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Lab 10: Kinematic Indicators and Strain Analysis - Geophysics at ...

Lab 10: Kinematic Indicators and Strain Analysis - Geophysics at ...

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Slickenlines<br />

• linear fe<strong>at</strong>ures,<br />

known as slickenlines,<br />

are formed by the<br />

rocks on two sides of<br />

a fault sliding past<br />

each other<br />

• slickenlines indic<strong>at</strong>e<br />

the general sense of<br />

motion on a fault, but<br />

they cannot tell you<br />

absolute motion by<br />

themselves

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