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- W2360727641 abstract "The paleo-earthquake parameters of Minjiang fault in Holocene provide the important data for seismic potential assessment.One large trench lies in front of terraceⅡ,in the estuary of Heisi gully,in Zhangla basin,along the Minjiang fault.Sedimentary sequences can be divided into two layers,with the light blue alluvial gravel strata in the lower and the light yellow to gray gravel layer of peat layer in the upper.Three paleo-earthquake events can be identified by the dislocation of the strata,and the vertical drop is about 1.5mthat accompany with each event,and simultaneous make the dip of the strata changed.According to the statistical regularity between the magnitude,the co-seismic displacement and the long rupture,the magnitude is concluded to be at 7.1.Based on the age of the 14 C in the lower A mark layer,we can conclude that the recurrence period is2 557-3 410a.Considering the current shape of fault scarp close to the buried shape of pre-earthquake,we should pay more attention to the seismic risk in this region after the Wenchuan earthquake." @default.
- W2360727641 created "2016-06-24" @default.
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- W2360727641 date "2013-01-01" @default.
- W2360727641 modified "2023-09-25" @default.
- W2360727641 title "Paleo-Earthquake Parameters of Minjiang Fault in Holocene" @default.
- W2360727641 hasPublicationYear "2013" @default.
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