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- W2380964283 abstract "Transverse structures can be classified into two kinds in Yalongjiang water-transferring region, namely sheared transverse structure and tension transverse structure. Sheared transverse structure extends with sharp interface at little regional scale. The formation of sheared transverse structure is more related to the activity of NW-structures, and with multiphase tectonic activity. Its succeeding activity usually is inherited. The intersected place of sheared transverse structure and NW-structure is the important earthquake-pregnant tectonic site. Tension transverse structure consist of a group of units assembled by faults, folds, fissures, and related land form. It extends at large scope in form of typical diffusive. Tension transverse structure is the classic superimposed structure and formed in early Quaternary. The genesis of transverse structure in Yalongjiang water-transferring region was the result from the newly activation of buried basement fault, and the deformational intensity became weaken from the base to cover. There are benefit factors to water-transferring project, also harmful to it." @default.
- W2380964283 created "2016-06-24" @default.
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- W2380964283 date "1999-01-01" @default.
- W2380964283 modified "2023-09-24" @default.
- W2380964283 title "Geological features of transverse structuresin Yalongjang water-transferring region and its mechanics" @default.
- W2380964283 hasPublicationYear "1999" @default.
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