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Apatite to Zircon, Inc., 1075 Matson Road, Viola, Idaho 83872-9709, U.S.A., Department of Geological Sciences, University of Nevada-Reno, Reno, Nevada 89557-0138, U.S.A., donelick@apatite.com
Apatite to Zircon, Inc., 1075 Matson Road, Viola, Idaho 83872-9709, U.S.A., Department of Geological Sciences, University of Idaho, Moscow, Idaho 83844-3022, U.S.A.
Jackson School of Geosciences, University of Texas at Austin Austin, Texas, 78712-0254, U.S.A.
| The first 20% of the full text of this article appears below. |
| INTRODUCTION |
|---|
Etched, natural fission tracks in several apatite grains are shown in Figure 1
. Successful AFT analysis is limited by the following: 1) the availability of apatite from which useful AFT data can be obtained, often due to a lack of apatite of sufficient grain size and quality within available rock types, or, alternatively, the lack of available rock samples due to minimal outcrop exposure or other reasons, 2) economic considerations in terms of the time and money required to obtain sufficient AFT data, 3) the inherent limitations of AFT data to resolve geological thermal history information, often related to limited numbers of accumulated spontaneous fission tracks due to low
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