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Lack of synsedimentary chemical alteration in polar carbonates (Ross Sea, Antarctica): Resolution of a conundrum

Tracy D. Frank; Noel P. James; Aaron I. Shultis
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Submarine-fan development revealed by integrated high-resolution datasets from La Jolla Fan, offshore California, U.S.A.

Katherine L. Maier; Charles K. Paull; David W. Caress; Krystle Anderson; Nora M. Nieminski; Eve Lundsten; Benjamin E. Erwin; Roberto Gwiazda; Andrea Fildani
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The origin and significance of convolute lamination and pseudonodules in an ancient deep-marine turbidite system: From deposition to diagenesis

Omar N. Al-Mufti; R. William C. Arnott
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Provenance of lower Cambrian quartz arenite on southwestern Baltica: Weathering versus recycling

Sanne Lorentzen; Tonje Braut; Carita Augustsson; Johan P. Nystuen; Jens Jahren; Niels H. Schovsbo
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Guidelines for assessing the provenance of Mesozoic and Cenozoic clastic successions sourced by pre-Jurassic basement complexes in southernmost North America

Michelangelo Martini; Luigi Solari; Mariana Peña-Guerrero; Mildred Zepeda-MartÍnez; Chiara Montomoli
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Facies heterogeneity and source potential of carbonate-mudstone-dominated distal ramp deposits, Agrio Formation, Neuquén Basin, Argentina

Shawn A. Moore; Lauren P. Birgenheier; Matthias D. Greb; Daniel Minisini; Maísa Tunik; Julieta Omarini
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  • Cover Image

    Cover Image

    issue cover

    COVER EXPLANATION.—A highly diachronous stratigraphic surface separating coarse-grained sandstone (right) and thin-bedded turbidites (left) within the fill of a slope channel element, Campanian Tres Pasos Formation, Magallanes Basin, Chilean Patagonia (see Hubbard et al. in an upcoming issue).

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