc. degree in sedimentology from the University of Oslo, Norway, in 1987. She has worked in the Norwegian Petroleum Directorate and Statoil and joined BP Norge in 2001, where she is currently working as a senior regional geologist. Her interests are sequence and seismic stratigraphy, paleotectonic influences on depositional systems, and outcrop to seismic-defined reservoir characterization.Tina R. Olsen received her M.Sc. degree from the University of Copenhagen, Denmark, in 1993 and her Ph.D. from the University of Bergen, Norway, in 1996. She joined Amoco in 1996 and is currently working as a senior reservoir geologist with BP Norge in Stavanger, Norway. Olsen specializes in sedimentology and stratigraphy and her areas of expertise cover exploration, development, and production geology on the Norwegian continental shelf.
    Print ISSN: 0149-1423
    Electronic ISSN: 1943-2674
    Topics: Geosciences
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  • 4
    Publication Date: 2007-11-01
    Description: The Dønna Terrace is part of the morphologically complex continental slope offshore mid-Norway and contains a series of tectonically confined subbasins. These subbasins all have different sizes, shapes, and locations that strongly controlled the development of the deep-marine, Upper Cretaceous Lysing Formation. Careful mapping of the entrance points and internal faults within each subbasin is crucial for constructing a depositional model for these slope turbidite complexes. The key to successful delineation of the turbidite systems and complexes in the study area is a four-step process: (1) understanding the main structural elements on a semiregional scale; (2) mapping all structural features in detail that can impact the sediment fill within and prior to the studied interval to build a structural framework of the area; (3) performing a thorough integration of seismic, biostratigraphy, wire-line, core, and formation-pressure data for each subbasin, identifying the geometry and reservoir architecture of turbidite systems and complexes; and (4) developing a sequence-stratigraphic framework to establish if the deep-marine sedimentary fill of the subbasins is genetically linked. The importance of establishing a genetic linkage between slope basins is related to the reservoir quality of the deep-marine turbidite systems; if a cannibalization of a sandstone-dominated sedimentary fill of an updip slope basin can be demonstrated, lower risk can be assigned for reservoir quality of lower-slope-basin reservoirs. In addition, onlap style and pinch-out character of the turbidite systems yield important information of sand deposition within the turbidite systems. Edith M. G. Fugelli received a Cand. Scient. degree in sedimentology from the University of Oslo, Norway, in 1987. She has worked in the Norwegian Petroleum Directorate and Statoil and joined BP Norway in 2001 as a senior regional geologist. Her interests are sequence and seismic stratigraphy and integration of different geodisciplines in exploration and outcrop to seismic-defined reservoir characterization. Tina R. Olsen received a Ph.D. in petroleum geology from the University of Bergen, Norway, in 1996. She worked for Amoco and BP Norway from 1996 to June 2006, when she joined Gaz de France as an area exploration leader. Olsen specializes in sedimentology and stratigraphy, and her areas of expertise cover exploration, development, and production geology on the Norwegian Continental Shelf.
    Print ISSN: 0149-1423
    Electronic ISSN: 1943-2674
    Topics: Geosciences
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  • 5
    Publication Date: 1999-08-01
    Print ISSN: 0037-0746
    Electronic ISSN: 1365-3091
    Topics: Geosciences
    Published by Wiley
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  • 6
    Publication Date: 2000-01-01
    Print ISSN: 0305-8719
    Electronic ISSN: 2041-4927
    Topics: Geosciences
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