Holocene paleoeseismology of the Fodongmiao-Hongyazi Fault along the Northern Tibetan margin (Western China) and implication to intraplate earthquake rupturing pattern
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DOI: 10.1016/j.tecto.2021.228812
Abstract: Abstract The margins of the Tibetan Plateau are the most recent evolving part of the orogen, where distributed fault systems accumulate intraplate crustal deformation induced by the Indo-Asian collision, and many great earthquakes occur. Understanding… read more here.
Keywords: earthquake; tibetan margin; along northern; northern tibetan ... See more keywords