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: Characterization of the structure of faults in the Eocene Carrizo Formation near Gause, Milam County, Texas
  name:
    name part: Yilmaz, Ramazan
    name part: 1970-
    role:
      role term: creator
  type of resource: text
  genre: bibliography
  origin info:
    place:
      place term: xx
    date issued: 1997
    issuance: monographic
  language:
    language term: eng
  physical description:
    form: print
    form: remote
    extent: xi, 97 leaves : illustrations, maps ; 28 cm.
  abstract: and localized in a narrow zone. Neighboring fault segments
  abstract: antithetic small faults also occurs near these geometric
  abstract: appears to be more common where the adjacent fault segment
  abstract: as well as the magnitude of overlap. With increasing
  abstract: comprise a small-scale graben accommodating NW-SE extension.
  abstract: consists of multiple fault segments arranged as "en echelon"
  abstract: curving to abut the other or the two segments are linked in
  abstract: displacement, fault structure becomes more complex. A fault
  abstract: earlier formed segments. As in the earlier stage, systems of
  abstract: exhibits a nonplanar local geometry. Enhanced development of
  abstract: faulting was between 100 and 900 m.
  abstract: faults. Wall rock deformation adjacent a fault occurs but is
  abstract: for this difference is unresolved. Cataclasis within the
  abstract: form between and abut the earlier formed larger fault
  abstract: Gause, Milam County, Texas. The faults strike NE-SW and
  abstract: in direct association with the larger faults except for a
  abstract: interbedded siltstones and shales. Five faults and fault
  abstract: irregularities. Clay smears develop along fault segments
  abstract: larger faults. In the initial stages of development, a fault
  abstract: limited grain breakage together with rigid body grain
  abstract: lithified quartz sandstones with several horizons with
  abstract: m to between 6-15 m. Smaller displacement faults occur only
  abstract: observed and are related to sense of fault stepover and shear
  abstract: of a limited nature. Locally, drag folding occurs, but this
  abstract: quarry in the Eocene Carrizo Formation near the town of
  abstract: rotation. The limited grain breakage together with other
  abstract: sandstone and clay in another subunit (unit B). The cause
  abstract: secondary faults form in the overlap regions of larger
  abstract: sedimentological data suggest the depth of burial during
  abstract: segments. Three different systems of secondary faults are
  abstract: series of excellently exposed, normal faults in a small
  abstract: shear zones of faults in the sandstone consists of some
  abstract: smears do not develop along faults that offset interbedded
  abstract: system of small faults that forms locally between two of the
  abstract: The Carrizo Fm. consists primarily of friable to weakly
  abstract: the overlapping region by a system of secondary faults that
  abstract: the subunits (unit A) of the Carrizo. In contrast, clay
  abstract: This study characterizes the structure and evolution of a
  abstract: usually overlap and link either directly by one segment
  abstract: where they offset interbedded sandstone and clay of one of
  abstract: zone evolves as more fault segments develop in proximity to
  abstract: zones occur in the quarry with displacements ranging from 0.3
  note: by Ramazan Yilmaz.
  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 1997.
  note: Includes bibliographical references.
  subject:
    topic: Major geology
  identifier: https://hdl.handle.net/1969.1/ETD-TAMU-1997-THESIS-Y35
  related item:
    location:
      url: https://hdl.handle.net/1969.1/ETD-TAMU-1997-THESIS-Y35
  record info:
    record content source: TXA
    record creation date: 980203
    record change date: 20220103134756.0
    record identifier: in00001397216