LEADER 05829nam 2200757 450 001 9910811747703321 005 20230803203737.0 010 $a1-118-92045-7 010 $a1-118-92043-0 010 $a1-118-92044-9 035 $a(CKB)3710000000202426 035 $a(EBL)1744757 035 $a(SSID)ssj0001261871 035 $a(PQKBManifestationID)11978160 035 $a(PQKBTitleCode)TC0001261871 035 $a(PQKBWorkID)11212113 035 $a(PQKB)10256425 035 $a(OCoLC)884646456 035 $a(MiAaPQ)EBC1744757 035 $a(DLC) 2014017875 035 $a(Au-PeEL)EBL1744757 035 $a(CaPaEBR)ebr10901881 035 $a(EXLCZ)993710000000202426 100 $a20140814h20142014 uy 0 101 0 $aeng 135 $aur|n|---||||| 181 $ctxt 182 $cc 183 $acr 200 00$aFrom depositional systems to sedimentary successions on the Norwegian continental shelf /$fedited by A. W. Martinius [and four others] 210 1$aChichester, England :$cWiley-Blackwell,$d2014. 210 4$dİ2014 215 $a1 online resource (712 p.) 225 0 $aInternational Association of Sedimentologists ;$vNumber 46 300 $aDescription based upon print version of record. 311 $a1-118-92046-5 320 $aIncludes bibliographical references at the end of each chapters and index. 327 $aFrom Depositional Systems to Sedimentary Successions on the Norwegian Continental MARGIN; Copyright; Contents; Preface; Dedication to John Gjelberg, Michael Talbot and Trevor Elliott; Chapter 1 Generic autogenic behaviour in fluvial systems: lessons from experimental studies; INTRODUCTION; AUTOGENIC PROCESSES; Steep-gradient alluvial fan; Moderate-gradient braided stream systems; Low-gradient rivers; FREQUENCY OF AUTOGENIC PROCESSES; ALLOGENIC CONTROLS ON GENERIC AUTOGENIC BEHAVIOUR; Aggradation rate; Sea-level; Climate; Tectonics; DISCUSSION; IMPLICATIONS 327 $aReconstructions of generic avulsion behaviourSteep-gradient and moderately-gradient systems; Low-gradient river systems; CONCLUSIONS; ACKNOWLEDGEMENTS; REFERENCES; Chapter 2 Climatic and tectonic controls on Triassic dryland terminal fluvial system architecture, central North Sea; INTRODUCTION; Central North Sea stratigraphic framework; Regional tectonic setting; DEPOSITIONAL SETTING; Early to early Middle Triassic facies associations; Middle to Late Triassic facies associations; Terminal character of the Triassic fluvial systems; TECTONIC CONTROLS ON FACIES ARCHITECTURE 327 $aExtensional basin architecturePods and interpods - deposition versus preservation; CLIMATIC CONTROLS; An arid rift interior; Skagerrak Formation fluvial expansion during pluvial phases; Fluvial expansion driven by catchment wettening; Sediment yield; Base level; DISCUSSION; CONCLUSIONS; ACKNOWLEDGEMENTS; REFERENCES; Chapter 3 Late Triassic to Early Jurassic climatic change, northern North Sea region: impact on alluvial architecture, palaeosols and clay mineralogy; INTRODUCTION; GEOLOGICAL FRAMEWORK; Stratigraphy and lithology; Basin configuration and structural framework 327 $aSubdivision of the Lunde Formation and the Statfjord GroupMaterial and methods; Sedimentary facies and alluvial architecture; Palaeosols and mudrock facies; Clay mineralogy and iron oxides; Vertical trends and regional correlation; DISCUSSION; Climate as a controlling factor on sedimentary trends; Tectonics and eustasy versus climate as cause of change in depositional trends; Cause and wider regional aspects of the Triassic-Jurassic climate change; Impact on alluvial architecture and consequences for hydrocarbon exploration; CONCLUSIONS; ACKNOWLEDGEMENTS; REFERENCES 327 $aChapter 4 Applying accommodation versus sediment supply ratio concepts to stratigraphic analysis and zonation of a fluvial reservoirINTRODUCTION; AIMS; ACCOMMODATION TO SEDIMENT SUPPLY RATIO: SIGNIFICANCE, RECOGNITION AND TRENDS; Allocyclic and autocyclic control; Fluvial base level; A/S change and recognition criteria; Trends in A/S change; Long-term A/S change versus short-term autogenic processes; APPLICATION TO THE STATFJORD GROUP; General setting and characteristics; Correlation and zonation challenges; Stratigraphic analysis; Reservoir zonation improvements; CONCLUSIONS 327 $aACKNOWLEDGEMENTS 330 $aThe Norwegian Continental Shelf (NCS), focus of this special publication, is a prolific hydrocarbon region and both exploration and production activity remains high to this day with a positive production outlook. A key element today and in the future is to couple technological developments to improving our understanding of specific geological situations. The theme of the publication reflects the immense efforts made by all industry operators and their academic partners on the NCS to understand in detail the structural setting, sedimentology and stratigraphy of the hydrocarbon bearing units and 410 0$aInternational Association Of Sedimentologists Series 606 $aSedimentary structures$zNorway 606 $aSedimentology$zNorway 606 $aContinental shelf$zNorway 606 $aGeology, Stratigraphic$yEocene 606 $aGeology, Stratigraphic$yPaleocene 606 $aPetroleum$xGeology$zNorway 615 0$aSedimentary structures 615 0$aSedimentology 615 0$aContinental shelf 615 0$aGeology, Stratigraphic 615 0$aGeology, Stratigraphic 615 0$aPetroleum$xGeology 676 $a552/.509481 702 $aMartinius$b A. W. 801 0$bMiAaPQ 801 1$bMiAaPQ 801 2$bMiAaPQ 906 $aBOOK 912 $a9910811747703321 996 $aFrom depositional systems to sedimentary successions on the Norwegian continental shelf$94016673 997 $aUNINA