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stratigraphic separation

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stratigraphic separation [¦strad·ə¦graf·ik ‚sep·ə′rā·shən]


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If the sequence coal, shale, sandstone that is exposed between zero and 30 feet is the same sequence, repeated by the west fault, as that exposed from 153-183 feet (Figure 3), then the stratigraphic separation and the slip of the fault would be approximately 80 feet.
Valley anticline associated with the Warrensburg Sandstone in Missouri by Nold, John L. / Transactions of the Missouri Academy of Science
 
 
 
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