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The Impact of a Shrinking Cryosphere on the Form of Arctic
Alluvial
Channels
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Lacustrine deltas in a Mesozoic
alluvial
sequence from Camp Hill, Antarctica
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Alluvial
stratigraphic sequences within the Permian Transantarctic foreland basin, Beardmore Glacier area, Antarctica
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Late Pleistocene and Holocene hydroclimate change in the Southeastern United Sta...
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Hyporheic Exchange and Water Chemistry of Two Arctic Tundra Streams of Contrasti...
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Influence of Morphology and Permafrost Dynamics on Hyporheic Exchange in Arctic...
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Estimating 3D Variation in Active-Layer Thickness Beneath Arctic Streams Using G...
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Mid-Jurassic age for the Botany Bay Group: implications for Weddell Sea Basin cr...
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Silicate inclusions in isoferroplatinum: Constraints on the origin of platinum m...
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Sedimentary Properties of the Middle−Upper Eocene Formations in Çardak, Burdur a...
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Inorganic geochemistry of El’gygytgyn Lake sediments (northeastern Russia) as an...
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Kansan Proglacial Environment, East-Central Nebraska
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Book review: Quaternary Geology and Geomorphology of South America by C. Clapper...
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Leg 188 Sythesis: Transitions in the Glacial History of the Prydz Bay Region, Ea...
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An Evaluation of Methods for Identifying and Interpreting Buried Soils in Late Q...
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Extending Airborne Electromagnetic Surveys for Regional Active Layer and Permafr...
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Fluvial Megafans on Earth and Mars
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Transcontinental retroarc sediment routing controlled by subduction geometry and...
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Remote Sensing of River Delta Inundation: Exploiting the Potential of Coarse Spa...
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Fluvial Megafans on Earth and Mars
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