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Paleocene (65–63 and 58.5 ma) marine flooding and 62–60 ma sediment bypass in southern Wyoming, U.S.A.: Implications for Laramide sediment flux to the Gulf of Mexico

Anton F.-J. Wroblewski; Ronald J. Steel
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The glass ramp of Wrangellia: Late Triassic to Early Jurassic outer ramp environments of the McCarthy Formation, Alaska, U.S.A.

Yorick P. Veenma; Kayla McCabe; Andrew H. Caruthers; Martin Aberhan; Martyn Golding; Selva M. Marroquín; Jeremy D. Owens; Theodore R. Them, II; Benjamin C. Gill; João P. Trabucho Alexandre
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Demarcation of Early Pennsylvanian paleovalleys in depozones of the Appalachian foreland-basin system based on detrital-zircon U-Pb and Hf analysis

Isaac Allred; Mike Blum
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Stratigraphic analysis of XES02: Implications for the sequence stratigraphic paradigm

Bradford E. Prather; Oriol Falivene; Peter M. Burgess
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Facies architecture and paleogeography evolution of regressive wave-dominated shorelines transitioning into tide-dominated estuaries: Early Devonian Subbat Member, Jauf Formation, Saudi A...

Hasan Algheryafi; César Viseras; Camilo Polo; Khalid Al-Ramadan
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How do grain coats prevent formation of quartz overgrowths?

Olav Walderhaug; Kristin W. Porten
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  • Cover Image

    Cover Image

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    COVER EXPLANATION.—An incised valley complex filled with fluvial and tidally influenced bars and bedforms marks the base of the Paleocene Hanna Formation in the Carbon Basin, Wyoming, U.S.A. Paleobotanist for scale in the foreground. See Wroblewski et al. this issue.

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