According to the existed geological data and the results of the discontinuty measurement by Borehole televiewer, Li-shan colluvial deposits may be formed by large-scale hillslope creep.

 
  • 根據過(guò)去地質(zhì)資料以及孔內造影之不連續面位態(tài)資料統計結果推論,梨山崩積地區可能為早期大規模山坡潛移破壞所造成。
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