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Generation of Earth's Early Continents From a Relatively Cool Archean Mantle

机译:从一个相对凉爽的成语地幔那一代地球早期的大陆

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Abstract > Several lines of evidence suggest that the Archean (4.0–2.5?Ga) mantle was hotter than today's potential temperature ( <fi>T</fi> <sub> <fi>P</fi> </sub> ) of 1350 °C. However, the magnitude of such difference is poorly constrained, with <fi>T</fi> <sub> <fi>P</fi> </sub> estimation spanning from 1500 to 1600 °C during the Meso‐Archean (3.2–2.8?Ga). Such differences have major implications for the interpreted mechanisms of continental crust generation on the early Earth, as their efficacy is highly sensitive to the <fi>T</fi> <sub> <fi>P</fi> </sub> . Here we integrate petrological modeling with thermomechanical simulations to understand the dynamics of crust formation during Archean. Our results predict that partial melting of primitive oceanic crust produces felsic melts with geochemical signatures matching those observed in Archean cratons from a mantle <fi>T</fi> <sub> <fi>P</fi> </sub> as low as 1450 °C thanks to lithospheric‐scale RayleighTaylor‐type instabilities. These simulations also infer the occurrence of intraplate deformation events that allow an efficient transport of crustal material into the mantle, hydrating it. </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 =“GGGE21831-ABS-ABS-0001”> <标题类型=“main”>抽象</ title> > 一些证据表明,Archean(4.0-2.5?Ga)披露的披风比今天的潜在温度更热( <fi> t </ fi> <sub> <fi> p </ fi> </ sub> )1350℃。然而,这种差异的幅度受到严重限制 <fi> t </ fi> <sub> <fi> p </ fi> </ sub> 在Meso-Archean(3.2-2.8〜GA)期间估计从1500到1600°C跨越。这种差异对早期地球上的大陆地壳发电的解释机制具有重大影响,因为它们的疗效对效果非常敏感 <fi> t </ fi> <sub> <fi> p </ fi> </ sub> 。在这里,我们将思科建模整合到热机械模拟,以了解Archean期间的地壳形成的动态。我们的结果预测,原始海底的部分熔化产生了与地幔中观察到的地球化学签名的肠道熔化 <fi> t </ fi> <sub> <fi> p </ fi> </ sub> 由于岩石尺寸Rayleightor-型无限度,低至1450°C。这些模拟还推断出缺口变形事件的发生,使得地壳材料的有效运输到地幔中,保湿。 </ 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4期</span><b style="margin: 0 2px;">|</b><span>共19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=Piccolo Andrea&option=202" target="_blank" rel="nofollow">Piccolo Andrea;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Palin Richard M.&option=202" target="_blank" rel="nofollow">Palin Richard M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kaus Boris J.P.&option=202" target="_blank" rel="nofollow">Kaus Boris J.P.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=White Richard W.&option=202" target="_blank" rel="nofollow">White Richard 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>Institute for GeosciencesJohannes‐Gutenberg University of MainzMainz Germany;</p> <p>Department of Geology and Geological EngineeringColorado School of MinesGolden CO USA;</p> <p>Institute for GeosciencesJohannes‐Gutenberg University of MainzMainz Germany;</p> <p>School of Earth and Environmental SciencesUniversity of St AndrewsSt Andrews UK;</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=continental crust&option=203" rel="nofollow">continental crust;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=early Earth&option=203" rel="nofollow">early Earth;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=geodynamic modeling&option=203" rel="nofollow">geodynamic modeling;</a> </p> <div class="translation"> 机译:大陆地壳;早期地球;地球动力学建模; 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Hawkesworth</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=张兴春&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,张兴春</a> <span> <a href="/journal-cn-50777/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 地质地球化学 </a> </span> <span> . 1991</span><span>,第6期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-4449_thesis/020221076681.html">前寒武纪大陆弧之下地幔再造:华南中生代安山岩的地球化学记录</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=陈龙&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 陈龙</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=赵子福&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,赵子福</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=郑永飞&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,郑永飞</a> <span> <a href="/conference-cn-4449/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 中国矿物岩石地球化学学会第14届学术年会 </a> <span> <span> . 2013</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020316045771.html">辽西中生代岩石圈地幔特征:义县组玄武岩中捕虏晶的矿物学和地球化学制约</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=许瑶&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 许瑶</a> <span> . 2020</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06130449138446.html">INNER STATIONARY PLANET MEANS, GLOBAL WARMING PREVENTING MEANS, EARTH METEOROLOGY CONTROL MEANS, ULTRAVIOLET RAY SHIELDING MEANS, SOLAR OBSERVATION PLANET MEANS, SOLAR POWER GENERATION PLANET MEANS, VENUS COOLING MEANS, OUTER STATIONARY PLANET MEANS, AND 'SOLAR ECLIPSE WHERE SUN HIDES EARTH OR GLOBAL ATMOSPHERE' OBSERVATION/SIGHTSEENG PLANET MEANS, MARS WARMING MEANS, JUPITER WARMING MEANS, TELESCOPIC PLANET MEANS, MAGNETIC FIELD OBSERVATION PLANET MEANS, EARTH MAGNETIC FIELD OBSERVATION PLANET MEANS, INNER GEOSTATIONARY SATELLITE MEANS OF SAME REVOLUTION ANGULAR VELOCITY TYPE, OUTER GEOSTATIONARY SATELLITE MEANS OF SAME REVOLUTION ANGULAR VELOCITY TYPE, 'EARTH ECLIPSE WHERE MOON HIDES EARTH' OBSERVATION/SIGHTSEENG SATELLITE MEANS, SPACE COMMUNICATION MEANS BETWEEN HIDDEN SIDE OF MOON AND EARTH, INNER STATIONARY CELESTIAL BODY MEANS OF SAME REVOLUTION ANGULAR VELOCITY TYPE, OUTER STATIONARY CELESTIAL BODY MEANS OF SAME REVOLUTION ANGULAR VELOCITY TYPE, LIGHT TRANSMISSIVE QUANTITY CONTR</a> <b>[P]</b> . <span> 外国专利: <!-- 日本专利: --> JP2001001997A </span> <span> . 2001-01-09</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译:内陆行星系手段,全球变暖预防手段,地球气象控制手段,紫外射线屏蔽手段,太阳能观测行星手段,太阳能发电行星手段,金星冷却手段,外地静止行星手段以及日月偏远大气观测/视场手段,火星暖化手段,准星变暖手段,望远镜观测手段,磁场观测观测手段,地球磁场观测观测手段,内地静止卫星同等旋转度的卫星平均值旋转角速度类型,“月蚀掩盖地球的月蚀”观测/高度卫星卫星,月球和地球之间的空间通信方式,同心转角角质体体位,同心转角V角均值角速度类型,光透射量转换 </span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06130403078137.html">METHOD OF GENERATION AND EVALUATION OF ENERGY OF GRAVITON RADIATION OF THE EARTH MANTLE</a> <b>[P]</b> . <span> 外国专利: <!-- 俄罗斯专利: --> RU2017144169A </span> <span> . 2019-06-10</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译:地球幔引力辐射的产生与评价方法 </span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130403078136.html">METHOD OF GENERATION AND EVALUATION OF ENERGY OF GRAVITON RADIATION OF THE EARTH MANTLE</a> <b>[P]</b> . <span> 外国专利: <!-- 俄罗斯专利: --> RU2017144169A3 </span> <span> . 2019-06-10</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译:地球幔引力辐射的产生与评价方法 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: auto;display:none"> <h3 class="all_title" id="enpatent55">相关主题</h3> <ul id="subject"> </ul> </div> </div> </div> </div> <div class="right rightcon"> <div class="details_img cardcommon clearfix" style="margin-bottom: 10px;display:none;" > </div> </div> </div> <div id="thesis_get_original1" class="downloadBth" style="bottom: 19px;z-index: 999;" onclick="ywcd('0704023360491','4',7,2,1,'',this,24)" class="delivery" prompt="010401" title="通过人工服务将文献原文发送至邮箱" >获取原文</div> <div class="journalsub-pop-up" style="display: none"> <div class="journal-sub"> <h2>期刊订阅</h2> <img src="https://cdn.zhangqiaokeyan.com/img/loginclose.png" alt="" onclick="$('.journalsub-pop-up').hide()"> <p 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