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tivity on the carmel faul

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DN-48<br />

DN-48 is a flowst<strong>on</strong>e core of a<br />

type B-1 seismite. It was taken<br />

from <strong>the</strong> edge of a pool. A<br />

possible mechanism which<br />

could explain <strong>the</strong> depositi<strong>on</strong>al<br />

unc<strong>on</strong>formity could be that <strong>the</strong><br />

pool <strong>on</strong> <strong>the</strong> edge of which <strong>the</strong><br />

tilted laminas were deposited<br />

was suddenly filled with debris<br />

during a seismic event. This<br />

could have caused <strong>the</strong><br />

subsequent laminae to be<br />

deposited horiz<strong>on</strong>tally.<br />

B-1<br />

post<br />

26.83ka<br />

pre<br />

28.53ka<br />

Seismic c<strong>on</strong>tact ()

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