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Quantifying the Correlation Between Mobile Continents and Elevated Temperatures in the Subcontinental Mantle

机译：量化移动大陆之间的相关性和亚联土地幔中的温度升高

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Abstract >Continents influence the mantle's convective wavelength and the heat flow escaping from the planet's surface. Over the last few decades, many numerical and analytical studies have contributed to the debate about whether the continents can warm up the subcontinental mantle or not and if they do, then to what extent? However, a consensus regarding the exact nature and magnitude of this correlation between continents and elevated temperatures in the subcontinental mantle remains to be achieved. By conducting a systematic parameter study using 2‐D global mantle convection simulations with mobile continents, we provide qualitative and quantitative observations on the nature of this correlation. In our incompressible and compressible convection models, we observe the general processes of downwellings bringing cold material into the mantle along continental margins and a subsequent buildup of warm thermal anomalies underneath the continents. We compute the amplitude and degree of this correlation using spectral decomposition of the temperature and composition fields. The dominant degree of correlation evolves with time and changes with continental configuration. Using simple empirical fits, we observe that this correlation decreases with increasing core temperature, number of continents, internal heating, or decreasing reference viscosity. We also report simple regressions of the time dependence of this correlation. Additionally, we show that decompression melting as a result of a mantle upwelling or small‐scale sublithospheric convection leads to voluminous volcanism. The emplacement of this dense basalt‐eclogite material breaks the continents apart and destroys the correlation. </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”XML：ID =“GGGE21827-ABS-ABS-0001”> <标题类型=“main”>抽象</ title> >大陆影响地幔的对流波长，并且从行星表面逸出的热流。在过去的几十年中，许多数值和分析研究有助于辩论大陆是否可以在多大程度上进行大陆，然后在多大程度上进行争论？然而，关于亚洲地幔中的大陆和升高的温度之间的这种相关性的确切性质和程度的共识仍有待实现仍然达到仍有待实现的仍有待实现。通过使用移动大陆的2-D全球地幔对流模拟进行系统参数研究，我们对这种相关性的性质提供了定性和定量观察。在我们不可压缩和可压缩的对流模型中，我们观察沉船的一般过程将冷材料带入沿着大陆边缘的地幔，随后在大陆下的温暖热异常积聚。我们使用温度和组成字段的光谱分解来计算这种相关性的幅度和程度。主导相关程度随着时间的推移和大陆配置而变化。使用简单的经验拟合，我们观察到这种相关性随着核心温度，大洲数量，内部加热的数量，内部加热或降低参考粘度而降低。我们还报告了这种相关性时间依赖性的简单回归。此外，我们表明，由于地幔上升或小规模的副间散对对流导致大量的火山，因此减压熔化。这种致密的玄武岩 - eClogite材料的施加打破了大陆分开并破坏了相关性。</ 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>2019年第3期</span><b style="margin: 0 2px;">|</b><span>共29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=Jain C.&option=202" target="_blank" rel="nofollow">Jain C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rozel A. B.&option=202" target="_blank" rel="nofollow">Rozel A. B.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tackley P. J.&option=202" target="_blank" rel="nofollow">Tackley P. J.;</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>Institute of Geophysics Department of Earth SciencesETH ZurichZurich Switzerland;</p> <p>Institute of Geophysics Department of Earth SciencesETH ZurichZurich Switzerland;</p> <p>Institute of Geophysics Department of Earth SciencesETH ZurichZurich Switzerland;</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=mantle convection&option=203" rel="nofollow">mantle convection;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=continents&option=203" rel="nofollow">continents;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=correlation&option=203" rel="nofollow">correlation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=subcontinental mantle temperatures&option=203" rel="nofollow">subcontinental mantle temperatures;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=continental flood basalts&option=203" rel="nofollow">continental flood basalts;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=numerical modeling&option=203" rel="nofollow">numerical modeling;</a> </p> <div class="translation"> 机译：地幔对流;洲;相关;亚丁风格罩温度;大陆洪水基础;数值建模; </div> </li> </ul> </div> </div> <div class="literature cardcommon"> <div class="similarity "> <h3 class="all_title" id="enpatent66">相似文献</h3> <div class="similaritytab clearfix"> <ul> <li class="active" >外文文献</li> <li >中文文献</li> <li >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704023360481.html">Quantifying the Correlation Between Mobile Continents and Elevated Temperatures in the Subcontinental Mantle</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jain C.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Jain C.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rozel A. 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