Major intracontinental strike-slip faults and contrasts in lithospheric strength
نویسندگان
چکیده
منابع مشابه
Major intracontinental strike-slip faults and contrasts in lithospheric strength
A large fraction of major intracontinental strike-slip faults, defi ned here as those slipping at rates of ~10 mm/yr or more, lie adjacent to relatively strong regions, such as oceanic lithosphere or Precambrian shields. We suggest that such faults form adjacent to discontinuities in strength, because strain in a continuous medium must concentrate near such strong objects. Concentration in stra...
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ژورنال
عنوان ژورنال: Geosphere
سال: 2010
ISSN: 1553-040X
DOI: 10.1130/ges00519.1