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Use of carbonate morphology and clay content to determine paleosol genesis in the Plio-Pleistocene St. David Formation, southeastern Arizona

Conference · · Geological Society of America, Abstracts with Programs; (United States)
OSTI ID:5807844
;  [1]
  1. Univ. of New Mexico, Albuquerque, NM (United States). Dept. of Earth and Planetary Science
Paleosols in the Plio-Pleistocene St. David Formation, southeastern Arizona, were studied to determine the origin of carbonate layers and relation of clay translocation to paleoenvironment. Paleosols that formed above the influence of the ground water table (vadose) have carbonate and clay accumulations similar to those found in nongravelly Quaternary surface soils. Carbonate-enriched zones are beneath clay-rich, carbonate-depleted zones. Carbonate is disseminated in the matrix and is segregated into small ([le]1 cm) nodules, filaments, and seams. Layers of increased clay accumulation have a higher ratio of fine to coarse (or total) clay than overlying or underlying layers indicating that clay in these layers was probably translocated. Paleosols that formed within the influence of the ground water table (hydromorphic) have carbonate and clay accumulations unlike those found in modern, well-drained surface soils. Carbonate is segregated into large (2--10 cm) concretions in a noncalcareous or weakly calcareous matrix. Layers of increased clay accumulation seldom have a genetic relation to zones of increased carbonate. These layers lie above or below or correspond to the zones of carbonate concretions. Thus, carbonate morphology and clay content, in addition to spatial relationships of carbonate- and clay-enriched zones, may be used to infer paleo-ground water table.
OSTI ID:
5807844
Report Number(s):
CONF-921058--
Conference Information:
Journal Name: Geological Society of America, Abstracts with Programs; (United States) Journal Volume: 24:7
Country of Publication:
United States
Language:
English

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