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Geochemical Insights Into Provenance of the Middle Devonian Hamilton Group of the Central Appalachian Basin, U.S.A.

Brittany N. Hupp; Amy L. Weislogel
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Topographic Controls On the Development of Contemporaneous but Contrasting Basin-Floor Depositional Architectures

Daniel Bell; Christopher J. Stevenson; Ian A. Kane; David M. Hodgson; Miquel Poyatos-Moré
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River Morphodynamic Evolution Under Dam-Induced Backwater: An Example from the Po River (Italy)

Vittorio Maselli; Claudio Pellegrini; Fabrizio Del Bianco; Alessandra Mercorella; Michael Nones; Luca Crose; Massimo Guerrero; Jeffrey A. Nittrouer
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Detrital Clay Coats, Clay Minerals, and Pyrite: A Modern Shallow-Core Analogue For Ancient and Deeply Buried Estuarine Sandstones

Joshua Griffiths; Richard H. Worden; Luke J. Wooldridge; James E. P. Utley; Robert A. Duller
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A Source-to-Sink Compositional Model of a Present Highstand: An Example in the Low-Rank Tiber Depositional Sequence (Latium Tyrrhenian Margin, Italy)

Daniel Tentori; Salvatore Milli; Kathleen M. Marsaglia
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    COVER EXPLANATION.—Submarine-lobe deposits of the Upper Broto System located at the Cascada de Sorrosal, Broto, Spain. Alternating sandstone- and mudstone-rich packages are interpreted to represent compensational stacking of lobes. Deformation in the developing foreland basin resulted in thrusting and folding of the buried deposits prior to exhumation and excavation by the modern river. See Bell et al., this issue.

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