LEADER 04038nam 2200697Ia 450 001 9910830272203321 005 20180612234432.0 010 $a1-282-00787-4 010 $a9786612007873 010 $a1-4443-0313-9 010 $a1-4443-0314-7 035 $a(CKB)1000000000722794 035 $a(EBL)416355 035 $a(SSID)ssj0000102850 035 $a(PQKBManifestationID)11126831 035 $a(PQKBTitleCode)TC0000102850 035 $a(PQKBWorkID)10061174 035 $a(PQKB)11698328 035 $a(MiAaPQ)EBC416355 035 $a(OCoLC)352832734 035 $a(PPN)149356161 035 $a(EXLCZ)991000000000722794 100 $a20080520d2008 uy 0 101 0 $aeng 135 $aur|n|---||||| 181 $ctxt 182 $cc 183 $acr 200 00$aAnalogue and numerical modelling of sedimentary systems$b[electronic resource] $efrom understanding to prediction /$fedited by Poppe de Boer ... [et al.] 210 $aChichester, UK ;$aHoboken, NJ $cWiley-Blackwell $cInternational Association of Sedimentologists$d2008 215 $a1 online resource (328 p.) 225 1 $aSpecial publication of the International Association of Sedimentologists ;$vnumber 40 300 $aDescription based upon print version of record. 311 $a1-4051-8930-4 320 $aIncludes bibliographical references and index. 327 $aPredicting discharge and sediment flux of the Po River, Italy sincethe Last Glacial MaximumALBERT J. KETTNER and JAMES P.M. SYVITSKIImpact of discharge, sediment flux and sea-level change onstratigraphic architecture of river-delta-shelf systemsGEORGE POSTMA and AART PETER VAN DEN BERG VAN SAPAROEA; Grain-size sorting of river-shelf-slope sediments duringglacial-interglacial cycles: modelling grain-size distributionand interconnectedness of coarse-grained bodiesXANDER D.MEIJER 327 $aModelling the preservation of sedimentary deposits on passivecontinental margins during glacial-interglacial cyclesXANDER D.MEIJER, GEORGE POSTMA, PETER A.BURROUGH and POPPE L.DE BOERModelling source-rock distribution and quality variations:the organic facies modelling approachUTE MANN and JANINE ZWEIGEL1; Spatial data templates: combining simple models ofphysical processes with stochastic noise to yield stable,archetypal landformsPETER A.BURROUGH 1; Models that talk backJOHN C.TIPPER; Index 330 $aUnderstanding basin-fill evolution and the origin of stratal architectures has traditionally been based on studies of outcrops, well and seismic data, studies of and inferences on qualitative geological processes, and to a lesser extent based on quantitative observations of modern and ancient sedimentary environments. Insight gained on the basis of these studies can increasingly be tested and extended through the application of numerical and analogue forward models. Present-day stratigraphic forward modelling follows two principle lines: 1) the deterministic process-based approach, ideally w 410 0$aSpecial publication ... of the International Association of Sedimentologists ;$vno. 40. 606 $aGeology$zItaly$zDolomite Alps$vCongresses 606 $aGeology, Stratigraphic$yMesozoic$vCongresses 606 $aCarbonate rocks$zItaly$zDolomite Alps$vCongresses 606 $aSedimentary basins$zItaly$zDolomite Alps$vCongresses 606 $aSedimentary structures$zItaly$zDolomite Alps$xMathematical models$vCongresses 606 $aSequence stratigraphy$vCongresses 615 0$aGeology 615 0$aGeology, Stratigraphic 615 0$aCarbonate rocks 615 0$aSedimentary basins 615 0$aSedimentary structures$xMathematical models 615 0$aSequence stratigraphy 676 $a552.5 676 $a552/.5 701 $aBoer$b Poppe Lubberts de$f1949-$01652370 801 0$bMiAaPQ 801 1$bMiAaPQ 801 2$bMiAaPQ 906 $aBOOK 912 $a9910830272203321 996 $aAnalogue and numerical modelling of sedimentary systems$94002977 997 $aUNINA