It is feasible to infer the specific shape of a fault scarp with the help of its average diffusion age and origin time of the scarp.

 
  • 無(wú)論是單一型斷層崖還是復合型斷層崖,通過(guò)斷層崖的平均擴散年齡和初始錯斷時(shí)間,就能推斷出它在某一時(shí)刻的具體形態(tài)。
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