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Textual heterogeneity in massive sandstones from the Grès d'Annot and Numidian Flysch: Implications for depositional processes

Urval S. Patel; Dorrik A.V. Stow; Andy Gardiner; Jim Buckman
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Occurrence and origin of glauconite in the Cambro-Ordovician Bliss Formation of southern New Mexico and West Texas (U.S.A.)

Karl Krainer; Peter Tropper; Kurt Krenn; Spencer G. Lucas
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Analysis of common pre-treatments in grain-size analysis (using a grain-size standard)

Adam J. White; Stephanie S. Kienast; Markus Kienast; Jessica C. Garwood; Paul S. Hill
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Influence of channelized-flow density structure on the stratal architecture of deep-marine levee deposits

Anika L. Bergen; Celeste M. Cunningham; Viktor Terlaky; R. William C. Arnott
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    COVER EXPLANATION.—Clast-supported conglomerate. Most clasts are from Triassic dolostones and, in lesser amounts, quartzites. Red clasts derive from continental deposits, probably overlying the basement before the late Miocene transgression. Coin diameter: 22 mm. See Sola et al. March 2022 issue.

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