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Showing 1–5 of 5 results
Advanced filters: Author: Karin Sigloch Clear advanced filters

  • Indo-African mantle upwellings are arranged in a tree-like structure, which might reflect linear staggered detachment of proto-plumes from the lowermost mantle, according to seismic tomographic imaging.

    • Maria Tsekhmistrenko
    • Karin Sigloch
    • Guilhem Barruol
    Research
    Nature Geoscience
    Volume: 14, P: 612-619

  • A new explanation for the origin of the accreted terranes that form the mountainous Cordillera of western North America is proposed and tested: stationary, intra-oceanic subduction deposited massive slab walls in the mantle and grew volcanic archipelagos at the surface, which were overridden by and accreted to North America during Cretaceous times.

    • Karin Sigloch
    • Mitchell G. Mihalynuk
    Research
    Nature
    Volume: 496, P: 50-56

  • The ancient Farallon plate subducted under North America in two distinct stages. High-resolution tomographic images show large pieces of the plate, including the currently active piece, which descends from the Pacific Northwest coast to 1,500 km depth, and its stalled predecessor, which now occupies the transition zone and lower mantle beneath the eastern half of the continent.

    • Karin Sigloch
    • Nadine McQuarrie
    • Guust Nolet
    Research
    Nature Geoscience
    Volume: 1, P: 458-462

  • The heat driving Yellowstone’s volcanism originates from a depth of at least 700 km, according to images of the mantle created using novel seismic methods.

    • Karin Sigloch
    News & Views
    Nature Geoscience
    Volume: 11, P: 385-387

  • The advent of advanced plate tectonic reconstruction software has instigated an explosive growth in their generation and use by the wider Earth science community. This Technical Review provides a best-practice guide for quantitative plate reconstructions and their applications.

    • Maria Seton
    • Simon E. Williams
    • Karin Sigloch
    Reviews
    Nature Reviews Earth & Environment
    Volume: 4, P: 185-204