PALEOBOTANICAL INVESTIGATION OF EARLY TERTIARY PALAEOELEVATIONS IN NORTHEASTERN NEVADA - INITIAL RESULTS
Physical models of surface uplift rates can be evaluated using palaeobotanically determined estimates of surface heights through time. Some classes of physical model imply that surface uplift rates are too great to be accounted for by known rates of crustal thickening. If these rates could be confir...
| Main Authors: | , , |
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| Format: | Conference item |
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1994
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