Field expressions of the transformation of debris flows into turbidity currents, with examples from the Polish Carpathians and the French Maritime Alps
暂无分享,去创建一个
J. Peakall | A. Uchman | L. Amy | A. Ślączka | S. Leszczyński | M. Félix
[1] B. Kneller,et al. Facies architecture of the Grès de Peïra Cava, SE France: landward stacking patterns in ponded turbiditic basins , 2007, Journal of the Geological Society.
[2] Jeff Peakall,et al. Transformation of debris flows into turbidity currents: mechanisms inferred from laboratory experiments , 2006 .
[3] P. Talling,et al. Anatomy of turbidites and linked debrites based on long distance (120 × 30 km) bed correlation, Marnoso Arenacea Formation, Northern Apennines, Italy , 2006 .
[4] J. Peakall,et al. Combined measurements of velocity and concentration in experimental turbidity currents , 2005 .
[5] Z. Sylvester,et al. Textural trends in turbidites and slurry beds from the Oligocene flysch of the East Carpathians, Romania , 2004 .
[6] R. Wynn,et al. Beds comprising debrite sandwiched within co‐genetic turbidite: origin and widespread occurrence in distal depositional environments , 2004 .
[7] P. Talling,et al. The character and origin of thick base-of-slope sandstone units of the Peïra Cava outlier, SE France , 2004, Geological Society, London, Special Publications.
[8] P. Joseph,et al. Deep-water sedimentation in the Alpine Foreland Basin of SE France: New perspectives on the Grès d’Annot and related systems—an introduction , 2004, Geological Society, London, Special Publications.
[9] B. Kneller,et al. The influence of a lateral basin-slope on the depositional patterns of natural and experimental turbidity currents , 2004, Geological Society, London, Special Publications.
[10] T. Elliott,et al. The structural setting and palaeogeographical evolution of the Grès d’Annot Basin , 2004, Geological Society, London, Special Publications.
[11] P. Joseph,et al. Deep-water sedimentation in the Alpine Basin of SE France : new perspectives on the Grès d'Annot and related systems , 2004 .
[12] P. Haughton,et al. ‘Linked’ debrites in sand‐rich turbidite systems – origin and significance , 2003 .
[13] Y. Sohn,et al. Transition from debris flow to hyperconcentrated flow in a submarine channel (the Cretaceous Cerro Toro Formation, southern Chile) , 2002 .
[14] R. Wynn,et al. Experimental constraints on shear mixing rates and processes: implications for the dilution of submarine debris flows , 2002, Geological Society, London, Special Publications.
[15] B. Kneller,et al. Process controls on the development of stratigraphic trap potential on the margins of confined turbidite systems and aids to reservoir evaluation , 2001 .
[16] Y. Sohn. Depositional Processes of Submarine Debris Flows in the Miocene Fan Deltas, Pohang Basin, SE Korea with Special Reference to Flow Transformation , 2000 .
[17] B. Kneller,et al. Evaluating the Links Between Turbidite Characteristics and Gross System Architecture: Upscaling Insights from the Turbidite Sheet-System of Peïra Cava, SE France , 2000 .
[18] Ben Kneller,et al. Depositional effects of flow nonuniformity and stratification within turbidity currents approaching a bounding slope; deflection, reflection, and facies variation , 1999 .
[19] Robert B. Kidd,et al. Heterogeneity and lithotype distribution in ancient deep-sea canyons: Point Lobos deep-sea canyon as a reservoir analogue , 1998 .
[20] M. Kováč,et al. On Late Oligocene to Pliocene depocentre migrations and the evolution of the Carpathian-Pannonian system , 1996 .
[21] Kelin X. Whipple,et al. Hydroplaning of subaqueous debris flows , 1995 .
[22] M. Valladares. Siliciclastic-carbonate slope apron in an immature tensional margin (Upper Precambrian-Lower Cambrian), Central Iberian Zone, Salamanca, Spain , 1995 .
[23] A. Martinius,et al. Modified-grain-flow Deposits from the Upper Cretaceous Vallcarga Formation, South-Central Pyrenees, Spain , 1994 .
[24] V. Hilton. Architecture of deep-marine confined sandstone bodies, Eocene-Oligocene Gres d'Annot formation, SE France. , 1994 .
[25] D. Stanley. Model for turbidite-to-contourite continuum and multiple process transport in deep marine settings: examples in the rock record , 1993 .
[26] A. Bouma. Clastic depositional styles and reservoir potential of Mediterranean basins , 1990 .
[27] F. Weirich. The generation of turbidity currents by subaerial debris flows, California , 1989 .
[28] S. Leszczyński. Characteristics and origin of fluxoturbidites from the Carpathian flysch (Cretaceous-Palaeogene), South Poland , 1989 .
[29] P. Trémolières,et al. Sédimentation et tectonique dans le bassin marin Eocène supérieur-Oligocène des Alpes du Sud , 1987 .
[30] P. Souquet,et al. Facies sequences in large-volume debris- and turbidity-flow deposits from the Pyrenees (Cretaceous; France, Spain) , 1987 .
[31] R. Bourrouilh. Evolutionary mass flow-megaturbidites in an interplate basin: Example of the north Pyrenean basin , 1987 .
[32] J. M. Coleman,et al. Peira-Cava Turbidite System, France , 1985 .
[33] A. Bouma,et al. Submarine fans and related turbidite systems , 1985 .
[34] R. V. Fisher. Flow transformations in sediment gravity flows , 1983 .
[35] D. Stanley. Welded slump-graded sand couplets: evidence for slide generated turbidity currents , 1982 .
[36] D. Lowe. Sediment Gravity Flows: II Depositional Models with Special Reference to the Deposits of High-Density Turbidity Currents , 1982 .
[37] H. Schwarz. Subaqueous Slope Failures: Experiments and Modern Occurrences , 1982 .
[38] A. Ślączka,et al. A revision of the fluxoturbidite concept based on type examples in the Polish Carpathian Flysch , 1981 .
[39] F. Krause,et al. Submarine carbonate breccia beds—a oppositional model for two-layer, sediment gravity flows from the Sekwi Formation (Lower Cambrian), Mackenzie Mountains, Northwest Territories, Canada , 1979 .
[40] D. Stanley,et al. Sedimentation in submarine canyons, fans and trenches , 1978 .
[41] H. Reineck,et al. Depositional sedimentary environments , 1973 .
[42] M. Hampton,et al. The Role of Subaqueous Debris Flow in Generating Turbidity Currents , 1972 .
[43] J. R. Allen. Mixing at Turbidity Current Heads, and Its Geological Implications , 1971 .
[44] T. H. Andel,et al. Ponded Sediments of the Mid-Atlantic Ridge between 22° and 23° North Latitude , 1969 .
[45] D. Stanley,et al. Sedimentological Evidence for an Emerged Land Mass in the Ligurian Sea during the Palaeogene , 1968, Nature.
[46] N R Morgenstern,et al. Submarine slumping and the initiation of turbidity currents , 1967 .
[47] C. Larsonneur,et al. Les courants de turbidité, les coulées boueuses et les glissements : Résultats d'expériences , 1965 .
[48] Arnold H. Bouma,et al. Sedimentology of some Flysch deposits : a graphic approach to facies interpretation , 1962 .
[49] P. Kuenen,et al. TURBIDITES IN FLYSCH OF THE POLISH CARPATHIAN MOUNTAINS , 1959 .
[50] P. Kuenen,et al. Turbidity Currents as a Cause of Graded Bedding , 1950, The Journal of Geology.