Depositional record of confined turbidites in syn-subduction intraslope basin: Insight from the Tufiti di Tusa Formation (Southern Apennines, Italy)

[1]  S. Critelli,et al.  Detrital zircon ages of Oligocene to Miocene sandstone suites of the Southern Apennines foreland basin system, Italy , 2022, Journal of Palaeogeography.

[2]  T. Mazza,et al.  Contained-Reflected Megaturbidites of the Marnoso-arenacea Formation (Contessa Key Bed) and Helminthoid Flysches (Northern Apennines, Italy) and Hecho Group (South-Western Pyrenees) , 2022, Frontiers in Earth Science.

[3]  S. Clarke,et al.  Hybrid event bed character and distribution in the context of ancient deep‐lacustrine fan models , 2022, Sedimentology.

[4]  D. Cerone,et al.  Depositional evolution of a tectonically‐confined proximal‐foredeep deep‐marine system: Miocene Serra Palazzo Formation (Southern Apennines, Italy) , 2021, Geological Journal.

[5]  A. Civa,et al.  Laterally accreted deposits in low efficiency turbidites associated with a structurally-induced topography (Oligocene Molare Group, Tertiary Piedmont Basin, NW Italy) , 2021, Journal of Sedimentary Research.

[6]  W. McCaffrey,et al.  Deformation–sedimentation feedback and the development of anomalously thick aggradational turbidite lobes: Outcrop and subsurface examples from the Hikurangi Margin, New Zealand , 2021 .

[7]  J. Eggenhuisen,et al.  The Influence of Confining Topography Orientation on Experimental Turbidity Currents and Geological Implications , 2021, Frontiers in Earth Science.

[8]  K. Pickering,et al.  Submarine topographic control on distribution of supercritical-flow deposits in lobe and related environments, middle Eocene, Jaca Basin, Spanish Pyrenees , 2020 .

[9]  A. Piazza,et al.  Cyclic stacking pattern, architecture and facies of the turbidite lobes in the Macigno Sandstones Formation (Chattian-Aquitanian, northern Apennines, Italy) , 2020 .

[10]  A. Langone,et al.  Preliminary U-Pb Detrital Zircon Ages from Tufiti di Tusa Formation (Lucanian Apennines, Southern Italy): Evidence of Rupelian Volcaniclastic Supply , 2020, Minerals.

[11]  M. Martín-Martín,et al.  Geodynamic Implications of the Latest Chattian-Langhian Central-Western Peri-Mediterranean Volcano-Sedimentary Event: A Review , 2020, The Journal of Geology.

[12]  B. E. Prather,et al.  Controls on reservoir distribution, architecture and stratigraphic trapping in slope settings , 2003, Regional Geology and Tectonics: Principles of Geologic Analysis.

[13]  A. Civa,et al.  Turbidites and turbidity currents , 2020 .

[14]  M. Martín-Martín,et al.  Evolutionary geological models of the central-western peri-Mediterranean chains: a review , 2019 .

[15]  W. McCaffrey,et al.  Sedimentary architecture of detached deep‐marine canyons: Examples from the East Coast Basin of New Zealand , 2018, Sedimentology.

[16]  D. Hodgson,et al.  Topographic Controls On the Development of Contemporaneous but Contrasting Basin-Floor Depositional Architectures , 2018, Journal of Sedimentary Research.

[17]  S. Critelli.  Provenance of Mesozoic to Cenozoic circum-Mediterranean sandstones in relation to tectonic setting , 2018, Earth-Science Reviews.

[18]  A. Piazza,et al.  Turbidites facies response to the morphological confinement of a foredeep (Cervarola Sandstones Formation, Miocene, northern Apennines, Italy) , 2018, Sedimentology.

[19]  M. Pontiggia,et al.  Basin-scale, high-resolution three-dimensional facies modeling of tectonically confined turbidites: An example from the Firenzuola system (Marnoso-arenacea Formation, northern Apennines, Italy) , 2018 .

[20]  F. Perri,et al.  Interpreting provenance relations from sandstone detrital modes, southern Italy foreland region: Stratigraphic record of the Miocene tectonic evolution , 2017 .

[21]  K. Ogata,et al.  Asymmetrical cross-current turbidite facies tract in a structurally-confined mini-basin (Priabonian-Rupelian, Ranzano Sandstone, northern Apennines, Italy) , 2017 .

[22]  W. McCaffrey,et al.  Hybrid event beds dominated by transitional‐flow facies: character, distribution and significance in the Maastrichtian Springar Formation, north‐west Vøring Basin, Norwegian Sea , 2017 .

[23]  D. Hodgson,et al.  Frontal and Lateral Submarine Lobe Fringes: Comparing Sedimentary Facies, Architecture and Flow Processes , 2017 .

[24]  A. Hartley,et al.  The Numidian of Sicily revisited: a thrust-influenced confined turbidite system , 2016 .

[25]  R. Tinterri,et al.  The tectonically confined Firenzuola turbidite system (Marnoso-arenacea Formation, northern Apennines, Italy) , 2016 .

[26]  R. Tinterri,et al.  Convolute laminations and load structures in turbidites as indicators of flow reflections and decelerations against bounding slopes. Examples from the Marnoso-arenacea Formation (northern Italy) and Annot Sandstones (south eastern France) , 2016 .

[27]  G. Groppelli,et al.  Climatic, tectonic and volcanic controls of sediment supply to an Oligocene Foredeep basin: The Val d'Aveto Formation (Northern Italian Apennines) , 2016 .

[28]  M. Moretti,et al.  Contained-reflected turbidites and Slurry Beds in the Tufiti di Tusa Formation.Examples from Lucanian Apennines (Southern Italy) and their significance , 2016 .

[29]  R. Tinterri,et al.  The syntectonic evolution of foredeep turbidites related to basin segmentation: Facies response to the increase in tectonic confinement (Marnoso-arenacea Formation, Miocene, Northern Apennines, Italy) , 2015 .

[30]  F. Felletti,et al.  Short length-scale variability of hybrid event beds and its applied significance , 2015 .

[31]  P. Haughton,et al.  Flow Behavior of Ponded Turbidity Currents , 2015 .

[32]  M. Martín-Martín,et al.  Geodynamic events reconstructed in the Betic, Maghrebian, and Apennine chains (central-western Tethys) , 2014 .

[33]  P. Haughton,et al.  Rheological Complexity In Sediment Gravity Flows Forced To Decelerate Against A Confining Slope, Braux, SE France , 2014 .

[34]  P. Talling.  Hybrid submarine flows comprising turbidity current and cohesive debris flow: Deposits, theoretical and experimental analyses, and generalized models , 2013 .

[35]  E. Carminati,et al.  Geodynamic evolution of the central and western Mediterranean: Tectonics vs. igneous petrology constraints , 2012 .

[36]  I. Kane,et al.  Submarine transitional flow deposits in the Paleogene Gulf of Mexico , 2012 .

[37]  P. DeCelles.  Foreland basin systems revisited: variations in response to tectonic settings , 2012 .

[38]  R. Ingersoll.  Tectonics of Sedimentary Basins, with Revised Nomenclature , 2011 .

[39]  J. Best,et al.  Depositional processes, bedform development and hybrid bed formation in rapidly decelerated cohesive (mud–sand) sediment flows , 2011 .

[40]  F. Perri,et al.  Provenance signatures for the Miocene volcaniclastic succession of the Tufiti di Tusa Formation, southern Apennines, Italy , 2011, Geological Magazine.

[41]  R. Tinterri,et al.  Synsedimentary structural control on foredeep turbidites: An example from Miocene Marnoso-arenacea Formation, Northern Apennines, Italy , 2011 .

[42]  R. Tinterri,et al.  Stratigraphy and depositional setting of slurry and contained (reflected) beds in the Marnoso‐arenacea Formation (Langhian‐Serravallian) Northern Apennines, Italy , 2010 .

[43]  P. Haughton,et al.  Hybrid sediment gravity flow deposits – Classification, origin and significance , 2009 .

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

[45]  M. Covey.  The Evolution of Foreland Basins to Steady State: Evidence from the Western Taiwan Foreland Basin , 2009 .

[46]  F. Lucchi.  The Oligocene to Recent Foreland Basins of the Northern Apennines , 2009 .

[47]  Jeff Peakall,et al.  A Phase Diagram for Turbulent, Transitional, and Laminar Clay Suspension Flows , 2009 .

[48]  E. Patacca,et al.  Geology of the Southern Apennines , 2007 .

[49]  L. Sabato,et al.  Cretaceous anoxic events in the argilliti e radiolariti di Campomaggiore unit (Lagonegro-Molise basin, southern Italy) , 2007 .

[50]  E. Sumner,et al.  An experimental investigation of sand–mud suspension settling behaviour: implications for bimodal mud contents of submarine flow deposits , 2006 .

[51]  L. Fernández,et al.  The Transition Between Sheet-Like Lobe and Basin-Plain Turbidites in the Hecho Basin (South-Central Pyrenees, Spain) , 2005 .

[52]  V. Perrone,et al.  Tectono‐sedimentary evolution of the southern branch of the Western Tethys (Maghrebian Flysch Basin and Lucanian Ocean): consequences for Western Mediterranean geodynamics , 2005 .

[53]  John B. Southard,et al.  Experiments on Oscillatory-Flow and Combined-Flow Bed Forms: Implications for Interpreting Parts of the Shallow-Marine Sedimentary Record , 2005 .

[54]  V. Perrone,et al.  The age of the oceanic accretionary wedge and onset of continental collision in the Sicilian Maghrebian Chain , 2004 .

[55]  B. Kneller,et al.  Experimental Modeling of the Spatial Distribution of Grain Size Developed in a Fill-and-Spill Mini-Basin Setting , 2004 .

[56]  R. Wynn,et al.  Beds comprising debrite sandwiched within co‐genetic turbidite: origin and widespread occurrence in distal depositional environments , 2004 .

[57]  R. Smith.  Silled sub-basins to connected tortuous corridors: sediment distribution systems on topographically complex sub-aqueous slopes , 2004, Geological Society, London, Special Publications.

[58]  A. Bouma.  Key controls on the characteristics of turbidite systems , 2004, Geological Society, London, Special Publications.

[59]  J. Alexander,et al.  Changes in Flow Direction at a Point Caused by Obstacles During Passage of a Density Current , 2003 .

[60]  A. Taira,et al.  Sedimentary and Tectonic Evolution of a Trench-Slope Basin in the Nankai Subduction Zone of Southwest Japan , 2003 .

[61]  E. Mutti,et al.  Deltaic, mixed and turbidite sedimentation of ancient foreland basins , 2003 .

[62]  M. Grasso,et al.  Pattern of orogenic rotations in central–eastern Sicily: implications for the timing of spreading in the Tyrrhenian Sea , 2003, Journal of the Geological Society.

[63]  R. Maniscalco,et al.  Genesis and evolution of a curved mountain front: paleomagnetic and geological evidence from the Gran Sasso range (central Apennines, Italy) , 2003 .

[64]  F. Lottaroli,et al.  INTEGRATED HIGH-RESOLUTION STRATIGRAPHY OF THE LOWER OLIGOCENETUSA TUFFITE FORMATION IN THE CALABRO-LUCANO AREAAND SICILY (SOUTHERN ITALY) , 2002 .

[65]  A. D. Stefano,et al.  Stratigraphical and structural constraints in the Lucanian Apennines (southern Italy): tools for reconstructing the geological evolution , 2002 .

[66]  J. Gattacceca,et al.  Paleomagnetism of Jurassic to Miocene sediments from the Apenninic carbonate platform (southern Apennines, Italy): evidence for a 60° counterclockwise Miocene rotation , 2002 .

[67]  H. Sinclair,et al.  Depositional Evolution of Confined Turbidite Basins , 2002 .

[68]  Jan Alexander,et al.  Abrupt change in slope causes variation in the deposit thickness of concentrated particle-driven density currents , 2001 .

[69]  P. Maiorano,et al.  REVISED STRATIGRAPHY OF THE SERRA PALAZZO FORMATION, A MIOCENE FOREDEEP TURBIDITE SUCCESSION OF THE SOUTHERN APENNINES (ITALY) , 1999 .

[70]  J. R. Booth,et al.  Classification, Lithologic Calibration, and Stratigraphic Succession of Seismic Facies of Intraslope Basins, Deep-Water Gulf of Mexico , 1998 .

[71]  G. Piccarreta,et al.  Mineral and chemical provenance indicators in some early Miocene sandstones of the Southern Apennines (Italy) , 1997 .

[72]  M. Yokokawa.  Combined-Flow Ripples : Genetic Experiments and Applications for Geologic Records , 1995 .

[73]  E. Pera,et al.  Tectonic Evolution of the Southern Apennines Thrust-Belt (Italy) as Reflected in Modal Compositions of Cenozoic Sandstone , 1995, The Journal of Geology.

[74]  J. Best,et al.  On experimental reflected density currents and the interpretation of certain turbidites , 1994 .

[75]  P. Haughton.  Deposits of deflected and ponded turbidity currents, Sorbas Basin, Southeast Spain , 1994 .

[76]  H. Sinclair.  The influence of lateral basinal slopes on turbidite sedimentation in the Annot sandstones of SE France , 1994 .

[77]  S. Critelli.  Sandstone detrital modes in the Paleogene Liguride Complex, accretionary wedge of the southern Apennines (Italy) , 1993 .

[78]  B. Kneller,et al.  Oblique reflection of turbidity currents , 1991 .

[79]  R. D. Rosa,et al.  Significato dei depositi vulcanoclastici della formazione delle Tufiti di Tusa (Miocene inferiore, Lucania meridionale) , 1990 .

[80]  M. Leeder,et al.  Reverse Flow in Turbidity Currents: The Role of Internal Solitons , 1987 .

[81]  Kevin T. Pickering,et al.  Contained (reflected) turbidity currents from the Middle Ordovician Cloridorme Formation, Quebec, Canada: an alternative to the antidune hypothesis , 1985 .

[82]  F. Lucchi,et al.  Basin‐wide turbidites in a Miocene, over‐supplied deep‐sea plain: a geometrical analysis , 1980 .

[83]  O. Riba.  Syntectonic unconformities of the Alto Cardener, Spanish Pyrenees: a genetic interpretation☆ , 1976 .

[84]  F. Wezel,et al.  Nuovi dati sulla eta' e posizione strutturale del Flysch di Tusa in Sicilia , 1973 .