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pro vyhledávání: '"Hong-wai Conrad (鄧康偉) Tang"'
Publikováno v:
Journal of Geophysical Research: Solid Earth. 108
[1] In north China, most earthquakes occur at depths of 10–25 km and are considered to be the direct result of deformation or rupture of the brittle upper crustal layer. To describe this mechanism, a planar horizontal negative dislocation plane is
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2d944fd204fca191c5f4161150b1a65c
https://doi.org/10.1029/2002jb002171
https://doi.org/10.1029/2002jb002171
