Abstract
A depth profile of cosmogenic neutron-capture-produced 36Cl was measured in quartz extracted from a siliceous dolomite ejecta boulder drill core at Meteor Crater, AZ. The results show a maximum in production below the top surface of the boulder and are consistent with the depth dependence of production predicted by Monte Carlo calculations. A model is presented here that uses the special features of the profile to determine both the exposure age and steady-state erosion rate of a geomorphic surface.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 301-307 |
| Number of pages | 7 |
| Journal | Nuclear Inst. and Methods in Physics Research, B |
| Volume | 92 |
| Issue number | 1-4 |
| DOIs | |
| State | Published - Jun 3 1994 |
| Externally published | Yes |
ASJC Scopus subject areas
- Nuclear and High Energy Physics
- Instrumentation
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