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Title: Patterns of permeability in eolian deposits

Journal Article · · SPE (Society of Petroleum Engineers) Format. Eval.; (United States)
OSTI ID:6483934

The eolian, Jurassic Page sandstone of northeastern Arizona is marked by a highly ordered heterogeneity. The heterogeneity is expressed by the intricate association of stratification types, which are a direct result of the depositional processes. The dominant stratification types in eolian reservoirs are grainflow, grainfall, and wind-ripple deposits, which form on the lee faces of migrating dunes; interdune deposits, which form between migrating dunes; and extra-erg deposits, which occur sporadically when other depositional environments encroach upon an eolian system. These stratification types each have a unique permeability range, which implies that the fluid migration routes in eolian reservoirs will be dictated by the geometry and types of stratification present. One of the most important aspects of this study is the correlation of qualitative geologic descriptions with quantitative variables such as permeability. About 2,000 measurements were made with a field minipermeameter on an outcrop of the Page sandstone. These data show that three distinct permeability modes directly relate to the different stratification types.

Research Organization:
Univ. of Texas (US)
OSTI ID:
6483934
Journal Information:
SPE (Society of Petroleum Engineers) Format. Eval.; (United States), Vol. 3:2
Country of Publication:
United States
Language:
English