Studies of Sedimentary Facies, Stratigraphy, and Deformation Structures of the Chelungpu Fault Zone on Cores from Drilled Wells in Fengyuan and Nantou, Central Taiwan


Stratigraphy, sedimentary facies, and deformation characteristics of drill cores from Fengyuan and Noutou wells reveal impartant attributes for the westmost portion of active Chelungup thrust fault and contrasting deformation mechanisms between the north and south ends.

Read 879 times