简体版 繁體版 English
登録 ログイン

lateral variationの例文

例文モバイル版
  • The lateral variation in sediment within a stratum is known as sedimentary facies.
  • The Late Eocene reflects more frequent lateral variations of interbedded limestones, dolomites, marls, and shales.
  • This behaviour has been reproduced by modelling the viscoelastic response of the megathrust fault plane with lateral variations in both convergence rate and frictional properties.
  • This behavior has been reproduced by modeling the viscoelastic response of the megathrust fault plane with lateral variations in both convergence rate and frictional properties.