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    Median Tectonic Line

    Strike-Slip Fault (Right-Lateral) · Japan

    The Median Tectonic Line is a strike-slip fault, where the two blocks slide horizontally past each other, right-lateral (the opposite block moves to the right). Its mapped traces are about 510 km long in Japan. It lies within the Amur Plate, which deforms under the push of neighbouring plates. Its slip rate is estimated between 0.9 and 5 mm per year depending on the section.

    Type
    Strike-Slip Fault
    Sense of Slip
    Right-Lateral
    Mapped Length
    ≈ 510 km
    Slip Rate
    0.9 – 5 mm per year
    Countries
    Japan
    Plates
    Amur Plate

    Sources: GEM Global Active Faults (Styron et Pagani, 2020), CC BY-SA 4.0, catalogue GEM Faulted Earth · NOAA NCEI · Bird (2003), PB2002 · Wikidata