Many paleosols formed by autocyclic processes, while not regionally correlative, may be significant with respect to groundwater flow (e.g., Weissmann and Fogg 1999 ) and contaminant fate and transport both from the perspective of their potential function as a hydraulic barrier and their potential utility to a stratigrapher as a chronostratigraphic surface or marker bed (Catuneanu 2006 ).
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The Geology of Aquitards in Alluvial Aquifers: A Predictive Approach Based on Facies Models.
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