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Toward Robust Interpretation of Low‐Temperature Thermochronometers in Magmatic Terranes

机译：朝着岩浆地带中的低温热量计的强大解释

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Abstract >Many regions central to our understanding of tectonics and landscape evolution are active or ancient magmatic terranes, and robust interpretation of low‐temperature thermochronologic ages in these settings requires careful attention to the drivers of rock heating and cooling, including magmatism. However, we currently lack a quantitative framework for evaluating the potential role of magmatic cooling—that is, post‐magmatic thermal relaxation—in shaping cooling age patterns in regions with a history of intrusive magmatism. Here we use analytical approximations and numerical models to characterize how low‐temperature thermochronometers document cooling inside and around plutons in steadily exhuming environments. Our models predict that the thermal field a pluton intrudes into, specifically the ambient temperatures relative to the closure temperature of a given thermochronometer, is as important as the pluton size and temperature in controlling the pattern and extent of thermochronometer resetting in the country rocks around a pluton. We identify one advective and several conductive timescales that govern the relationship between the crystallization and cooling ages inside a pluton. In synthetic vertical age‐elevation relationships (AERs), resetting next to plutons results in changes in AER slope that could be misinterpreted as past changes in exhumation rate if the history of magmatism is not accounted for. Finally, we find that large midcrustal plutons, such as those emplaced at ~10–15‐km depth, can reset the low‐temperature thermochronometers far above them in the upper crust—a result with considerable consequences for thermochronology in arcs and regions with a history of magmatic activity that may not have a surface expression. </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> <P>许多地区我们对构造和景观演变的理解的核心是活跃的或古老的岩岩地面，在这些环境中对低温热量造影的强大解释需要仔细关注岩石加热和冷却的驱动器，包括岩浆。然而，我们目前缺乏用于评估岩浆冷却的潜在作用的定量框架 - 即在具有侵入性岩浆历史的地区的岩浆热弛豫 - 在地区成形冷却时代模式。在这里，我们使用分析近似和数值模型来表征低温热量计数器文件在稳步挖掘环境中的内部和芦苇周围的剪影。我们的模型预测，热场芦苇的侵入，特别是相对于给定热量计的闭合温度的环境温度，与富富乐尺寸和温度控制在乡村岩石中的热量计重置的图案和程度上芦苇。我们鉴定了一种方向性和几个导电时间尺度，用于控制芦苇内的结晶和冷却年龄之间的关系。在综合垂直年龄 - 高度关系（AARS）中，钚旁边重置，如果岩浆史没有考虑，可以误解为过去的送达率的变化。最后，我们发现大型的中性型材，例如在〜10-15公里的深度上施加的那些，可以将远高于其上方的低温热化学计 - A的结果，在弧形和地区的热量造成相当大的后果中的结果岩石活动的历史可能没有表面表达。</ 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10期</span><b style="margin: 0 2px;">|</b><span>共25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=Murray Kendra E.&option=202" target="_blank" rel="nofollow">Murray Kendra E.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Braun Jean&option=202" target="_blank" rel="nofollow">Braun Jean;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Reiners Peter W.&option=202" target="_blank" rel="nofollow">Reiners Peter W.;</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 GeosciencesUniversity of ArizonaTucson AZ USA;</p> <p>ISTerreUniversité Grenoble‐Alpes CNRSGrenoble Cedex France;</p> <p>Department of GeosciencesUniversity of ArizonaTucson AZ USA;</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=He thermochronology&option=203" rel="nofollow">He thermochronology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Péclet number&option=203" rel="nofollow">Péclet number;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=age‐elevation relationships&option=203" rel="nofollow">age‐elevation relationships;</a> </p> <div class="translation"> 机译：他的热量学;Péclet号码;年龄高度的关系; 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