tivity on the carmel faul
tivity on the carmel faul
tivity on the carmel faul
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extremely high errors for <strong>the</strong>se values and make any calculati<strong>on</strong> for a correcti<strong>on</strong> factor<br />
highly suspicious (Tables 1b,2b,3b). Since <strong>the</strong>se correcti<strong>on</strong> factors vary between samples<br />
with high detrital c<strong>on</strong>tents (i.e. 230 Th/ 232 Th 100), it is possible that it is not indicative of a single phase or origin of<br />
detrital matter. It was <strong>the</strong>refore not possible to establish a unique correcti<strong>on</strong> factor for<br />
Denya Cave initial 230 Th.<br />
39
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