LEADER 05438nam 2200733 450 001 9910143126903321 005 20170810175547.0 010 $a1-282-17166-6 010 $a9786612171666 010 $a1-4443-0447-X 010 $a1-4443-0448-8 035 $a(CKB)1000000000767602 035 $a(EBL)428002 035 $a(OCoLC)815644801 035 $a(SSID)ssj0000293565 035 $a(PQKBManifestationID)11235750 035 $a(PQKBTitleCode)TC0000293565 035 $a(PQKBWorkID)10302601 035 $a(PQKB)11028118 035 $a(MiAaPQ)EBC428002 035 $a(EXLCZ)991000000000767602 100 $a20160804h19921992 uy 0 101 0 $aeng 135 $aur|n|---||||| 181 $ctxt 182 $cc 183 $acr 200 00$aDeep-water turbidite systems /$fedited by Dorrick A.V. Stow 210 1$aOxford, [England] :$cBlackwell Scientific Publications,$d1992. 210 4$dİ1992 215 $a1 online resource (483 p.) 225 1 $aReprint Series Volume 3 of the International Association of Sedimentologists 300 $aDescription based upon print version of record. 311 $a0-632-03262-6 320 $aIncludes bibliographical references at the end of each chapters and index. 327 $aDeep-Water Turbidite Systems; Contents; Preface; Deep-water turbidite systems: an introduction; Processes: overview and commentary; Modelling of turbidity currents on Navy Submarine Fan, California Continental Borderland; A physical model for the transport and sorting of fine-grained sediment by turbidity currents; The hydraulic interpretation of turbidites from their grain sizes and sedimentary structures; Subaqueous liquefied and fluidized sediment flows and their deposits; Flow regimes in debris flow 327 $aContained (reflected) turbidity currents from the Middle Ordovician Cloridorme Formation, Quebec, Canada: an alternative to the antidune hypothesisReverse flow in turbidity currents: the role of internal solitons [abstract only]; Measurements of density underflows from Walensee, Switzerland [abstract only]; Debris flow (olistostromes) and slumping on a distal passive continental margin: the Palombini limestone-shale sequence of the northern Apennines [abstract only]; Water escape structures in coarse-grained sediment flows and their deposits [abstract only] 327 $aFacies characteristics: overview and commentaryTurbiditic and non-turbiditic mudstone of Cretaceous flysch sections of the East Alps and other basins; Distinguishing between fine-grained turbidites and contourites on the Nova Scotian deep-water margin; Rhythms in deep sea, fine-grained turbidite and debris-flow sequences, Middle Ordovician, eastern Tennessee; Distinctive thin-bedded turbidite facies and related depositional environments in the Eocene Hecho Group (south-central Pyrenees, Spain) 327 $aSedimentology of very thick calcarenite marlstone beds in a flysch succession, southwestern PyreneesThe Cambro-Ordovician Cap Enrage Formation, Quebec, Canada: conglomeratic deposits of a braided submarine channel with terraces; Deep marine arc apron deposits and syndepositional magmatism in the Alisitos group at Punta Cono, Baja California, Mexico; Use of clay fabric to distinguish turbiditic and hemipelagic siltstones and silts [abstract only] 327 $aThe Cretaceous Talme Yafe Formation: a contour current shaped sedimentary prism of calcareous detritus at the continental margin of the Arabian Craton [abstract only]Mass transport in European Cretaceous chalk; fabric criteria for its recognition [abstract only]; Middle and Late Quaternary depositional sequences and cycles in the eastern Mediterranean [abstract only]; Texture and structure of resedimented conglomerates: examples from Ksiaz Formation (Famennian-Tournaisian), south-western Poland [abstract only] 327 $aWater escape structures in the context of a depositional model of a mass flow dominated conglomeratic fan-delta (Abrioja Formation, Pliocene, Almeria Basin, SE Spain) [abstract only] 330 $aThis third volume in the IAS Reprint Series reviews some of the major contributions that have been made over the last twenty years to our understanding of deep water environments. Few groups of rocks have received as much attention in recent years as deep sea sands and yet retained so many unsolved problems - How far and how fast can sediment debris flows travel? Do the many ancient series that have been interpreted as submarine fan deposits bear any resemblance to present day deep sea flows? How valid are the sequences described as coarsening upward or fining upward, and how should they be in 410 0$aReprint series ... of the International Association of Sedimentologists ;$vVolume 3. 606 $aTurbidites 606 $aMarine sediments 606 $aTurbidity currents 606 $aSubmarine geology 606 $aGeology, Stratigraphic 608 $aElectronic books. 615 0$aTurbidites. 615 0$aMarine sediments. 615 0$aTurbidity currents. 615 0$aSubmarine geology. 615 0$aGeology, Stratigraphic. 676 $a551.46083 676 $a552.5 702 $aStow$b D. A. V$g(Dorrik A. V.), 801 0$bMiAaPQ 801 1$bMiAaPQ 801 2$bMiAaPQ 906 $aBOOK 912 $a9910143126903321 996 $aDeep Water Turbidite Systems$91572071 997 $aUNINA