Eagleford formation

The San Luis Pass shallow salt dome lies about 7 miles offshore from the Texas coast under about 50 feet of water. A detailed submarine gravity survey was made to determine the outline, thickness and depth of caprock as a guide for test drilling for the evaluation of the dome as a sulphur prospect. There were no drilling contacts on the dome when the work was done. Seventeen test wells were subsequently drilled within the shallow dome outline as estimated from analysis of the gravity results. The caprock found was slightly smaller in area, considerably shallower in depth and of substantially the same thickness as predicted. The caprock material is nearly all gypsum.

@article{nettleton1957submarine,
    author = "Nettleton, Lewis Lomax",
    title = "Submarine gravity detailing, San Luis Pass dome, Brazoria County, Texas",
    year = "1957",
    journal = "Geophysics",
    abstract = "The San Luis Pass shallow salt dome lies about 7 miles offshore from the Texas coast under about 50 feet of water. A detailed submarine gravity survey was made to determine the outline, thickness and depth of caprock as a guide for test drilling for the evaluation of the dome as a sulphur prospect. There were no drilling contacts on the dome when the work was done. Seventeen test wells were subsequently drilled within the shallow dome outline as estimated from analysis of the gravity results. The caprock found was slightly smaller in area, considerably shallower in depth and of substantially the same thickness as predicted. The caprock material is nearly all gypsum.",
    url = "https://doi.org/10.1190/1.1438367",
    doi = "10.1190/1.1438367",
    number = "2",
    pages = "348-358",
    volume = "22"
}

@article{davis1970native,
    author = "Davis, J. B. and Kirkland, D. W.",
    title = "Native sulfur deposition in the Castile Formation, Culberson County, Texas",
    year = "1970",
    journal = "Economic Geology",
    url = "https://doi.org/10.2113/gsecongeo.65.2.107",
    doi = "10.2113/gsecongeo.65.2.107",
    number = "2",
    openalex = "W2037415867",
    pages = "107-121",
    volume = "65"
}

@misc{dickinson1976geologic,
    author = "Dickinson, Kendell A.",
    title = "Geologic controls of uranium deposition, Karnes County, Texas",
    year = "1976",
    booktitle = "Open-File Report",
    url = "https://doi.org/10.3133/ofr76331",
    doi = "10.3133/ofr76331",
    openalex = "W1521707859",
    references = "doi10130683d91d2116c711d78645000102c1865d, doi102113gsecongeo516495, doi102113gsecongeo592309, doi103133b1084a, doi103133pp765"
}

@article{seimers1978submarine1,
    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{ordonez1984permian,
    author = "Ordonez, Steve R.",
    title = "Permian (Guadalupian) Shelf Deposition and Diagenesis: Tansill Formation of Cheyenne Field, Winkler County, Texas: ABSTRACT",
    year = "1984",
    journal = "AAPG Bulletin",
    url = "https://doi.org/10.1306/ad4609bd-16f7-11d7-8645000102c1865d",
    doi = "10.1306/ad4609bd-16f7-11d7-8645000102c1865d",
    openalex = "W1995337112",
    volume = "68"
}

@article{richardchaack1984deposition,
    author = "Richard C. Haack, A. D. Jacka",
    title = "Deposition, Diagenesis, and Porosity Relationships in the Glorieta Formation, Keystone (Holt) Field, Winkler County, Texas: ABSTRACT",
    year = "1984",
    journal = "AAPG Bulletin",
    url = "https://doi.org/10.1306/ad460d96-16f7-11d7-8645000102c1865d",
    doi = "10.1306/ad460d96-16f7-11d7-8645000102c1865d",
    openalex = "W2149050902",
    volume = "68"
}

@article{galloway1985submarine,
    author = "Galloway, William E.",
    title = "Submarine Canyon System in Frio Formation of South Texas: ABSTRACT",
    year = "1985",
    journal = "AAPG Bulletin",
    url = "https://doi.org/10.1306/ad462ce0-16f7-11d7-8645000102c1865d",
    doi = "10.1306/ad462ce0-16f7-11d7-8645000102c1865d",
    openalex = "W2006995513",
    volume = "69"
}

@article{sidneyeglenn1986deposition,
    author = "Sidney E. Glenn, Alonzo D. Jacka",
    title = "Deposition, Diagenesis, and Porosity History of San Andres Formation, Shafter Lake Field, Andrews County, Texas: ABSTRACT",
    year = "1986",
    journal = "AAPG Bulletin",
    url = "https://doi.org/10.1306/948856b5-1704-11d7-8645000102c1865d",
    doi = "10.1306/948856b5-1704-11d7-8645000102c1865d",
    openalex = "W2153014917",
    volume = "70"
}

@article{moore1987environment,
    author = "Moore, Brian K.",
    title = "Environment of Deposition of Clear Fork Formation: Yoakum County, Texas: ABSTRACT",
    year = "1987",
    journal = "AAPG Bulletin",
    url = "https://doi.org/10.1306/94887541-1704-11d7-8645000102c1865d",
    doi = "10.1306/94887541-1704-11d7-8645000102c1865d",
    openalex = "W1973382313",
    volume = "71"
}

@article{miller1991lower,
    author = "{MILLER, RANDALL S., Reservoirs, Inc}",
    title = "Lower Wilcox Submarine Canyon Channel Sandstones, Sheridan Field, Colorado County, Texas",
    year = "1991",
    journal = "AAPG Bulletin",
    url = "https://doi.org/10.1306/0c9b2051-1710-11d7-8645000102c1865d",
    doi = "10.1306/0c9b2051-1710-11d7-8645000102c1865d",
    volume = "75"
}

Worldview-3 (WV3) 16-band multispectral data were used to map exposed bedrock and mine waste piles associated with legacy open-pit mining of sandstone-hosted roll-front uranium deposits along the South Texas Coastal Plain. We used the “spectral hourglass” approach to extract spectral endmembers representative of these features from the image. This approach first requires calibrating the imagery to reflectance, then masking for vegetation, followed by spatial and spectral data reduction using a principal component analysis-based procedure that reduces noise and identifies homogeneous targets which are “pure” enough to be considered spectral endmembers. In this case, we used a single WV3 image which covered an ~11.5 km by ~19.5 km area of Karnes, Atascosa and Live Oak Counties, underlain by mined rocks from the Jackson Group and Catahoula Formation. Up to 58 spectral endmembers were identified using a further multi-dimensional class segregation method and were used as inputs for spectral angle mapper (SAM) classification. SAM classification resulted in the identification of at least 117 mine- and mine waste-related features, most of which were previously unknown. Class similarity was further evaluated, and the dominant minerals in each class were identified by comparison to spectral libraries and measured samples of actual Jackson Group uranium host rocks. Redundant classes were eliminated, and SAM was run a second time using a reduced set of 23 endmembers, which were found to map these same features as effectively as using the full 58 set of endmembers, but with significantly reduced noise and spectral outliers. Our classification results were validated by evaluating detailed scale mapping of three known mine sites (Esse-Spoonamore, Wright-McCrady and Garbysch-Thane) with published ground truth information about the vegetation cover, extent of erosion and exposure of waste pile materials and/or geologic information about host lithology and mineralization. Despite successful demonstration of the utility of WV3 data for inventorying mine features, additional landscape features such as bare agricultural fields and oil and gas drill pads were also identified. The elimination of such features will require combining the spectral classification maps presented in this study with high-quality topographic data. Also, the spectral endmembers identified during the course of this study could be useful for larger-scale mapping efforts using additional well-calibrated WV3 images beyond the coverage of our initial study area.

@article{doi103390min13070839,
    author = "Hubbard, Bernard E. and Gallegos, Tanya J. and Stengel, Victoria",
    title = "Mapping Abandoned Uranium Mine Features Using Worldview-3 Imagery in Portions of Karnes, Atascosa and Live Oak Counties, Texas",
    year = "2023",
    journal = "Minerals",
    abstract = "Worldview-3 (WV3) 16-band multispectral data were used to map exposed bedrock and mine waste piles associated with legacy open-pit mining of sandstone-hosted roll-front uranium deposits along the South Texas Coastal Plain. We used the “spectral hourglass” approach to extract spectral endmembers representative of these features from the image. This approach first requires calibrating the imagery to reflectance, then masking for vegetation, followed by spatial and spectral data reduction using a principal component analysis-based procedure that reduces noise and identifies homogeneous targets which are “pure” enough to be considered spectral endmembers. In this case, we used a single WV3 image which covered an \textasciitilde 11.5 km by \textasciitilde 19.5 km area of Karnes, Atascosa and Live Oak Counties, underlain by mined rocks from the Jackson Group and Catahoula Formation. Up to 58 spectral endmembers were identified using a further multi-dimensional class segregation method and were used as inputs for spectral angle mapper (SAM) classification. SAM classification resulted in the identification of at least 117 mine- and mine waste-related features, most of which were previously unknown. Class similarity was further evaluated, and the dominant minerals in each class were identified by comparison to spectral libraries and measured samples of actual Jackson Group uranium host rocks. Redundant classes were eliminated, and SAM was run a second time using a reduced set of 23 endmembers, which were found to map these same features as effectively as using the full 58 set of endmembers, but with significantly reduced noise and spectral outliers. Our classification results were validated by evaluating detailed scale mapping of three known mine sites (Esse-Spoonamore, Wright-McCrady and Garbysch-Thane) with published ground truth information about the vegetation cover, extent of erosion and exposure of waste pile materials and/or geologic information about host lithology and mineralization. Despite successful demonstration of the utility of WV3 data for inventorying mine features, additional landscape features such as bare agricultural fields and oil and gas drill pads were also identified. The elimination of such features will require combining the spectral classification maps presented in this study with high-quality topographic data. Also, the spectral endmembers identified during the course of this study could be useful for larger-scale mapping efforts using additional well-calibrated WV3 images beyond the coverage of our initial study area.",
    url = "https://doi.org/10.3390/min13070839",
    doi = "10.3390/min13070839",
    openalex = "W4381742032",
    references = "dickinson1976geologic"
}