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Facies, Backwater Limits, and Paleohydraulic Analysis of Rivers in a Forced-regressive, Compound Incised Valley, Cretaceous Ferron Sandstone, Utah, U.s.a.

Stephanie Kimmerle; Janok P. Bhattacharya
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Authigenic Mineralization in Low-rank Coals from the Velenje Basin, Slovenia

TjaŠa KanduČ; Polona VreČa; Špela Gregorin; Mirijam Vrabec; Marko Vrabec; Fausto Grassa
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Re-evaluating the Paleogeography of the River-dominated and Wave-influenced Ferron Notom Delta, Southern Central Utah: an Integration of Detailed Facies-architecture and Paleocurrent Anal...

Yangyang Li; Janok P. Bhattacharya; Sumiyyah Ahmed; Daniel Garza
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Methods For Restoring and Describing Ancient Clinoform Surfaces

Tore Grane Klausen; William Helland-Hansen
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Facies Distribution in Sediment-gravity-flow Deposits Constructing Sediment Waves: an Outcrop Example of Forearc Basin Fills, Neogene Aoshima Formation, Southwest Japan

Yuri Onishi; Kiwako Takii-Kawakami; Hiroko Abe; Yoshiro Ishihara
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Quantifying Roundness of Detrital Minerals By Image Analysis: Sediment Transport, Shape Effects, and Provenance Implications

Alberto Resentini; Sergio AndÒ; Eduardo Garzanti
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Spatial Variations in the Chemical Composition of Eolian Sediments in Hyperarid Regions: a Case Study from the Badain Jaran Desert, Northwestern China

Qiujie Chen; Zhuolun Li; Shipei Dong; Nai'ang Wang; Derrick Y.F. Lai; Kai Ning
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Sediment Accumulation Rates For the Mississippi Delta Region: a Time-interval Synthesis

Chris Jenkins
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    COVER EXPLANATION.—The Badain Jaran Desert, the second largest desert in China, serves as an ideal site for studying the spatial variability of the chemical composition of eolian sediments, as well as controls on hyperarid regions. See Li et al., this issue.

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