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Grain size, composition, porosity and permeability contrasts within cross‐bedded sandstones in Tertiary fluvial deposits, central Spain
Author(s) -
HARTKAMP CHRISTEL A.,
ARRIBAS JOSÉ,
TORTOSA AMPARO
Publication year - 1993
Publication title -
sedimentology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.494
H-Index - 108
eISSN - 1365-3091
pISSN - 0037-0746
DOI - 10.1111/j.1365-3091.1993.tb01360.x
Subject(s) - geology , grain size , diagenesis , clastic rock , compaction , cementation (geology) , mineralogy , quartz , porosity , permeability (electromagnetism) , carbonate , outcrop , permeameter , granulometry , sedimentary rock , geochemistry , geomorphology , soil science , geotechnical engineering , composite material , materials science , chemistry , cement , hydraulic conductivity , sediment , soil water , metallurgy , paleontology , biochemistry , membrane
Permeability measured with a portable probe permeameter on outcrops of cross‐bedded sandstones ranges between 0·9 and 19 D. The highest permeability (2–19 D with an average of 8·5 D) occurs in the coarsest grained foreset laminae (CFL), intermediate values (2–12 D with an average of 5·3 D) occur in finer grained foreset laminae (FFL) and the lowest values (0·9–10 D with an average of 4·8 D) occur in bottomset layers (BL). In the cross‐beds the average grain size ranges from medium grained sand in the CFL to fine grained sand in the FFL and BL. In all three subfacies, the average size of the primary pores is approximately 1φ unit smaller than the average grain size. The abundance of unstable carbonate clasts correlates with increasing average grain size, micritic clasts being most abundant in the CFL. Conversely, quartz content increases with decreasing grain size and is highest in the FFL and BL. Diagenetic destruction of primary porosity by compaction and cementation, as well as generation of secondary porosity through dissolution, were controlled by the original mineralogical composition of the sand. Contrasts in grain size determine the primary pore size contrasts and differences in composition between CFL, FFL and BL. Permeability contrasts reflect variations in average primary pore size rather than differences in total porosity. Probe permeability contrasts between CFL, FFL and BL depend on contrasts in average pore size and contrasts in mineralogical composition between the subfacies.