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  1. Miocene reversal of bottom water flow along the Pacific margin of the Antarctic Peninsula: stratigraphic evidence from a contourite sedimentary tail

    A Fossil Mounded Sedimentary Body (MB) has been identified in the sedimentary record on the central continental rise west of Adelaide Island, on the Antarctic Peninsula Pacific margin. The growth […]

    Read more of: Miocene reversal of bottom water flow along the Pacific margin of the Antarctic Peninsula: stratigraphic evidence from a contourite sedimentary tail
  2. The source of granitic gneisses and migmatites in the Antarctic Peninsula: a combined U-Pb SHRIMP and laser ablation Hf isotope study of complex zircons

    Zircons gneisses and migmatites collected from the Antarctic Peninsula have different core–rim hafnium isotope ratio relationships depending on whether evidence for zircon dissolution is present or absent. Two samples contain […]

    Read more of: The source of granitic gneisses and migmatites in the Antarctic Peninsula: a combined U-Pb SHRIMP and laser ablation Hf isotope study of complex zircons