提出了一种构建含断层地质体三维模型的新方法。
A new method to model 3d geological bodies including faults is presented.
1965年以前，地质学家认为，两个巨大的岩石板块在圣安德烈亚斯断层上相遇，通过摩擦产生热量。
Prior to 1965 geologists assumed that the two giant rock plates meeting at the San Andreas Fault generate heat through friction as they grind past each otherd.
一些地质学家想知道，是否可以用构成断层的岩石来解释没有摩擦产生的热量。
Some geologists wondered whether the absence of friction-generated heat could be explained by the kinds of rock composing the fault.
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