rdf-syntax-grammar
mods:
  schema location: http://www.loc.gov/mods/v3 http://www.loc.gov/standards/mods/v3/mods-3-2.xsd
  title info:
    title: Depositional facies and environments of the lower Mineral Wells formation, Pennsylvanian Strawn group, north central Texas
  name:
    name part: Bradshaw, Susan Elizabeth.
    role:
      role term: creator
  type of resource: text
  genre: bibliography
  origin info:
    place:
      place term: xx
    date issued: 1996
    issuance: monographic
  language:
    language term: eng
  physical description:
    form: print
    form: remote
    extent: viii, 81 leaves : illustrations ; 28 cm.
  abstract: abundant plant fragments, red mudstones containing iron
  abstract: and consists of massive mudstones, massive silty mudstones
  abstract: concretions, and dark gray mudstones containing plant
  abstract: conglomerates, rippled very fine- to fine-grained sandstones
  abstract: conglomerates. Lastly, the aggrading channel facies consists
  abstract: conglomerates. The stratigraphy of the lower Mineral Wells
  abstract: consist of vertical successions from open marine to prodelta
  abstract: consists of trough and tabular cross-laminated sandstones,
  abstract: deposited in fluvial, deltaic, interdeltaic, and inner shelf
  abstract: depositional environments, and stratigraphy. Eight
  abstract: depositional facies were identified in the lower Mineral
  abstract: deposits overlain by increasingly deeper marine facies.
  abstract: environments during late Desmoinesian and early Missourian
  abstract: formation is characterized by alternating progradational and
  abstract: fossiliferous and consists of gray, beige, green, and brown
  abstract: fragments and mudcracks. The distributary channel facies
  abstract: grained sandstones, very thinly-bedded very fine-grained
  abstract: group is a siliciclastic-dominated sequence of cyclically
  abstract: highly bioturbated sandy mudstones and muddy sandstones, and
  abstract: horizontal planar- and cross-laminated fine-to medium-grained
  abstract: interbedded mudstones, sandstones. and carbonates that was
  abstract: interdistributary bay facies consists of massive clayey
  abstract: interlayered with muddy sandstones and sandy mudstones, and
  abstract: laminated fine-grained sandstones, highly bioturbated fine-
  abstract: lenticular-laminated muddy siltstones. The transgressive
  abstract: limestones. The prodelta facies is largely nonfossiliferous
  abstract: medium-grained quartz sandstones and cherty pebble
  abstract: mudstones and sandstones. The meanderbeft facies consists of
  abstract: mudstones with some rippled very fine-grained sandstones,
  abstract: mudstones, black mudstones with phosphate nodules, and
  abstract: of large scale trough cross-bedded, wavy-bedded, and rippled
  abstract: Pinto and Parker counties in north-central Texas for the
  abstract: purpose of describing and interpreting its facies,
  abstract: sandstones interlayered with cross-bedded and massive
  abstract: sandstones, and sandy and silty mudstones. The
  abstract: shoreface facies consists of cross-laminated and ripple
  abstract: stratified very fine- to medium-grained sandstones. The
  abstract: structures, and fossil content. The open marine facies is
  abstract: swampmarsh facies consists of gray platy mudstones containing
  abstract: The lower Mineral Wells formation of the Pennsylvanian Strawn
  abstract: time. This study examined outcrops of the formation in Palo
  abstract: to distributary channel or interdistributary bay.
  abstract: Transgressive sequences consist of transgressive shoreface
  abstract: transgressive sequences. Progradational sequences typically
  abstract: trough cross-bedded fine-grained sandstones, massive
  abstract: wavy-bedded sandstones, and wavy-laminated and lenticular
  abstract: Wells formation on the basis of lithology. sedimentary
  abstract: with occasional siltstone lenses, and horizontal planar- and
  note: by Susan Elizabeth Bradshaw.
  note: "Major subject: Geology".
  note: Vita.
  note: Also available online.
  note: Issued also on microfiche from Lange Micrographics.
  note: M.S. Texas A&M University 1996.
  note: Includes bibliographical references.
  subject:
    topic: Major geology
  identifier: https://hdl.handle.net/1969.1/ETD-TAMU-1996-THESIS-B737
  related item:
    location:
      url: https://hdl.handle.net/1969.1/ETD-TAMU-1996-THESIS-B737
  record info:
    record content source: TXA
    record creation date: 970404
    record change date: 20220103134331.0
    record identifier: in00001333415