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5 results for “fission track”
Supporting information for: An assessment of monazite fission-track thermochronology as a proxy for low-magnitude cooling, Catalina-Rincon Metamorphic Core Complex, AZ, U.S.A.
<p><span>The following supporting information contains: The detailed location and age data for the geochronological, isotopic, and geochemical data used in this study, and their associated publications. Detailed thermochronometric data and associated thermal history modelling information for all thermochronology and modelling presented in the study.</span></p>
Table 1 in Fission track dating of obsidian source samples from the Willaumez Peninsula, Papua New Guinea and eastern Australia
<p>Table 1. Measurement of thermal neutron fluence.1</p><table><tbody><tr><th>monitor</th><th>external detector</th><th>B (109ntl)</th><th>trackdensity onext.detector (105tcm2)</th><th>thermal neutronfluence (1015ncm2)</th></tr></tbody><tbody><tr><th>Auwire</th><td>TODO</td><td>TODO</td><td>TODO</td><td>2.399±0.034</td></tr><tr><th>Cowire</th><td>TODO</td><td>TODO</td><td>TODO</td><td>2.392±0.025</td></tr><tr><th>CNlglass</th><td>mIca</td><td>1.873±0.025</td><td>13.43±0.26</td><td>2.515±0.036</td></tr><tr><td>makrofol</td><td>1.863±0.023</td><td>13.24±0.26</td><td>2.468±0.058</td></tr><tr><th>CN2glass</th><td>mIca</td><td>1.985±0.007</td><td>12.34±0.25</td><td>2.449±0.051</td></tr><tr><td>makrofol</td><td>2.016±0.041</td><td>12.31±0.25</td><td>2.482±0.072</td></tr></tbody></table><p>1 Calibration of glass dosimeters (B value measurement) was performed by using cobalt and gold monitors (Bonetti <i>et al.,</i> 1994). The thermal neutron fluence value used in the age measurements has been obtained as a weighted mean of the values listed in the last column.</p>
Table 2 in Fission track dating of obsidian source samples from the Willaumez Peninsula, Papua New Guinea and eastern Australia
<p>Table 2. Results for fission track dating of Papua New Guinean obsidians.1</p><table><tbody><tr><th></th><th></th><th>spontaneous</th><th></th><th>induced</th><th>neutron</th><th></th></tr></tbody><tbody><tr><th>sample</th><td>ns</td><td>trackdensity</td><td>nj</td><td>trackdensity</td><td>fluence</td><td>age±</td></tr><tr><th></th><td>(t)</td><td>(tcm2)</td><td>(t)</td><td>(x104tcm2)</td><td>(X1015 ncm-2)</td><td>(a)</td></tr><tr><th>Baki</th><td>11</td><td>17</td><td>2933</td><td>5.54</td><td>1.644±0.014</td><td>30198±8906</td></tr><tr><th>Kutau</th><td>15</td><td>14</td><td>7094</td><td>5.16</td><td>1.644±0.014</td><td>26707±7688</td></tr></tbody></table><p>1 ns and nj represent the number of spontaneous and induced tracks counted, respectively. The induced track density has been evaluated by means of the population subtraction method. Ages are calculated by using the following constants (Ao; = 1.551 x 1O-lOa·1, <i>238U/235U</i> = 137.88, O"f = 580.2 b, Af = 7.03 x 1O.17a-1). The thermal neutron fluence is determined from both two calibrated mica and Makrofol detectors in contact with glass dosimeters (Coming CNl, CN2) and two metallic monitors (Co, Au). All corrected ages are weighted means of values in the plateau region.</p>
Table 3 in Fission track dating of obsidian source samples from the Willaumez Peninsula, Papua New Guinea and eastern Australia
<p>Table 3. Results of fission track dating of Australian obsidian samples; ns' nj+s represent the number of spontaneous and induced+spontaneous tracks being counted, respectively. See Table 2 for constants. (*) In this case the corrected age is determined by using the correction curve of sample AU602.</p><table><tbody><tr><th></th><th>spontaneous</th><th></th><th>induced</th><th>neutron</th><th></th><th>apparentheatingcorrected</th></tr><tr><th>sample</th><th>ns trackdensity (t) (x104tcm-2)</th><th>lli+s (t)</th><th>trackdensity (x105tcm-2)</th><th>fluence (X1015 ncm-2)</th><th>Ds/Di</th><th>age±0" (Ma)</th><th>hours at 140°C</th><th>age±0" (Ma)</th></tr><tr><th>Far North Queensland (FNQ)</th></tr></tbody><tbody><tr><th>AU602</th><td>2533 8.17±0.16</td><td>3736</td><td>3.51 ±0.07</td><td>2.431 ±0.016</td><td>0.63 ±0.06</td><td>33.9± 1.1</td><td>60</td><td>86.9±3.8</td></tr><tr><th>AU603</th><td>1390 7.25 ± 0.19</td><td>3666</td><td>3.23 ±0.07</td><td>2.431 ± 0.016</td><td>0.54 ± 0.05</td><td>32.7 ± 1.3</td><td>(*)</td><td>88.5 ± 9.0</td></tr><tr><th>AU612</th><td>278 10.86±0.65</td><td>1002</td><td>4.13 ±0.15</td><td>2.431 ±0.016</td><td>0.68±0.07</td><td>38.2±3.2</td><td>(*)</td><td>92.3 ± 10.6</td></tr><tr><th>AU662</th><td>122 4.24±0.38</td><td>608</td><td>1.69 ±0.09</td><td>1.644 ±0.014</td><td>0.53 ±0.10</td><td>24.7 ± 3.1</td><td>70</td><td>85.5 ± 5.9</td></tr><tr><th>New South Wales (NSW</th></tr><tr><th>AUlOl</th><td>273 2.32±</td><td>0.14</td><td>8982.57</td><td>±0.092.431</td><td>±0.016</td><td>0.79±0.06</td><td>13.1</td><td>TODO</td></tr><tr><th>AUl02</th><td>95 1.48±</td><td>0.15</td><td>7602.23</td><td>±0.092.431</td><td>0.016</td><td>TODO</td><td>9.7</td><td>TODO</td></tr></tbody></table>
Apatite fission track data from debris from the basal ice of the Byrd ice core, central West Antarctica
<p>This dataset comprises of 10 apatite fission track ages. Apatite grains were picked out of the 75-150 micron size fraction of debris melted from two intervals of basal ice from the Byrd ice core. The Byrd ice core was drilled at 80<i><strong>°</strong></i> 0.1'S, 119<i><strong>°</strong></i> 31.0'W at Byrd Station, West Antarctica, in January 1968.</p>
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