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      Basin formation at a contractional bend of a large transcurrent fault: Plio-Pleistocene subsidence of the Kobe and northern Osaka Basins, Japan

      , , , ,
      Tectonophysics
      Elsevier BV

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          Journal
          Tectonophysics
          Tectonophysics
          Elsevier BV
          00401951
          June 2000
          June 2000
          : 321
          : 3
          : 327-341
          Article
          10.1016/S0040-1951(00)00072-X
          6b4011fd-531d-4300-949c-44cc7796fb84
          © 2000

          https://www.elsevier.com/tdm/userlicense/1.0/

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