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National Geologic Map Database
Geologic Unit: Werner
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Map showing publication footprint
  • Usage in publication:
    • Werner Formation
  • Modifications:
    • Overview
  • Dominant lithology:
    • Anhydrite
    • Shale
    • Sandstone
    • Conglomerate
  • AAPG geologic province:
    • Mid-Gulf Coast basin
Publication:

Mancini, E.A., Tew, B.H., and Mink, R.M., 1990, Jurassic sequence stratigraphy in the Mississippi Interior salt basin of Alabama: Gulf Coast Association of Geological Societies Transactions, v. 40, p. 521-530.


Summary:

Werner Formation consists predominantly of anhydrite, but includes shale, sandstone, and conglomerate in the lower portion of the formation. Maximum thickness in report area exceeds 500 ft. Disconformably overlies the Late Triassic to Early Jurassic Eagle Mills Formation or basement rocks. Represents initial transgression of marine waters into the Gulf of Mexico basin. Callovian age assigned by Salvador (1987) based on regional stratigraphic and paleogeographic relationships.

Source: GNU records (USGS DDS-6; Reston GNULEX).


Map showing publication footprint
  • Usage in publication:
    • Werner Anhydrite
  • Modifications:
    • Redescribed
  • AAPG geologic province:
    • Mid-Gulf Coast basin
Publication:

Wade, W.J., and Moore, C.H., 1993, Jurassic sequence stratigraphy of southwest Alabama: Gulf Coast Association of Geological Societies Transactions, v. 43, p. 431-443.


Summary:

Unit referred to in this report as Werner Anhydrite. Though according to the original definition of the Werner, unit consists of an upper massive anhydrite member and a lower conglomeratic redbed member, the lower redbeds cannot be distinguished from the underlying Eagle Mills redbeds on well logs. Consequently, the term Werner Formation often refers only to the anhydrite member. Interpreted as a marginal facies of the Louann Salt.

Source: GNU records (USGS DDS-6; Reston GNULEX).


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