Oligocene

@article{hershalcferguson1960turtle,
    author = "Hershal C. Ferguson, Jr.",
    title = "Turtle Bayou-Kent Bayou-North Turtle Bayou Complex: ABSTRACT",
    year = "1960",
    journal = "AAPG Bulletin",
    url = "https://doi.org/10.1306/0bda61ee-16bd-11d7-8645000102c1865d",
    doi = "10.1306/0bda61ee-16bd-11d7-8645000102c1865d",
    volume = "44"
}

@article{paterson1967tertiary,
    author = "Paterson, SJ",
    title = "Tertiary deep lead deposits, Moina Area",
    year = "1967",
    journal = "Papers and proceedings of the Royal Society of Tasmania",
    url = "https://doi.org/10.26749/ptxo6653",
    doi = "10.26749/ptxo6653",
    pages = "251-262",
    volume = "101.0"
}

@article{benson1971geology,
    author = "Benson, Paul H.",
    title = "Geology of Oligocene Hackberry Trend, Gillis English Bayou--Manchester Area, Calcasieu Parish, Louisiana: ABSTRACT",
    year = "1971",
    journal = "AAPG Bulletin",
    url = "https://doi.org/10.1306/819a3d44-16c5-11d7-8645000102c1865d",
    doi = "10.1306/819a3d44-16c5-11d7-8645000102c1865d",
    volume = "55"
}

@article{benson1971geology1,
    author = "Benson, P. H",
    title = "Geology of the Oligocene Hackberry trend, Gillis English Bayou - Manchester area, Calcasieu Parish, Louisiana",
    year = "1971",
    journal = "Gulf Coast Association of Geological Societies Transactions, v. 21, p. 1-14",
    note = "talkorigins\_source = {true}; raw\_reference = {Benson, P. H., 1971, Geology of the Oligocene Hackberry trend, Gillis English Bayou - Manchester area, Calcasieu Parish, Louisiana: Gulf Coast Association of Geological Societies Transactions, v. 21, p. 1-14.}"
}

@article{hiscott1981deep2,
    author = "Hiscott, R. N",
    title = "Deep sea fan deposits in the Macigno Formation (Middle- Upper Oilgocene) of the Gordana Valley, Northern Appennines, Italy",
    year = "1981",
    journal = "Discussion: Journal of Sedimentary Petrology, v. 51, p. 1015-1021",
    note = "talkorigins\_source = {true}; raw\_reference = {Hiscott, R. N., 1981, Deep sea fan deposits in the Macigno Formation (Middle- Upper Oilgocene) of the Gordana Valley, Northern Appennines, Italy: Discussion: Journal of Sedimentary Petrology, v. 51, p. 1015-1021.}"
}

@article{thomaseewing1984thermal,
    author = "Thomas E. Ewing, Malcolm P. R. Ligh",
    title = "Thermal and Diagenetic History of Pleasant Bayou-Chocolate Bayou Area, Brazoria County, Texas: ABSTRACT",
    year = "1984",
    journal = "AAPG Bulletin",
    url = "https://doi.org/10.1306/ad4617dc-16f7-11d7-8645000102c1865d",
    doi = "10.1306/ad4617dc-16f7-11d7-8645000102c1865d",
    volume = "68"
}

@article{guth1985calcasieu,
    author = "Guth, Edwin F.",
    title = "Calcasieu Aglow",
    year = "1985",
    journal = "Lighting Design + Application",
    url = "https://doi.org/10.1177/036063258501501012",
    doi = "10.1177/036063258501501012",
    number = "10",
    pages = "24-26",
    volume = "15"
}

@incollection{crossref1986the,
    title = "The Eocene/Oligocene Boundary in Deep Sea Deposits",
    year = "1986",
    booktitle = "Developments in Palaeontology and Stratigraphy",
    url = "https://doi.org/10.1016/s0920-5446(08)70122-5",
    doi = "10.1016/s0920-5446(08)70122-5",
    pages = "203-207"
}

@article{spencer1993deepseated,
    author = "SPENCER, JEFFREY A. and L., CHARLES",
    title = "Deep-Seated Salt Sheet: Eastern Calcasieu Parish, Louisiana",
    year = "1993",
    journal = "AAPG Bulletin",
    url = "https://doi.org/10.1306/bdff7d2c-1718-11d7-8645000102c1865d",
    doi = "10.1306/bdff7d2c-1718-11d7-8645000102c1865d",
    volume = "77"
}

@article{custer2006contaminant,
    author = "Custer, Thomas W. and Custer, Christine M. and Goatcher, Buddy L. and Melancon, Mark J. and Matson, Cole W. and Bickham, John W.",
    title = "Contaminant Exposure of Barn Swallows Nesting on Bayou D'Inde, Calcasieu Estuary, Louisiana, USA",
    year = "2006",
    journal = "Environmental Monitoring and Assessment",
    url = "https://doi.org/10.1007/s10661-005-9153-x",
    doi = "10.1007/s10661-005-9153-x",
    number = "1-3",
    pages = "543-560",
    volume = "121"
}

New data are reported on the stratigraphy of the Oligocene deposits of Lake Baikal (the Tankhoi field, the outcrops near the mouths of the Osinovka, Polovinka, and Klyuevka Rivers). Detailed paleontological analysis of the key sections on the continental part of the Baikal eastern coast revealed four floristic horizons that could be used as indicator horizons and showed that the Tankhoi Formation formed throughout the Oligocene and at the early Early Miocene. Lithologically, blue vivianite clays and coal beds could be used as the most important indicator horizons. Formation of the deposits began after a long stratigraphic break from the Early Cretaceous to the Early Oligocene. The deposits were formed by erosion and denudation of weathering crust and accumulation of redeposited weathering residues in the Tankhoi paleobasin with a lacustrine-marsh landscape. Coarse-clastic foehn deposits of the Osinovka Formation, containing rich Miocene palynological assemblages, were eroded and overlie concordantly the Upper Tankhoi Subformation and redeposited weathering residues of the weathering crust, and underlie the Anosovka Formation. The study suggests that the Baikal rift valley began to form at 38 Ma.

@article{mashchuk2012oligocene,
    author = "Mashchuk, I.M. and Akulov, N.I.",
    title = "Oligocene deposits of the Baikal rift valley",
    year = "2012",
    journal = "Russian Geology and Geophysics",
    abstract = "New data are reported on the stratigraphy of the Oligocene deposits of Lake Baikal (the Tankhoi field, the outcrops near the mouths of the Osinovka, Polovinka, and Klyuevka Rivers). Detailed paleontological analysis of the key sections on the continental part of the Baikal eastern coast revealed four floristic horizons that could be used as indicator horizons and showed that the Tankhoi Formation formed throughout the Oligocene and at the early Early Miocene. Lithologically, blue vivianite clays and coal beds could be used as the most important indicator horizons. Formation of the deposits began after a long stratigraphic break from the Early Cretaceous to the Early Oligocene. The deposits were formed by erosion and denudation of weathering crust and accumulation of redeposited weathering residues in the Tankhoi paleobasin with a lacustrine-marsh landscape. Coarse-clastic foehn deposits of the Osinovka Formation, containing rich Miocene palynological assemblages, were eroded and overlie concordantly the Upper Tankhoi Subformation and redeposited weathering residues of the weathering crust, and underlie the Anosovka Formation. The study suggests that the Baikal rift valley began to form at 38 Ma.",
    url = "https://doi.org/10.1016/j.rgg.2012.02.012",
    doi = "10.1016/j.rgg.2012.02.012",
    number = "4",
    pages = "356-366",
    volume = "53"
}

@incollection{shaltami2021oligocene,
    author = "Shaltami, Osama Rahil and Fares, Fares F. and Errishi, Hwedi and EL Oshebi, Farag M.",
    title = "Oligocene Deposits",
    year = "2021",
    booktitle = "SpringerBriefs in Earth System Sciences",
    url = "https://doi.org/10.1007/978-3-030-63010-2\_4",
    doi = "10.1007/978-3-030-63010-2\_4",
    pages = "41-59"
}