题目内容

Nonconformity is also called sedimentary contact and disconformity is called parallel unconformity.

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The evidences of faults in the field incude:

A. slickenside
B. fault breccia
C. fault gouge
D. drag fold
E. fault scarps

Fault gouge is very fine-grained, unconsolidated material consisting of pulverized rock fragments.

A slickenside is a smooth, striated, polished surface and can be used to determine the direction and sense of motion on a fault.

A joint is a crack along which there has been no appreciable movement, while fault is a fracture with relative movement of the rocks on both sides of it, parallel to the fracture.

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