Woodbine formation

@misc{stephenson1953mollusks,
    author = "Stephenson, L.W.",
    title = "Mollusks from the Pepper shale member of the Woodbine formation, McLennan County, Texas",
    year = "1953",
    booktitle = "Professional Paper",
    url = "https://doi.org/10.3133/pp243e",
    doi = "10.3133/pp243e"
}

@article{oliver1970depositional,
    author = "Oliver, William B.",
    title = "Depositional Systems in Woodbine Formation (Upper Cretaceous), Northeast Texas: ABSTRACT",
    year = "1970",
    journal = "AAPG Bulletin",
    url = "https://doi.org/10.1306/5d25cc1d-16c1-11d7-8645000102c1865d",
    doi = "10.1306/5d25cc1d-16c1-11d7-8645000102c1865d",
    volume = "54"
}

@misc{andoliver1971depositional,
    author = "Oliver, William",
    title = "Depositional Systems in the Woodbine Formation (Upper Cretaceous), Northeast Texas",
    year = "1971",
    booktitle = "Report Investigation",
    url = "https://doi.org/10.23867/ri0073d",
    doi = "10.23867/ri0073d"
}

The Woodbine Formation is composed largely of terrigenous sediment eroded from Paleozoic sedimentary and weakly metamorphosed sedimentary rocks of the Ouachita Mountains in southern Oklahoma and Arkansas, and subsequently deposited in a complex of nearshore environments along the margins of the broadly subsiding Northeast Texas basin. Three principal depositional systems are recognized in Woodbine rocks—a fluvial system, a high-destructive delta system, and a shelf-strandplain system. Their recognition is based on a regional outcrop and subsurface investigation in which external geometry of framework sandstone was integrated with lithology, sedimentary structures, fossil distribution, and bounding relations. Two components of the fluvial system, a tributary channel sandstone facies and a meander belt sandstone facies, are developed in the Dexter Member (lower Woodbine) northeast of a line from Dallas to Tyler. On the south and southwest, a high-destructive delta system is persistent throughout the entire Woodbine section. The 3 component facies of the delta system are: progradational channel-mouth bar sands; coastal barrier sands, deposited along shore adjacent to the channel mouth; and prodelta-shelf muds. The Lewisville (upper Woodbine) shelf-strandplain system, developed in the northern third of the basin marginal to principal deltaic facies, is composed of 2 facies: shelf muds and strandplain sands that accumulated along shore. Near the end of Woodbine deposition, but before transgression by Eagle Ford seas, emergence of the Sabine uplift resulted in erosion of Woodbine sediments, which were subsequently redeposited along margins of the uplift as the Harris sand.

@article{oliver1971depositional,
    author = "Oliver, William",
    title = "Depositional Systems in Woodbine Formation (Upper Cretaceous), Northeast Texas: ABSTRACT",
    year = "1971",
    journal = "AAPG Bulletin",
    abstract = "The Woodbine Formation is composed largely of terrigenous sediment eroded from Paleozoic sedimentary and weakly metamorphosed sedimentary rocks of the Ouachita Mountains in southern Oklahoma and Arkansas, and subsequently deposited in a complex of nearshore environments along the margins of the broadly subsiding Northeast Texas basin. Three principal depositional systems are recognized in Woodbine rocks—a fluvial system, a high-destructive delta system, and a shelf-strandplain system. Their recognition is based on a regional outcrop and subsurface investigation in which external geometry of framework sandstone was integrated with lithology, sedimentary structures, fossil distribution, and bounding relations. Two components of the fluvial system, a tributary channel sandstone facies and a meander belt sandstone facies, are developed in the Dexter Member (lower Woodbine) northeast of a line from Dallas to Tyler. On the south and southwest, a high-destructive delta system is persistent throughout the entire Woodbine section. The 3 component facies of the delta system are: progradational channel-mouth bar sands; coastal barrier sands, deposited along shore adjacent to the channel mouth; and prodelta-shelf muds. The Lewisville (upper Woodbine) shelf-strandplain system, developed in the northern third of the basin marginal to principal deltaic facies, is composed of 2 facies: shelf muds and strandplain sands that accumulated along shore. Near the end of Woodbine deposition, but before transgression by Eagle Ford seas, emergence of the Sabine uplift resulted in erosion of Woodbine sediments, which were subsequently redeposited along margins of the uplift as the Harris sand.",
    url = "https://doi.org/10.1306/5d25ce07-16c1-11d7-8645000102c1865d",
    doi = "10.1306/5d25ce07-16c1-11d7-8645000102c1865d",
    number = "1",
    pages = "156-156",
    volume = "55"
}

@article{johnson1976lithofacies,
    author = "Johnson, Ron",
    title = "Lithofacies and Depositional Environments of Rush Creek Member of Woodbine Formation, North-Central Texas: ABSTRACT",
    year = "1976",
    journal = "AAPG Bulletin",
    url = "https://doi.org/10.1306/83d92393-16c7-11d7-8645000102c1865d",
    doi = "10.1306/83d92393-16c7-11d7-8645000102c1865d",
    volume = "60"
}

@article{seimers1978submarine2,
    author = "Seimers, C. T",
    title = "Submarine fan deposition of the Woodbine-Eagleford interval (Upper Creatceous), Tyler County, Texas",
    year = "1978",
    journal = "Gulf Coast Association of Geological Societies Transactions, v. 28, p. 493-533",
    note = "talkorigins\_source = {true}; raw\_reference = {Seimers, C. T., 1978, Submarine fan deposition of the Woodbine-Eagleford interval (Upper Creatceous), Tyler County, Texas: Gulf Coast Association of Geological Societies Transactions, v. 28, p. 493-533.}"
}

@article{siemers1978submarinefan,
    author = "Siemers, Charles T.",
    title = "Submarine-Fan Deposition of Woodbine Formation (Upper Cretaceous), Central Tyler County, Texas--Subsurface Core Study: ABSTRACT",
    year = "1978",
    journal = "AAPG Bulletin",
    url = "https://doi.org/10.1306/c1ea5355-16c9-11d7-8645000102c1865d",
    doi = "10.1306/c1ea5355-16c9-11d7-8645000102c1865d",
    volume = "62"
}

@article{foss1979depositional1,
    author = "Foss, D. C",
    title = "Depositional environment of Woodbine sandstones, Polk County, Texas",
    year = "1979",
    journal = "Gulf Coast Association of Geological Societies Transactions, v. 29, p. 83-94",
    note = "talkorigins\_source = {true}; raw\_reference = {Foss, D. C., 1979, Depositional environment of Woodbine sandstones, Polk County, Texas: Gulf Coast Association of Geological Societies Transactions, v. 29, p. 83-94.}"
}

@article{newport1981age,
    author = "Newport, R. Leo",
    title = "Age, Depositional Environment, and Organic Metamorphism of Woodbine (Cretaceous) of Polk County, Texas: ABSTRACT",
    year = "1981",
    journal = "AAPG Bulletin",
    url = "https://doi.org/10.1306/03b5988c-16d1-11d7-8645000102c1865d",
    doi = "10.1306/03b5988c-16d1-11d7-8645000102c1865d",
    volume = "65"
}

@article{robertrberg1985woodbine,
    author = "Robert R. Berg, John T. Leethem",
    title = "Woodbine Reservoir Facies, Kurten Field, Brazos County, Texas: ABSTRACT",
    year = "1985",
    journal = "AAPG Bulletin",
    url = "https://doi.org/10.1306/ad461bba-16f7-11d7-8645000102c1865d",
    doi = "10.1306/ad461bba-16f7-11d7-8645000102c1865d",
    volume = "69"
}

@article{carden1986petroleum,
    author = "Carden, Michael",
    title = "Petroleum Geology of Woodbine Formation, Freestone County, Texas: ABSTRACT",
    year = "1986",
    journal = "AAPG Bulletin",
    url = "https://doi.org/10.1306/94885a7f-1704-11d7-8645000102c1865d",
    doi = "10.1306/94885a7f-1704-11d7-8645000102c1865d",
    volume = "70"
}

@article{dedominic1988deposition,
    author = "Dedominic, Joseph R.",
    title = "Deposition of Woodbine-Eagle Ford Sandstones, Aggieland Field, Brazos County, Texas: ABSTRACT",
    year = "1988",
    journal = "AAPG Bulletin",
    url = "https://doi.org/10.1306/703c9811-1707-11d7-8645000102c1865d",
    doi = "10.1306/703c9811-1707-11d7-8645000102c1865d",
    volume = "72"
}