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Showing 1–4 of 4 results
Advanced filters: Author: Michael E. Oskin Clear advanced filters

  • The high eastern Tibetan Plateau was thought to have formed from an inflow of material from the lower crust. The cooling histories of rocks exposed at the plateau margin, however, reveal protracted, episodic growth, suggesting that faulting also played a role.

    • Michael E. Oskin
    News & Views
    Nature Geoscience
    Volume: 5, P: 597-598

  • Fisher et al. combine sediment geochemistry and climate modelling to reveal long-term synchrony between erosion rates and orbitally-driven climate oscillations in the tectonically-active southern Central Andes.

    • G. Burch Fisher
    • Lisa V. Luna
    • Lucas J. Lourens
    ResearchOpen Access
    Nature Communications
    Volume: 14, P: 1-15

  • Fracture density decays continuously with distance from the fault resulting in regionally widespread damage over multiple earthquake cycles, according to combined maps of fracture, strain and aftershocks from the 2019 Ridgecrest earthquakes.

    • Alba M. Rodriguez Padilla
    • Michael E. Oskin
    • Andreas Plesch
    Research
    Nature Geoscience
    Volume: 15, P: 222-226