PK
b"@ refs.MYD
? Bridge, J.S.
Tye, R.S. 2000u Interpreting the dimensions of ancient fluvial channel bars, channels, and channel belts from wireline-logs and cores 1205-12285 American Association of Petroleum Geologists Bulletin 84 8- case-studies; channels-; clastic-rocks; Colorado-; Comanchean-; conglomerate-; cores-; Cretaceous-; fluvial-environment; lithofacies-; Lower-Cretaceous; Mesaverde-Group; Mesozoic-; models-; modern-analogs; North-Appleby-Field; oil-and-gas-fields; petroleum-; petroleum-exploration; Piceance-Creek-basin; planar-bedding-structures; reservoir-rocks; sand-bodies; sandstone-; sedimentary-rocks; sedimentary-structures; Texas-; Travis-Peak-Formation; United-States; Upper-Cretaceous; well-logs; Economic-geology,-geology-of-energy-sources; Sedimentary-petrology Clastic sedimentology A primary objective in exploration for and development of fluvial reservoirs is determining the thickness and width of sandstone-conglomerate bodies (mainly channel-belt deposits). Most of the existing techniques for estimating the dimensions of fluvial reservoirs have major drawbacks. A fresh approach to the problem is made using recent theoretical, experimental, and field studies. This new approach involves (1) new models for the lateral and vertical variation of lithofacies and petrophysical-log response of river-channel deposits with explicit recognition of the different superimposed scales of strata, (2) distinction among single and superimposed channel bars, channels, and channel belts, (3) interpretation of maximum paleochannel depth from the thickness of channel bars and the thickness of sets of cross-strata formed by dunes, and (4) evaluation of various methods for estimation of widths of sandstone-conglomerate bodies that represent either single or connected channel belts (outcrop analogs; correlation of sandstone-conglomerate bodies between wells; use of empirical equations relating channel depth, channel width, and channel-belt width; theoretical models; and three-dimensional seismic data). Two fluvial reservoirs were reinterpreted using this new approach. In the first example from the Mesaverde Group, Colorado, maximum paleochannel depth had been underestimated because the degree of superposition of channel bars had been overestimated. As a result, channel-belt widths determined from empirical equations were underestimated. In the second example from the Travis Peak Formation, Texas, channel-belt width and connectivity of channel-belt sandstone bodies had been overestimated because of overzealous well-to-well correlation and inappropriate use of width and thickness data from supposed analogs. These examples demonstrate the potential value of this new approach in reservoir characterization and management. Generic Generic? Allen, J. R. L. 1978 Studies in fluviatile sedimentation; an exploratory quantitative model for the architecture of avulsion-controlled alluvial sites 129-147 Sedimentary Geology 21 2 alluvium-; avulsion-; changes-; channels-; clastic-sediments; coastal-plains; drainage-patterns; experimental-studies; fluvial-features; geomorphology-; mathematical-models; models-; physical-models; planar-bedding-structures; processes-; rivers-; sand-bodies; sedimentary-structures; sedimentation-; sediments-; stream-transport; theoretical-studies; transport-; Sedimentary-petrology Clastic sedimentology Generic Generic7 internal-pdf://Allen (1978)-0775222550/Allen (1978).pdf h? Kędzior, A 2001 Identification of the fluvial-channel tracts based on thickness analysis: Zabrze beds (Namurian B) in the main anticline and Bytom-Dąbrowa trough of Upper Silesia coal basin, Poland. 21-34' Annales Societatis Geologorum Poloniae 71 1 Clastic sedimentology Poland
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? o $ Aitken, J.F.
Quirk, D.G.
Guion, P.D. 1999p Regional correlation of Westphalian sandbodies onshore UK; implications for reservoirs in the southern North Sea 747-756I Petroleum Geology of North-West Europe: Proceedings of the 5th Conference Fleet, A.J.
Boldy, S.A.R. London The Geological Society% Atlantic-Ocean; Carboniferous-; clastic-rocks; coal-; coal-fields; correlation-; England-; Europe-; geophysical-methods; Great-Britain; Lincolnshire-England; Midlands-; North-Atlantic; North-Sea; offshore-; oil-and-gas-fields; onshore-; Paleozoic-; Pennines-; petroleum-; petroleum-engineering; petroleum-exploration; reservoir-properties; reservoir-rocks; sandstone-; sedimentary-rocks; seismic-methods; southern-North-Sea; United-Kingdom; Upper-Carboniferous; well-logging; Western-Europe; Westphalian-; Economic-geology,-geology-of-energy-sources Petroleum Geology
1-86239-039-8 UK
CarboniferousG internal-pdf://Aitken et al. (1999)-3679706173/Aitken et al. (1999).pdf ? Birrel, S.
Courtier, J. 1999 Structural analysis of 3D seismic data, using the correlation attribute: a case study -Carboniferous of the Southern North Sea (UK) 789-797I Petroleum Geology of North-West Europe: Proceedings of the 5th Conference Fleet, A.J.
Boldy, S.A.R. London Geological Society London
Geophysics UK North Sea
CarboniferousO internal-pdf://Birrel & Courtier (1999)-1029285437/Birrel & Courtier (1999).pdf ? C Bramwell, N.P.
Caillet, G.
Meciani, L.
Judge, N.
Green, M.
Adam, P. 19990 Chalk exploration, the search for a subtle trap 911-937I Petroleum Geology of North-West Europe: Proceedings of the 5th Conference Fleet, A.J.
Boldy, S.A.R. London Geological Society London Petroleum Geology UK North Sea
CretaceousK internal-pdf://Bramwell et al. (1999)-0761195325/Bramwell et al. (1999).pdf ? ' Kadolsky, D.
Johansen, S.J.
Duxbury, S. 1999 Sequence stratigraphy and sedimentary history of the Humber Group (Late Jurassic-Ryazanian) in the Outer Moray Firth (UKCS, North Sea) 839-860I Petroleum Geology of North-West Europe: Proceedings of the 5th Conference Fleet, A.J.
Boldy, S.A.R. London Geological Society London Stratigraphy UK North Sea JurassicK internal-pdf://Kadolsky et al. (1999)-2390194493/Kadolsky et al. (1999).pdf # ? > Lasocki, J.
Guemene, J.M.
Hedayati, A.
Legorius, C.
Page, W.M. 1999B The Elgin and Franklin fields: UK Blocks 22/30c, 22/30b and 29/5b 1008-1020I Petroleum Geology of North-West Europe: Proceedings of the 5th Conference Fleet, A.J.
Boldy, S.A.R. London Geologica) ? o + Bartholomew, I.D.
Peters, J.M.
Powell, C.M. 1993h Regional structural evolution of the North Sea: oblique slip and the reactivation of basement lineaments 1109-1122I Petroleum Geology of North-West Europe: Proceedings of the 4th Conference 4 Parker, J.R. London The Geological Society Structural Geology North Sea GenericO internal-pdf://Bartholomew et al (1993)-3438009866/Bartholomew et al (1993).pdf? Bodenhausen, J.W.A.
Ott, W.F. 1981> Habitat of the Rijswijk oil province, onshore, the Netherlands 301-309b Petroleum Geology of the continental Shelf of North-West Europe: Proceedings of the 2nd Conference Illing, L.V.
Hobson, G.D. London Institute of Petroleum Petroleum Geology Netherlands GenericO internal-pdf://Bodenhausen & Ott (1981)-0154841856/Bodenhausen & Ott (1981).pdf ]? Bénard, F.
Bouché, P. 1991K Aspects of the petroleum geology of the Variscan foreland of Western Europe 119-137@ Generation, accumulation and production of Europe's hydrocarbons 1
Spencer, A.M. BerlinJ Special Publication of the European Association of Petroleum Geoscientists basement-; basins-; black-shale; cap-rocks; carbonate-rocks; Carboniferous-; Central-Europe; chemically-precipitated-rocks; clastic-rocks; coal-; compression-tectonics; deformation-; deltaic-environment; Devonian-; Dinantian-; distribution-; England-; Europe-; evaporites-; evolution-; faults-; foreland-basins; genesis-; geochemistry-; Germany-; Great-Britain; heat-flow; Hercynian-Orogeny; lacustrine-environment; limestone-; lithofacies-; maturity-; Midland-Valley; Namurian-; organic-residues; orogeny-; paleogeography-; Paleozoic-; petroleum-; petroleum-engineering; Poland-; possibilities-; reactivation-; reservoir-properties; sandstone-; Scotland-; sea-level-changes; sediment-supply; sedimentary-rocks; sedimentation-; shale-; siltstone-; Sole-Pit-Basin; source-rocks; subsidence-; tectonics-; Tornquist-Fault; transgression-; United-Kingdom; Upper-Carboniferous; Western-Europe; Economic-geology,-geology-of-energy-sources Petroleum Geology Western Europe
CarboniferousK internal-pdf://Benard & Bouche (1991)-2751055361/Benard & Bouche (1991).tif ? o # Besly, B.M.
Burley, S.D.
Turner, P. 1993W The Late Carboniferous "barren red bed" play of the Silver Pit area, southern North Sea 727-740I Petroleum Geology of North-West Europe: Proceedings of the 4th Conference 4 Parker, J.R. London The Geological SocietyR alluvium-; Atlantic-Ocean; Carboniferous-; clastic-rocks; clastic-sediments; natural-gas; North-Atlantic; North-Sea; Paleozoic-; petroleum-; red-beds; reservoir-rocks; sedimentary-rocks; sediments-; Silver-Pit-Basin; southern-North-Sea; Upper-Carboniferous; Westphalian-; Economic-geology,-geology-of-energy-sources; Sedimentary-petrology Petroleum Geology UK
Carboniferous ?
Cocks, L. R. M.
Torsvik, T. H. 2005d Baltica from the late Precambrian to mid-Palaeozoic times: The gain and loss of a terrane's identity 39-66 Earth Science Reviews 72 1-2J Baltica
Cambrian
Ordovician
Silurian
paleogeography
Avalonia
Iapetus Ocean Palaeogeography The old terrane of Baltica occupies the mass of northern Europe eastwards to the Urals and lies mostly to the north of the Trans-European Suture Zone. The core, the East European Craton, is thick and formed of rocks dating back to well over 3 billion yr, and Protobaltica can be identified as forming part of the supercontinent of Rodinia at about 1 billion yr ago. Following Rodinia's break up at about 800 Ma, Protobaltica remained attached to Laurentia until it became the newly independent Baltica at between 570 and 550 Ma, with the inauguration of plate spreading to form the northern part of the Iapetus Ocean. To the south, during the Early Cambrian, Baltica was separated from Gondwana by the relatively narrow Ran Ocean. Baltica remained a separate terrane until its docking, firstly with Avalonia at the very end of the Ordovician (443 Ma), and then with Laurentia during the Silurian in the Scandian part of the Caledonide Orogeny. The terrane was much enlarged in the Vendian to include the areas such as Timan-Pechora now lying to the north as they became accreted to Baltica during the late Precambrian Timanide Orogeny. During the Cambrian and Ordovician, Baltica firstly rotated through more than 120[degree sign] and then drifted northwards from high to low palaeolatitudes. New maps present Baltica's outline and progressive positioning, its late Precambrian and Lower Palaeozoic history, and the Cambrian, Ordovician and Silurian land, basins and biofacies belts within and around it. Some of the Lower Palaeozoic faunas are reviewed briefly: the oceans surrounding Baltica were so wide during the Early Ordovician that a substantial part of the benthic fauna of trilobites, brachiopods and other phyla were endemic. As those oceans narrowed, so the faunas of Baltica became progressively more similar to those of adjacent terranes. Some plankton distributions augment the palaeomagnetic data in latitudinal positioning. Europe
PalaeozoicK internal-pdf://Cocks & Torsvik (2005)-2024988728/Cocks & Torsvik (2005).pdf ? o W Collinson, J.D.
Jones, C. M.
Blackbourn, G.A.
Besly, B.M.
Archard, G. M.
McMahon, A. H. 1993<