@article{menard1955deepsea,
    author = "Menard, Henry W.",
    title = "Deep-Sea Channels, Topography, and Sedimentation",
    year = "1955",
    journal = "AAPG Bulletin",
    abstract = "The type and distribution of much of the minor topography in the northeastern Pacific basin can be correlated with the accessibility of a given area to deposition from turbidity currents. Deep-sea areas separated from North America by basins or troughs, which act as sediment traps for turbidity currents, are characterized by a highly irregular relief of a few hundred feet. Other areas connected to the continent by a gradual continuous slope are characterized by very smooth plains like those of the North Atlantic sea floor. These plains slope out from the continent except in the vicinity of long ridges on the sea floor. The plains slope around the ridges because the slopes are formed by turbidity currents and the ridges act as dams to deflect the currents to one side. Roug-bottomed basins thousands of feet deep are found in the regions of smooth plains, but with one exception all are inaccessible to turbidity currents because they are surrounded by mountains, or lie on the “lee” side of ridges relative to the general direction of flow of turbidity currents. The exceptional basin is in a seismically active area, and it may have formed too recently to be filled by turbidity-current deposition. Turbidity currents have formed deep-sea fans at the mouths of many submarine canyons, and deep-sea channels cross most, if not all, of the fans. All twelve of the channels which have been explored in any detail hook sharply to the left across the fans. This left hook can be explained as a secondary effect of the action of Coriolis force on the turbidity currents which formed the channels. Without channels, this type of flow would have no tendency to hook left. Unchannelized turbidity currents are required to form the fans.",
    url = "https://doi.org/10.1306/5ceae136-16bb-11d7-8645000102c1865d",
    doi = "10.1306/5ceae136-16bb-11d7-8645000102c1865d",
    number = "2",
    pages = "236-255",
    volume = "39"
}

@misc{sullwold1961turbidites3,
    author = "Sullwold, H. H. and Jr",
    title = "Turbidites in Oil Exploration, in Peterson, J. A., and Osmond, J. C., eds., Geometry of Sand Bodies",
    year = "1961",
    howpublished = "American Association of Petroleum Geologists, p. 63-81",
    note = "talkorigins\_source = {true}; raw\_reference = {Sullwold, H. H., Jr., 1961, Turbidites in Oil Exploration, in Peterson, J. A., and Osmond, J. C., eds., Geometry of Sand Bodies: American Association of Petroleum Geologists, p. 63-81.}"
}

@misc{mutti1972le1,
    author = "Mutti, E. and Ricci Lucchi, F",
    title = "Le torbiditi dell'Appennino settentrionale",
    year = "1972",
    howpublished = "introduzione all'ananisi di facies: Memoirs Soc. Geol. Italiana, v. 11, p. 161-199",
    note = "talkorigins\_source = {true}; raw\_reference = {Mutti, E., and Ricci Lucchi, F., 1972, Le torbiditi dell'Appennino settentrionale: introduzione all'ananisi di facies: Memoirs Soc. Geol. Italiana, v. 11, p. 161-199.}"
}

@article{crossref1973turbidites,
    title = "Turbidites and Deep-Water Sedimentation",
    year = "1973",
    journal = "Earth-Science Reviews",
    url = "https://doi.org/10.1016/0012-8252(73)90033-0",
    doi = "10.1016/0012-8252(73)90033-0",
    number = "4",
    pages = "389",
    volume = "9"
}

@misc{nelsom1973submarine2,
    author = "Nelsom, C. H. and Kulm, L. D",
    title = "Submarine fans and deep-sea channels, in Middleton, G. V., and Bouma, A. H., eds., Turbidites and deep-water sedimentation",
    year = "1973",
    howpublished = "Society of Economic Paleontologists and Mineralogists, p. 39-78",
    note = "talkorigins\_source = {true}; raw\_reference = {Nelsom, C. H., and Kulm, L. D., 1973, Submarine fans and deep-sea channels, in Middleton, G. V., and Bouma, A. H., eds., Turbidites and deep-water sedimentation: Society of Economic Paleontologists and Mineralogists, p. 39-78.}"
}

@article{gorsline1974turbidites,
    author = "Gorsline, D. S.",
    title = "Turbidites and Deep Water Sedimentation [book review]",
    year = "1974",
    journal = "Journal of Sedimentary Research",
    url = "https://doi.org/10.2110/jsr.279",
    doi = "10.2110/jsr.279",
    number = "1",
    pages = "279-0",
    volume = "44"
}

@article{sestini1974turbidites,
    author = "Sestini, G.",
    title = "Turbidites and deep-water sedimentation",
    year = "1974",
    journal = "Sedimentary Geology",
    url = "https://doi.org/10.1016/0037-0738(74)90017-7",
    doi = "10.1016/0037-0738(74)90017-7",
    number = "1",
    pages = "67-69",
    volume = "12"
}

@article{sternberg1974turbidites,
    author = "Sternberg, Richard W.",
    title = "Turbidites and deep-water sedimentation",
    year = "1974",
    journal = "Marine Geology",
    url = "https://doi.org/10.1016/0025-3227(74)90089-9",
    doi = "10.1016/0025-3227(74)90089-9",
    number = "4",
    pages = "239-240",
    volume = "16"
}

@incollection{swift1974continental,
    author = "Swift, Donald J. P.",
    title = "Continental Shelf Sedimentation",
    year = "1974",
    booktitle = "The Geology of Continental Margins",
    url = "https://doi.org/10.1007/978-3-662-01141-6\_10",
    doi = "10.1007/978-3-662-01141-6\_10",
    pages = "117-135"
}

@incollection{eisma1982shelf,
    author = "Eisma, D.",
    title = "Shelf sedimentation",
    year = "1982",
    booktitle = "Encyclopedia of Earth Sciences Series",
    url = "https://doi.org/10.1007/0-387-30843-1\_410",
    doi = "10.1007/0-387-30843-1\_410",
    pages = "749-750"
}

@incollection{scott2003influence,
    author = "Scott, Erik D. and Bouma, Arnold H.",
    title = "Influence of Shelf and Slope Processes on Deep-Water Sedimentation",
    year = "2003",
    booktitle = "Shelf Margin Deltas and Linked Down Slope Petroleum Systems: 23rd Annual",
    url = "https://doi.org/10.5724/gcs.03.23.0577",
    doi = "10.5724/gcs.03.23.0577",
    pages = "577-596"
}

@article{vrbanac2010sedimentation,
    author = "Vrbanac, Boris and Velić, Josipa and Malvić, Tomislav",
    title = "Sedimentation of deep-water turbidites in the SW part of the Pannonian Basin",
    year = "2010",
    journal = "Geologica Carpathica",
    abstract = "Sedimentation of deep-water turbidites in the SW part of the Pannonian Basin The Sava Depression and the Bjelovar Subdepression belong to the SW margin of the Pannonian Basin System, which was part of the Central Paratethys during the Pannonian period. Upper Pannonian deposits of the Ivanic-Grad Formation in the Sava Depression include several lithostratigraphic members such as Iva and Okoli Sandstone Member or their lateral equivalents, the Zagreb Member and Lipovac Marlstone Member. Their total thickness in the deepest part of the Sava Depression reaches up to 800 meters, while it is 100-200 meters in the margins of the depression. Deposits in the depression are composed of 4 facies. In the period of turbiditic activities these facies are primarily sedimented as different sandstone bodies. In the Bjelovar Subdepression, two lithostratigraphic members (lateral equivalent) were analysed, the Zagreb Member and Okoli Sandstone Member. The thickness of the Bjelovar Subdepression ranges from 50 meters along the S and SE margins to more than 350 meters along the E margin. Generally, detritus in the north-west part of the analysed area originated from a single source, the Eastern Alps, as demonstrated by sedimentological and physical properties, the geometry of the sandstone body and the fossil content. This clastic material was found to be dispersed throughout the elongated and relatively narrow Sava Depression and in the smaller Bjelovar Subdepression. Sedimentation primarily occurred in up to 200 meters water depth and was strongly influenced by the sub-aqueous paleorelief, which determined the direction of the flow of turbidity currents and sandstone body geometries. The main stream with medium- and fine-grained material was separated by two independent turbiditic flows from N-NW to the SE-E. Variability in the thickness of sandstone bodies is the result of differences in subsidence and cycles of progradation and retrogradation of turbidite fans.",
    url = "https://doi.org/10.2478/v10096-010-0001-8",
    doi = "10.2478/v10096-010-0001-8",
    number = "1",
    pages = "55-69",
    volume = "61"
}

@misc{crossrefNoneshelf,
    title = "Shelf sedimentation",
    year = "None",
    booktitle = "SpringerReference",
    url = "https://doi.org/10.1007/springerreference\_4728",
    doi = "10.1007/springerreference\_4728"
}