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- W2014154415 abstract "This study focuses on the geometry andkinematics of the Sinnyeong Fault which is the most conspicuous fault among theWNW-trending Gaeum Fault System in the Gyeongsang Basin,SE Korea.The fault is traced for over ca.70 kmand has a consistent WNW-trending strike with a nearly vertical dip. It has anasymmetric fault damage zone of several meters to several tens of meters inwidth and a several meter-thickfault core. Its main movement is interpreted as sinistral-reverse oblique-slipor sinistral strike-slip under NE-SW compressional stress regime, although it couldhave experienced other faultings with different senses before/after this movement. Cylindricalfolds, having the NW-trending fold axes of low angle plunge, are only observed along the southern damagezone of the fault with a continuous narrow width of several tens of meters. Itis thus interpreted that the formation of the folds and sinistral movement ofthe fault were almost contemporaneously generated due to the concentration ofthe regional NE-SW compressionalstress along pre-existing WNW-trending faults or densely populated fracturezone in a relatively stableintraplate region." @default.
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- W2014154415 date "2013-01-01" @default.
- W2014154415 modified "2023-10-16" @default.
- W2014154415 title "Intraplate Strike-Slip Reactivation of the Sinnyeong Fault in the Cretaceous Gyeongsang Basin, Korea, Due to the Concentration of Later Compressional Stress" @default.
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- W2014154415 doi "https://doi.org/10.4236/gep.2013.13003" @default.
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