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Lake Waco Formation

The Lake Waco Formation is a geologic formation within the Eagle Ford Group deposited during the Middle Cenomanian to the Early Turonian of the Late Cretaceous in central Texas.[1] The formation was named for outcrops near Lake Waco, south of the city of Waco, Texas by W. S. Adkins and F. E. Lozo in 1951.[2] The Lake Waco Formation is primarily composed of shale, with minor amounts of limestone and volcanic ash beds (bentonites). It is subdivided into three members: Bluebonnet Member, Cloice Member, and the Bouldin Member.[2] The Bluebonnet Member is 10 to 20 ft (3 to 6 m) thick, and is made up of broken pieces (prisms) of inoceramid clams and planktonic foraminifera.[3] The Cloice Member is 35 ft (11 m) thick at its type section on the Cloice Branch of the South Bosque River, whereas the Bouldin Member was named for outcrops on Bouldin Creek south of downtown Austin, where it is roughly 9 ft (3 m) thick. They are both made up of shales rich in organic matter with thin limestones and volcanic ash beds.[2]

Lake Waco Formation
Stratigraphic range: Mid Cenomanian-Early Turonian
~96–93.5 Ma
[1]
TypeGeological formation
Unit ofEagle Ford Group
Sub-unitsBluebonnet Member, Cloice Member, Bouldin Member
UnderliesSouth Bosque Formation
OverliesPepper Shale
Lithology
PrimaryShale
OtherMarl, limestone, volcanic ash beds
Location
RegionEast Texas
Country United States
Type section
Named forLake Waco near Waco, Texas[2]
Named byAdkins and Lozo[2]

Plesiosaur remains, shark's teeth, ammonites, and inoceramid clams are among the fossils that have been recovered from its strata.[3][4]


See also edit

References edit

  1. ^ a b Denne, R. A., Breyer, J. A., Callender, A. D., Hinote, R. E., Kariminia, M., Kosanke, T. H., Kita, Z., Lees, J. A., Rowe, H., Spaw, J. M., and Tur, N. (2016). Biostratigraphic and geochemical constraints on the stratigraphy and depositional environments of the Eagle Ford and Woodbine Groups of Texas: in Breyer, J. A. (ed.), The Eagle Ford Shale: A renaissance in U.S. oil production, AAPG Memoir 110, p. 1-86.
  2. ^ a b c d e Adkins, W. S., and F. E. Lozo, 1951, Stratigraphy of the Woodbine and Eagle Ford, Waco area, Texas, in F. E. Lozo, ed., The Woodbine and adjacent strata of the Waco area of central Texas, a symposium for the 1951 field trip sponsored by the East Texas Geological Society: Southern Methodist University Press, Fondren Science Series 2, Dallas, Texas, p. 101–163.
  3. ^ a b Silver, B. A. (1963) The Bluebonnet Member, Lake Waco Formation (Upper Cretaceous), Central Texas-A lagoonal deposit: Baylor Geologic Studies Bulletin 4, Waco, Texas, 46 p.
  4. ^ Thurmond, John T. (1968). "A New Polycotylid Plesiosaur from the Lake Waco Formation (Cenomanian) of Texas". Journal of Paleontology. 42 (5). jstor.org: 1289–1296. JSTOR 1302265.

lake, waco, formation, geologic, formation, within, eagle, ford, group, deposited, during, middle, cenomanian, early, turonian, late, cretaceous, central, texas, formation, named, outcrops, near, lake, waco, south, city, waco, texas, adkins, lozo, 1951, primar. The Lake Waco Formation is a geologic formation within the Eagle Ford Group deposited during the Middle Cenomanian to the Early Turonian of the Late Cretaceous in central Texas 1 The formation was named for outcrops near Lake Waco south of the city of Waco Texas by W S Adkins and F E Lozo in 1951 2 The Lake Waco Formation is primarily composed of shale with minor amounts of limestone and volcanic ash beds bentonites It is subdivided into three members Bluebonnet Member Cloice Member and the Bouldin Member 2 The Bluebonnet Member is 10 to 20 ft 3 to 6 m thick and is made up of broken pieces prisms of inoceramid clams and planktonic foraminifera 3 The Cloice Member is 35 ft 11 m thick at its type section on the Cloice Branch of the South Bosque River whereas the Bouldin Member was named for outcrops on Bouldin Creek south of downtown Austin where it is roughly 9 ft 3 m thick They are both made up of shales rich in organic matter with thin limestones and volcanic ash beds 2 Lake Waco FormationStratigraphic range Mid Cenomanian Early Turonian 96 93 5 Ma PreꞒ Ꞓ O S D C P T J K Pg N 1 TypeGeological formationUnit ofEagle Ford GroupSub unitsBluebonnet Member Cloice Member Bouldin MemberUnderliesSouth Bosque FormationOverliesPepper ShaleLithologyPrimaryShaleOtherMarl limestone volcanic ash bedsLocationRegionEast TexasCountry United StatesType sectionNamed forLake Waco near Waco Texas 2 Named byAdkins and Lozo 2 Plesiosaur remains shark s teeth ammonites and inoceramid clams are among the fossils that have been recovered from its strata 3 4 See also editPlesiosaur stratigraphic distributionReferences edit a b Denne R A Breyer J A Callender A D Hinote R E Kariminia M Kosanke T H Kita Z Lees J A Rowe H Spaw J M and Tur N 2016 Biostratigraphic and geochemical constraints on the stratigraphy and depositional environments of the Eagle Ford and Woodbine Groups of Texas in Breyer J A ed The Eagle Ford Shale A renaissance in U S oil production AAPG Memoir 110 p 1 86 a b c d e Adkins W S and F E Lozo 1951 Stratigraphy of the Woodbine and Eagle Ford Waco area Texas in F E Lozo ed The Woodbine and adjacent strata of the Waco area of central Texas a symposium for the 1951 field trip sponsored by the East Texas Geological Society Southern Methodist University Press Fondren Science Series 2 Dallas Texas p 101 163 a b Silver B A 1963 The Bluebonnet Member Lake Waco Formation Upper Cretaceous Central Texas A lagoonal deposit Baylor Geologic Studies Bulletin 4 Waco Texas 46 p Thurmond John T 1968 A New Polycotylid Plesiosaur from the Lake Waco Formation Cenomanian of Texas Journal of Paleontology 42 5 jstor org 1289 1296 JSTOR 1302265 Retrieved from https en wikipedia org w index php title Lake Waco Formation amp oldid 1070843242, wikipedia, wiki, book, books, library,

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