Reply to Comment by R. Higgs on 'Hybrid sediment gravity flows ― classification, origin and significance

[1]  J. Eggenhuisen,et al.  Shallow erosion beneath turbidity currents and its impact on the architectural development of turbidite sheet systems , 2011 .

[2]  Y. L. Gonidec,et al.  Lobe construction and sand/mud segregation by turbidity currents and debris flows on the western Nile deep-sea fan (Eastern Mediterranean) , 2010 .

[3]  P. Haughton,et al.  Character and distribution of hybrid sediment gravity flow deposits from the outer Forties Fan, Palaeocene Central North Sea, UKCS , 2009 .

[4]  D. Hodgson.  Distribution and origin of hybrid beds in sand-rich submarine fans of the Tanqua depocentre, Karoo Basin, South Africa , 2009 .

[5]  E. Sumner,et al.  Deposits of flows transitional between turbidity current and debris flow , 2009 .

[6]  Makoto Ito.  Downfan Transformation from Turbidity Currents to Debris Flows at a Channel-to-Lobe Transitional Zone: The Lower Pleistocene Otadai Formation, Boso Peninsula, Japan , 2008 .

[7]  P. Haughton,et al.  Development of Rheological Heterogeneity in Clay-Rich High-Density Turbidity Currents: Aptian Britannia Sandstone Member, U.K. Continental Shelf , 2008 .

[8]  R. Schiebel,et al.  Onset of submarine debris flow deposition far from original giant landslide , 2007, Nature.

[9]  E. Fugelli,et al.  Delineating confined slope turbidite systems offshore mid-Norway: The Cretaceous deep-marine Lysing Formation , 2007 .

[10]  R. Wynn,et al.  New insight into the evolution of large‐volume turbidity currents: comparison of turbidite shape and previous modelling results , 2007 .

[11]  C. Montenat,et al.  Seismites: An attempt at critical analysis and classification , 2007 .

[12]  Larry Zarra,et al.  Chronostratigraphic Framework for the Wilcox Formation (Upper Paleocene–Lower Eocene) in the Deep-Water Gulf of Mexico: Biostratigraphy, Sequences, and Depositional Systems , 2007 .

[13]  J. Dunham,et al.  Leaves in turbidite sands: The main source of oil and gas in the deep-water Kutei Basin, Indonesia , 2006 .

[14]  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 .

[15]  B. Kneller,et al.  The Interpretation of Vertical Sequences in Turbidite Beds: The Influence of Longitudinal Flow Structure , 2003 .

[16]  P. Haughton,et al.  ‘Linked’ debrites in sand‐rich turbidite systems – origin and significance , 2003 .

[17]  Sébastien Migeon,et al.  Marine hyperpycnal flows: initiation, behavior and related deposits. A review , 2003 .

[18]  A. Palfrey,et al.  Facies of slurry‐flow deposits, Britannia Formation (Lower Cretaceous), North Sea: implications for flow evolution and deposit geometry , 2003 .

[19]  J. Best,et al.  Turbulence Modulation in Clay-Rich Sediment-Laden Flows and Some Implications for Sediment Deposition , 2002 .

[20]  D. Lowe,et al.  Slurry‐flow deposits in the Britannia Formation (Lower Cretaceous), North Sea: a new perspective on the turbidity current and debris flow problem , 2000 .

[21]  R. Higgs.  Return of `The Fan That Never Was': Westphalian turbidite systems in the Variscan Culm Basin: Bude Formation (south‐west England) , 1998 .

[22]  D. B. Prior,et al.  Flow properties of turbidity currents in Bute Inlet, British Columbia , 1991 .