@techreport{trowbridge1930building26,
    author = "Trowbridge, A. C",
    title = "Building of the Mississippi delta",
    year = "1930",
    howpublished = "Bulletin of the American Association of Petroleum Geologists, v. 38, p. 167-192",
    note = "talkorigins\_source = {true}; raw\_reference = {Trowbridge, A. C., 1930, Building of the Mississippi delta: Bulletin of the American Association of Petroleum Geologists, v. 38, p. 167-192.}"
}

@book{pettijohn1957sedimentary22,
    author = "Pettijohn, F. J",
    title = "Sedimentary Rocks [2nd ed.]",
    year = "1957",
    publisher = "New York, John Wiley \& Sons, 718 p",
    note = "talkorigins\_source = {true}; raw\_reference = {Pettijohn, F. J., 1957, Sedimentary Rocks [2nd ed.]: New York, John Wiley \& Sons, 718 p.}"
}

@misc{krumbein1963stratigraphy11,
    author = "Krumbein, W. C. and Sloss, L. L",
    title = "Stratigraphy and Sedimentation",
    year = "1963",
    howpublished = "San Francisco, Freeman, 660 p",
    note = "talkorigins\_source = {true}; raw\_reference = {Krumbein, W. C., and Sloss, L. L., 1963, Stratigraphy and Sedimentation: San Francisco, Freeman, 660 p.}"
}

@misc{bekker1968ancient1,
    author = "Bekker, Y. R",
    title = "Ancient mollasses of folded systems in European USSR and their importance for stratigraphy [in Russian], in Precambrian Geology",
    year = "1968",
    howpublished = "Moscow, Nauka, p. 52-58",
    note = "talkorigins\_source = {true}; raw\_reference = {Bekker, Y. R., 1968, Ancient mollasses of folded systems in European USSR and their importance for stratigraphy [in Russian], in Precambrian Geology: Moscow, Nauka, p. 52-58.}"
}

@misc{folk1968petrology6,
    author = "Folk, R. L",
    title = "Petrology of Sedimentary Rocks",
    year = "1968",
    howpublished = "Austin, Texas, Hemphills, 170 p",
    note = "talkorigins\_source = {true}; raw\_reference = {Folk, R. L., 1968, Petrology of Sedimentary Rocks: Austin, Texas, Hemphills, 170 p.}"
}

@techreport{paine1968stratigraphy21,
    author = "Paine, R",
    title = "Stratigraphy and sedimentation of subsurface Hackberry wedge and associated beds of southwestern Louisiana",
    year = "1968",
    howpublished = "American Association of Petroleum Geologists Bulletin, v. 52, p. 322-342",
    note = "talkorigins\_source = {true}; raw\_reference = {Paine, R., 1968, Stratigraphy and sedimentation of subsurface Hackberry wedge and associated beds of southwestern Louisiana: American Association of Petroleum Geologists Bulletin, v. 52, p. 322-342.}"
}

@techreport{scholl1970peruchile24,
    author = "Scholl, D. W. et al",
    title = "Peru-Chile Trench sediments and sea-floor spreading",
    year = "1970",
    howpublished = "Geological Society of America Bulletin, v. 81, p. 1339-1360",
    note = "talkorigins\_source = {true}; raw\_reference = {Scholl, D. W. et al., 1970, Peru-Chile Trench sediments and sea-floor spreading: Geological Society of America Bulletin, v. 81, p. 1339-1360.}"
}

@misc{samsonov1977epigenetic23,
    author = "Samsonov, V. V. et al",
    title = "Epigenetic cementation of terrigenous collectors and special features of bitumonites spreading on the southern slope of the Nepskii arch",
    year = "1977",
    howpublished = "Geology of Oil and Gas, v. 2, p. 18-25",
    note = "talkorigins\_source = {true}; raw\_reference = {Samsonov, V. V. et al., 1977, Epigenetic cementation of terrigenous collectors and special features of bitumonites spreading on the southern slope of the Nepskii arch: Geology of Oil and Gas, v. 2, p. 18-25.}"
}

@misc{biederman1978crudeoil2,
    author = "Biederman, E. W",
    title = "Crude-oil Composition and Migration, in Fairbridge, R. W., and Bourgeois, J., eds., The Encyclopedia of Sedimentology",
    year = "1978",
    howpublished = "Stroudsburg, Pa., Dowden, Hutchinson, and Ross, p. 212-220",
    note = "talkorigins\_source = {true}; raw\_reference = {Biederman, E. W., 1978, Crude-oil Composition and Migration, in Fairbridge, R. W., and Bourgeois, J., eds., The Encyclopedia of Sedimentology: Stroudsburg, Pa., Dowden, Hutchinson, and Ross, p. 212-220.}"
}

@misc{braitsch1978marine3,
    author = "Braitsch, O. and Kinsman, D. J",
    title = "Marine evaporites--diagenesis and metamorphism, in Fairbridge, R. W., and Bourgeois, J., eds., The Encyclopedia of Sedimentology",
    year = "1978",
    howpublished = "Stroudsburg, Pa., Dowden, Hutchinson and Ross, p. 464-468",
    note = "talkorigins\_source = {true}; raw\_reference = {Braitsch, O., and Kinsman, D. J., 1978, Marine evaporites--diagenesis and metamorphism, in Fairbridge, R. W., and Bourgeois, J., eds., The Encyclopedia of Sedimentology: Stroudsburg, Pa., Dowden, Hutchinson and Ross, p. 464-468.}"
}

@misc{briggs1978evaporite4,
    author = "Briggs, L. I",
    title = "Evaporite Facies, in Fairbridge, R. W., and Bourgeois, J., eds., The Encyclopedia of Sedimentology",
    year = "1978",
    howpublished = "Stroudsburg, Pa., Dowden, Hutchinson and Ross, p. 300-303",
    note = "talkorigins\_source = {true}; raw\_reference = {Briggs, L. I., 1978, Evaporite Facies, in Fairbridge, R. W., and Bourgeois, J., eds., The Encyclopedia of Sedimentology: Stroudsburg, Pa., Dowden, Hutchinson and Ross, p. 300-303.}"
}

@misc{fairbridge1978the5,
    author = "Fairbridge, R. W. and Bourgeois, J",
    title = "The Encyclopedia of Sedimentology",
    year = "1978",
    howpublished = "Stroudsburg, Pa., Dowden, Hutchinson and Ross, 901 p",
    note = "talkorigins\_source = {true}; raw\_reference = {Fairbridge, R. W., and Bourgeois, J., 1978, The Encyclopedia of Sedimentology: Stroudsburg, Pa., Dowden, Hutchinson and Ross, 901 p.}"
}

@book{freidman1978principles7,
    author = "Freidman, G. M. and Sanders, J. E",
    title = "Principles of Sedimentology",
    year = "1978",
    publisher = "New York, John Wiley and Sons, 972 p",
    note = "talkorigins\_source = {true}; raw\_reference = {Freidman, G. M., and Sanders, J. E., 1978, Principles of Sedimentology: New York, John Wiley and Sons, 972 p.}"
}

@misc{horis1978lacustrine8,
    author = "Horis, S",
    title = "Lacustrine Sedimentation, in Fairbridge, R. W., and Bourgeois, J., eds., The Encyclopedia of Sedimentology",
    year = "1978",
    howpublished = "Stroudsburg, Pa., Dowden, Hutchinson and Ross, p. 421-427",
    note = "talkorigins\_source = {true}; raw\_reference = {Horis, S., 1978, Lacustrine Sedimentation, in Fairbridge, R. W., and Bourgeois, J., eds., The Encyclopedia of Sedimentology: Stroudsburg, Pa., Dowden, Hutchinson and Ross, p. 421-427.}"
}

@misc{landis1978coal12,
    author = "Landis, E. R. and Averitt, P",
    title = "Coal, in Fairbridge, R. W., and Bourgeois, J., eds., The Encyclopedia of Sedimentology",
    year = "1978",
    howpublished = "Stroudsburg, Pa., Dowden, Hutchinson and Ross, p. 165-167",
    note = "talkorigins\_source = {true}; raw\_reference = {Landis, E. R., and Averitt, P., 1978, Coal, in Fairbridge, R. W., and Bourgeois, J., eds., The Encyclopedia of Sedimentology: Stroudsburg, Pa., Dowden, Hutchinson and Ross, p. 165-167.}"
}

@misc{morner1978varves19,
    author = "Morner, N.-A",
    title = "Varves and Varved Clay, in Fairbridge, R. W., and Bourgeois, J., eds., Encyclopedia of Sedimentology",
    year = "1978",
    howpublished = "Stroudsburg, Pa., Dowden, Hutchinson and Ross, p. 841-843",
    note = "talkorigins\_source = {true}; raw\_reference = {Morner, N.-A., 1978, Varves and Varved Clay, in Fairbridge, R. W., and Bourgeois, J., eds., Encyclopedia of Sedimentology: Stroudsburg, Pa., Dowden, Hutchinson and Ross, p. 841-843.}"
}

@misc{thurston1978chert25,
    author = "Thurston, D. R",
    title = "Chert and Flint, in Fairbridge, R. W., and Bourgeois, J., eds., The Encyclopedia of Sedimentology",
    year = "1978",
    howpublished = "Stroudsburg, Pa., Dowden, Hutchinson and Ross, p. 119-124",
    note = "talkorigins\_source = {true}; raw\_reference = {Thurston, D. R., 1978, Chert and Flint, in Fairbridge, R. W., and Bourgeois, J., eds., The Encyclopedia of Sedimentology: Stroudsburg, Pa., Dowden, Hutchinson and Ross, p. 119-124.}"
}

@misc{wszolek1978petroleumorigin27,
    author = "Wszolek, P. C. and Burlingame, A. L",
    title = "Petroleum--Origin and Evolution, in Fairbridge, R. W., and Bourgeois, J., eds., The Encyclopedia of Sedimentology",
    year = "1978",
    howpublished = "Stroudsburg, Pa., Dowden, Hutchinson and Ross, p. 565-574",
    note = "talkorigins\_source = {true}; raw\_reference = {Wszolek, P. C., and Burlingame, A. L., 1978, Petroleum--Origin and Evolution, in Fairbridge, R. W., and Bourgeois, J., eds., The Encyclopedia of Sedimentology: Stroudsburg, Pa., Dowden, Hutchinson and Ross, p. 565-574.}"
}

@article{poag1979stratigraphy,
    author = "Poag, C. Wylie",
    title = "Stratigraphy and Depositional Environments of Baltimore Canyon Trough",
    year = "1979",
    journal = "AAPG Bulletin",
    abstract = "The Baltimore Canyon Trough, lying offshore from the United States Middle Atlantic States, contains a thickness of at least 14 km of marine and nonmarine sedimentary rocks. One deep offshore stratigraphic test (COST B-2 well), several wells on the coastal plain, 18 shallow core holes (Deep Sea Drilling Project, Atlantic Slope Project, and Atlantic Margin Coring Project) on the continental shelf and slope, and scattered oceanographic cores and dredgings provide rich foraminiferal assemblages from which the geologic age and depositional environments have been determined. The oldest sedimentary rocks penetrated are Upper Jurassic terrigenous sandstone and shale, which are interspersed with shallow-marine limestone. Lower Cretaceous rocks, where penetrated, are also chiefly terrigenous sandstone and shale, but Upper Cretaceous rocks are progressively more marine. Paleogene strata reflect even deeper marine conditions (bathyal carbonate deposits in the B-2 well). In the Neogene, terrigenous clastic deposits replaced the Paieogene carbonate sequences throughout the trough. Deposition began with thick (\>800 m) deltaic beds in the Miocene and Pliocene and culminated in sandy and, in many places, nonfofesiHferous strata of the Pleistocene shelf. Surprisingly thick (\>300 m) silty and sandy clay composes the Pleistocene section on the continental slope. These stratigraphic and paleoecologic relations are graphically illustrated in eight geologic cross sections parallel with and perpendicular to the axis of the trough.",
    url = "https://doi.org/10.1306/2f9185bd-16ce-11d7-8645000102c1865d",
    doi = "10.1306/2f9185bd-16ce-11d7-8645000102c1865d",
    number = "9",
    pages = "1452-1466",
    volume = "63"
}

@book{leipzig1980foraminiferal13,
    author = "Leipzig, M. R",
    title = "Foraminiferal Biodiversity and Recent Sedimentation Rates From Grab-Samples; Point Arena, California [BS dissert.]",
    year = "1980",
    publisher = "University of Wisconsin-Parkside, 67 p",
    note = "talkorigins\_source = {true}; raw\_reference = {Leipzig, M. R., 1980, Foraminiferal Biodiversity and Recent Sedimentation Rates From Grab-Samples; Point Arena, California [BS dissert.]: University of Wisconsin-Parkside, 67 p.}"
}

@misc{howell1982sedimentology9,
    author = "Howell, D. G. and Normark, W. R",
    title = "Sedimentology of submarine fans, in Scholle, P. A., and Spearing, D. R., eds., Sandstone depositional environments, 31 of AAPG Memoirs",
    year = "1982",
    howpublished = "Tulsa, OK, AAPG, p. 365-404",
    note = "talkorigins\_source = {true}; raw\_reference = {Howell, D. G., and Normark, W. R., 1982, Sedimentology of submarine fans, in Scholle, P. A., and Spearing, D. R., eds., Sandstone depositional environments, 31 of AAPG Memoirs: Tulsa, OK, AAPG, p. 365-404.}"
}

@book{leipzig1982stratigraphy14,
    author = "Leipzig, M. R",
    title = "Stratigraphy, Sedimentation and Depositional Environments of the Late Cretaceous Pictured Cliffs Sandstone, Fruitland Formation, Kirtland Shale and Early Tertiary Ojo Alamo Sandstone; Eastern San Juan Basin, New Mexico [MS dissert.]",
    year = "1982",
    publisher = "University of Wisconsin-Milwaukee, 555 p",
    note = "talkorigins\_source = {true}; raw\_reference = {Leipzig, M. R., 1982, Stratigraphy, Sedimentation and Depositional Environments of the Late Cretaceous Pictured Cliffs Sandstone, Fruitland Formation, Kirtland Shale and Early Tertiary Ojo Alamo Sandstone; Eastern San Juan Basin, New Mexico [MS dissert.]: University of Wisconsin-Milwaukee, 555 p.}"
}

@techreport{leipzig1984stratigraphy15,
    author = "Leipzig, M. R",
    title = "Stratigraphy, Sedimentology and Depositional Environments of the Late Cretaceous/Early Tertiary Transition, Eastern San Juan Basin, New Mexico",
    year = "1984",
    howpublished = "New Mexico Bureau of Mines and Mineral Resources Bulletin, v. 142, no. 5, p. 109-256",
    note = "talkorigins\_source = {true}; raw\_reference = {Leipzig, M. R., 1984, Stratigraphy, Sedimentology and Depositional Environments of the Late Cretaceous/Early Tertiary Transition, Eastern San Juan Basin, New Mexico: New Mexico Bureau of Mines and Mineral Resources Bulletin, v. 142, no. 5, p. 109-256.}"
}

@incollection{roberts1984sedimentology,
    author = "Roberts, Harry H. and Thayer, Paul",
    title = "SEDIMENTOLOGY OF DEPOSITIONAL ENVIRONMENTS ENCOUNTERED IN DSDP LEG 96 BORINGS",
    year = "1984",
    booktitle = "Characteristics of Gulf Basin Deep-Water Sediments and Their Exploration Potential",
    url = "https://doi.org/10.5724/gcs.84.05.0086",
    doi = "10.5724/gcs.84.05.0086",
    pages = "86-87"
}

@misc{gibson1985stratigraphy,
    author = "Gibson, D W",
    title = "Stratigraphy, sedimentology and depositional environments of the coal-bearing Jurassic-Cretaceous Kootenay Group, Alberta and British Columbia",
    year = "1985",
    abstract = "Strata of the Jurassic-Cretaceous Kootenay Group have long been of economic interest as a readily accessible source of thermal and metallurgical coal. This report attempts to synthesize and describe the geology of the Kootenay Group on a regional basis, by providing detailed information and data on lithofacies, lithofacies relationships, correlation of major rock units, the distribution and continuity of coal seams, and major environments of deposition. The Kootenay Group, up to 1112 m thick, comprises three formations which, in ascending order, are: the Morrissey, which ranges in measured thickness from 20 to 80 m and comprises a massive cliff-forming succession of fine- to medium-grained sandstone; the Mist Mountain, ranging in measured thickness from 25 to 665 m and comprising an interbedded succession of predominantly nonmarine sandstone, siltstone, mudstone, rare conglomerate, and economically important thin to thick seams of coal; and the Elk, ranging in measured thickness from a zero erosional edge to 590 m and comprising an interbedded sequence of nonmarine sandstone, siltstone, mudstone, shale and, locally, chert-pebble conglomerate and thin seams of coal. The Morrissey Formation can be further subdivided throughout most of the area into the Weary Ridge (lower) and Moose Mountain members. Economically, the Mist Mountain Formation is the most important formation of the Kootenay Group, containing coal seams up to 18 m thick, which range in rank from medium to high volatile bituminous in the south, to low volatile bituminous to semianthracite in the north. Seams are thicker and more numerous in areas of the Fernie Basin and upper Elk River valley. Coal seams in the Elk Formation are thin, less abundant, regionally discontinuous, and generally lower in rank than those in the Mist Mountain Formation. Coal in the Morrissey Formation is rare and of no economic value. Petrographic analyses of many thin sections from the Kootenay Group indicate two main detrital components, quartz and lithic rock fragments, the latter including several varieties of chert; grains and pebbles of sedimentary quartzite or quartz arenite; grains of dolostone and limestone, commonly sandy to silty; grains and pebbles of silicified mudstone-argillite; and grains of collophane. The cement consists predominantly of quartz and chert, and less commonly dolomite, calcite and rare clay minerals. Composition and textural relationships indicate that most, if not all, detrital components were derived from pre-existing sedimentary rocks located east of the Rocky Mountain Trench. The analysis of sedimentary facies, facies relationships, petrographic data, the presence or absence of characteristic megafossil, microfossil and microfloral assemblages, suggest that strata of the Kootenay Group formed part of a major, prograding, clastic wedge, deposited within three major depositional environments. The Morrissey Formation is diagnosed as a beach, beach ridge, and coastal dune depositional environment. The overlying Mist Mountain Formation is interpreted as a fluvial-deltaic-interdeltaic clastic succession, deposited in an environment largely unaffected by marine or brackish water inundations. The Elk Formation represents deposition within a major, coastal, fluvial-alluvial plain depositional environment. In the Front Ranges of the southern Rocky Mountains, the Elk contains strata characteristic of a distal alluvial fan or braidplain depositional environment.",
    url = "https://doi.org/10.4095/120289",
    doi = "10.4095/120289"
}

@book{olsen1986correlation20,
    author = "Olsen, P. E. and Sues, H.-D",
    title = "Correlation of continental Late Triassic and Early Jurassic sediments, and patterns of the Triassic-Jurassic transition, in Padian, K., ed., The Beginning of the Age of Dinosaurs",
    year = "1986",
    publisher = "Cambridge, Cambridge University Press, p. 321-351",
    note = "talkorigins\_source = {true}; raw\_reference = {Olsen, P. E., and Sues, H.-D., 1986, Correlation of continental Late Triassic and Early Jurassic sediments, and patterns of the Triassic-Jurassic transition, in Padian, K., ed., The Beginning of the Age of Dinosaurs: Cambridge, Cambridge University Press, p. 321-351.}"
}

@incollection{jerzykiewicz1987semiarid10,
    author = "Jerzykiewicz, T. and Sweet, A. R",
    editor = "Currie, P. J. and Koster, E.",
    title = "Semiarid Floodplain as a Paleoenvironmental Setting of the Upper Cretaceous Dinosaurs: Sedimentological Evidence from Mongolia and Alberta",
    year = "1987",
    booktitle = "Fourth Symposium on Mesozoic Terrestrial Ecosystems",
    publisher = "Drumheller, Canada, Tyrrell Museum, p. 120-124",
    note = "talkorigins\_source = {true}; raw\_reference = {Jerzykiewicz, T., and Sweet, A. R., 1987, Semiarid Floodplain as a Paleoenvironmental Setting of the Upper Cretaceous Dinosaurs: Sedimentological Evidence from Mongolia and Alberta, in Currie, P. J., and Koster, E., eds., Fourth Symposium on Mesozoic Terrestrial Ecosystems: Drumheller, Canada, Tyrrell Museum, p. 120-124.}"
}

@phdthesis{leipzig1989the16,
    author = "Leipzig, M. R",
    title = "The Stratigraphy, Sedimentology and Depositional Environments of the Late Cretaceous Pictured Cliffs Sandstone, Fruitland and Kirtland Formations and the Early Tertiary Ojo Alamo Sandstone. Eastern San Juan Basin, New Mexico. The Saga Continues [PhD dissert.]",
    year = "1989",
    publisher = "University of Wisconsin - Milwaukee and Madison, 978 p",
    note = "talkorigins\_source = {true}; raw\_reference = {Leipzig, M. R., 1989, The Stratigraphy, Sedimentology and Depositional Environments of the Late Cretaceous Pictured Cliffs Sandstone, Fruitland and Kirtland Formations and the Early Tertiary Ojo Alamo Sandstone. Eastern San Juan Basin, New Mexico. The Saga Continues [PhD dissert.]: University of Wisconsin - Milwaukee and Madison, 978 p.}"
}

@misc{naylor1989stratigraphy,
    author = "Naylor, R D and Kalkreuth, W D and Smith, W D and Yeo, G M",
    title = "Stratigraphy, sedimentology and depositional environments of the coal-bearing Stellarton Formation, Nova Scotia",
    year = "1989",
    url = "https://doi.org/10.4095/126738",
    doi = "10.4095/126738"
}

@misc{leipzig1990the17,
    author = "Leipzig, M. R",
    title = "The stratigraphy, electrofacies and depositional environments of the Reklaw Formation of Goliad and adjacent counties, south Texas",
    year = "1990",
    howpublished = "American Association of Petroleum Geologists, v. 215, no. 1, p. 76-84",
    note = "talkorigins\_source = {true}; raw\_reference = {Leipzig, M. R., 1990, The stratigraphy, electrofacies and depositional environments of the Reklaw Formation of Goliad and adjacent counties, south Texas: American Association of Petroleum Geologists, v. 215, no. 1, p. 76-84.}"
}

@misc{leipzig1990the18,
    author = "Leipzig, M. R. and Jetelina, D",
    title = "The Gibbs Sand- A new Wilcox reservoir in south Texas. Geologic and engineering considerations",
    year = "1990",
    howpublished = "American Association of Petroleum Geologists; In Prep",
    note = "talkorigins\_source = {true}; raw\_reference = {Leipzig, M. R., and Jetelina, D., 1990, The Gibbs Sand- A new Wilcox reservoir in south Texas. Geologic and engineering considerations: American Association of Petroleum Geologists; In Prep.}"
}

@article{persson1990sedimentology,
    author = "PERSSON, KÄRSTIN MALMBERG and LAGERLUND, ERIK",
    title = "Sedimentology and depositional environments of the Lund Diamicton, southern Sweden",
    year = "1990",
    journal = "Boreas",
    abstract = "The Lund Diamicton (earlier named Lund Till) in SW Skåne, S. Sweden, is a glacioaquatic sediment consisting of clay and massive and laminated diamictons. It is characterized by clasts derived from the Baltic depression and its depositional history can be summarized as follows: After deglaciation, large fields of stagnant ice remained in the area and a periglacial land surface with ice‐wedge polygons and wind‐abraded clasts was developed in ice‐free areas. A transgression followed and a clay/diamicton sediment was deposited, partly on top of stagnant ice and against a coastal barrier of stagnant ice along large parts of the basin boundary. This sediment is the Lund Diamicton. The main depositional processes were: fall‐out of clay from suspension, sediment gravity flow from stagnant ice and icebergs and rain‐out of debris from floating icebergs. The unit was extensively deformed by escaping pore water, loading, flow and due to melting of buried ice. The Lund Diamicton is the equivalent in this area of the classical ‘Low Baltic till’, which has been interpreted as a basal till deposited by the ‘Low Baltic ice stream’. The present study concludes that this unit is instead a glacioaquatic sediment deposited during a transgression in the Öresund area. Its boundary represents the highest coastline and not the margin of a glacier.",
    url = "https://doi.org/10.1111/j.1502-3885.1990.tb00578.x",
    doi = "10.1111/j.1502-3885.1990.tb00578.x",
    number = "2",
    pages = "181-199",
    volume = "19"
}

@article{sanders1999rudist,
    author = "Sanders, Diethard and Pons, Josep Maria",
    title = "Rudist formations in mixed siliciclastic-carbonate depositional environments, Upper Cretaceous, Austria: stratigraphy, sedimentology, and models of development",
    year = "1999",
    journal = "Palaeogeography, Palaeoclimatology, Palaeoecology",
    url = "https://doi.org/10.1016/s0031-0182(98)00186-2",
    doi = "10.1016/s0031-0182(98)00186-2",
    number = "4",
    pages = "249-284",
    volume = "148"
}

@incollection{mandel2002stratigraphy,
    author = "Mandel, Rolfe D.",
    title = "Stratigraphy and Sedimentology",
    year = "2002",
    booktitle = "Interdisciplinary Contributions to Archaeology",
    url = "https://doi.org/10.1007/0-306-47162-0\_3",
    doi = "10.1007/0-306-47162-0\_3",
    pages = "49-69"
}

@inproceedings{maurer2009primary,
    author = "Maurer, F. and Rettori, R. and Cirilli, S. and Hillgärtner, H.",
    title = "Primary Category - Sedimentology and Stratigraphy, and Depositional Environments (e.g. Framework for Geological Modelling)",
    year = "2009",
    booktitle = "IPTC 2009: International Petroleum Technology Conference",
    url = "https://doi.org/10.3997/2214-4609-pdb.151.iptc13108",
    doi = "10.3997/2214-4609-pdb.151.iptc13108"
}

@inproceedings{wilson2009stratigraphy,
    author = "Wilson, C.R. and Le Heron, D.P. and Armstrong, H.A. and Gindre, L.",
    title = "Stratigraphy, Sedimentology and Depositional Environments of the Late Ordovician Succession in Al Kufrah Basin, SE Libya",
    year = "2009",
    booktitle = "4th EAGE North African/Mediterranean Petroleum and Geosciences Conference and Exhibition Tunis 2009",
    url = "https://doi.org/10.3997/2214-4609.20145807",
    doi = "10.3997/2214-4609.20145807"
}

@article{webster2010sedimentology,
    author = "Webster, R.",
    title = "Sedimentology and Stratigraphy",
    year = "2010",
    journal = "European Journal of Soil Science",
    url = "https://doi.org/10.1111/j.1365-2389.2009.01225.x",
    doi = "10.1111/j.1365-2389.2009.01225.x",
    number = "2",
    pages = "315-316",
    volume = "61"
}