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Reproducibility of Thermal History Reconstruction From Apatite Fission‐Track and (U‐Th)/He Data

机译：磷灰石裂变轨道和（U-TH）/ HE数据的热历史重建再现性

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Abstract > We report a new interlaboratory exercise to evaluate the reproducibility of apatite fission‐track (AFT) and (U‐Th)/He (AHe) data and thermal history analysis. Twelve laboratory groups participated, analyzing apatite separates from two previously studied localities. Ten groups returned AFT data from 13 analysts, five groups returned AHe data, one contributed apatite U/Pb data, and nine contributed thermal history models. Submitted AFT age data were generally consistent with the original studies and each other to within uncertainties, although there were departures, particularly among results obtained using laser ablation inductively coupled plasma mass spectrometry for uranium determination. AFT‐confined track‐length data showed more variation, which correlated between samples, suggesting that they may reflect analyst‐specific factors. Accounting for anisotropy using c axis projection reduced the variation and correlation. AHe ages showed more dispersion than observed in the previous studies, with one sample showing many ages consistent with prior work but also many significantly older ages, and the other roughly matching prior work but showing symmetrical scatter suggesting a 1SE uncertainty of 17–21%. Thermal history models generally agreed in their major features but showed considerable variation in detail, due to differences in data and data entry, model setup, and modeling software approach. Addressing pitfalls in data entry and model setup improved congruence, as would greater emphasis on AFT length and etch figure calibration. Because of scatter, AHe data had to be entered selectively into the models to achieve reasonable results. Although cautionary in several respects, study results point to promising avenues for improving the reproducibility of thermal history modeling. </abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> <div class="translation abstracttxt"> <span class="zhankaihshouqi fivelineshidden" id="abstract"> <span>机译：</span><Abstract Type =“Main”XML：Lang =“en”> <标题类型=“main”>抽象</ title> > 我们报告了一个新的互别练习，以评估磷灰石裂变轨道（AFT）和（U-TH）/ HE（AHE）数据和热历史分析的再现性。 12个实验室组参加，分析磷灰石与前一位先前研究的地方分离。十组从13分析师返回AFT数据，五组返回AHE数据，一个贡献的磷灰石U / PB数据，九个贡献的热历史模型。提交的后续年龄数据通常与原始研究和彼此一致，尽管存在偏离的不确定性，但特别是在使用激光烧蚀电感耦合等离子体质谱法得到铀的测定获得的结果。尾声轨迹长度数据显示出更多的变异，它们在样品之间相关，这表明它们可能反映分析人特定的因素。占各向异性的使用 c </ i> 轴投影减少了变化和相关性。 AHE AGES显示出比以往的研究中观察到的比较多，一个样本显示出许多年龄与现有工作一致，而且还有许多较大的年龄，以及其他粗略匹配的现有工作，但显示对称分散，表明1SE不确定性为17-21％。由于数据和数据输入，模型设置和建模软件方法的差异，热历史模型通常在其主要功能中同意，但详细介绍了相当大的变化。在数据输入和模型设置中寻址陷阱改进的同时，更加强调AFT长度和蚀刻图校准。由于分散，必须选择性地进入模型的AHE数据以实现合理的结果。虽然在几个方面警告虽然谨慎，但研究结果指出了提高热历史建模的再现性的承诺途径。 </ p> </摘要> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> </div> <div class="record"> <h2 class="all_title" id="enpatent33" >著录项</h2> <ul> <li> <span class="lefttit">来源</span> <div style="width: 86%;vertical-align: text-top;display: inline-block;"> <a href='/journal-foreign-23285/'>《Geochemistry, geophysics, geosystems》</a> <b style="margin: 0 2px;">|</b><span>2018年第8期</span><b style="margin: 0 2px;">|</b><span>共26页</span> </div> </li> <li> <div class="author"> <span class="lefttit">作者</span> <p id="fAuthorthree" class="threelineshidden zhankaihshouqi"> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ketcham Richard A.&option=202" target="_blank" rel="nofollow">Ketcham Richard A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Beek Peter&option=202" target="_blank" rel="nofollow">Beek Peter;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Barbarand Jocelyn&option=202" target="_blank" rel="nofollow">Barbarand Jocelyn;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bernet Matthias&option=202" target="_blank" rel="nofollow">Bernet Matthias;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gautheron Cécile&option=202" target="_blank" rel="nofollow">Gautheron Cécile;</a> </p> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zkzz" style="display: none;">展开▼</span> </div> </li> <li> <div style="display: flex;"> <span class="lefttit">作者单位</span> <div style="position: relative;margin-left: 3px;max-width: 639px;"> <div class="threelineshidden zhankaihshouqi" id="fOrgthree"> <p>Department of Geological Sciences Jackson School of GeosciencesUniversity of Texas at AustinAustin TX USA;</p> <p>Institut des Sciences de la TerreUniversité Grenoble AlpesGrenoble France;</p> <p>GEOPS Université Paris‐Sud CNRSUniversité Paris‐SaclayOrsay France;</p> <p>Institut des Sciences de la TerreUniversité Grenoble AlpesGrenoble France;</p> <p>GEOPS Université Paris‐Sud CNRSUniversité Paris‐SaclayOrsay France;</p> </div> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zhdw" style="display: none;">展开▼</span> </div> </div> </li> <li > <span class="lefttit">收录信息</span> <span style="width: 86%;vertical-align: text-top;display: inline-block;"></span> </li> <li> <span class="lefttit">原文格式</span> <span>PDF</span> </li> <li> <span class="lefttit">正文语种</span> <span>eng</span> </li> <li> <span class="lefttit">中图分类</span> <span><a href="https://www.zhangqiaokeyan.com/clc/163.html" title="地球物理学">地球物理学;</a></span> </li> <li class="antistop"> <span class="lefttit">关键词</span> <p style="width: 86%;vertical-align: text-top;"> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=fission‐track&option=203" rel="nofollow">fission‐track;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=(U‐Th)/He&option=203" rel="nofollow">(U‐Th)/He;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=thermal history modeling&option=203" rel="nofollow">thermal history modeling;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=interlab calibration&option=203" rel="nofollow">interlab calibration;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=thermochronology&option=203" rel="nofollow">thermochronology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=reproducibility&option=203" rel="nofollow">reproducibility;</a> </p> <div class="translation"> 机译：裂变轨道;（u-th）/他;热历史建模;Interlab校准;热量校准;再现性; 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