Composite Particles in Mudstones: Examples from the Late Cretaceous Tununk Shale Member of the Mancos Shale Formation
Impact of Stylolitization On Fluid Flow and Diagenesis in Foreland Basins: Evidence from an Upper Jurassic Carbonate Gas Reservoir, Abu Dhabi, United Arab Emirates
Meteoric Water and Salt-Dome-Related Diagenesis in Tertiary Turbidite Reservoirs from the EspÍrito Santo Basin, Brazil
COVER EXPLANATION.—Cliff-forming Grassy Member, Desert Member, and Lower Castlegate Sandstone, Coal Canyon, Book Cliffs, eastern Utah. The lower sandstone bench is dominated by Grassy parasequence G2, which is cut by a shoreface-incised channel a few kilometers west, at Tusher Canyon. Marine mudstones of Desert parasequences D1 to D3 separate the lower and middle benches. The middle sandstone bench is Desert parasequences D4 to D5, with D5 cut out by a shoreface-incised channel to the right (west). Coal-bearing coastal-plain mudstones overlie the D5 sandstones, separating the middle and upper benches. The uppermost sandstone bench is comprised of the amalgamated fluvial sandstones of the Lower Castlegate Sandstone. Cliff section approximately 150 m high. Photo looks south. See Pattison, this issue.