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Spreading rate‐dependent variations in crystallization along the global mid‐ocean ridge system

机译：沿全球中海脊系统结晶的速率依赖性变化

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Abstract > We investigate crustal accretion at mid‐ocean ridges by combining crystallization pressures calculated from major element contents in mid‐ocean ridge basalt (MORB) glasses and vapor‐saturation pressures from melt inclusions and MORB glasses. Specifically, we use established major element barometers and pressures estimated from 192 fractional crystallization trends to calculate crystallization pressures from 9000 MORB glasses across the global range of mid‐ocean ridge spreading rates. Additionally, we estimate vapor‐saturation pressures from 400 MORB glasses from PETDB and 400 olivine‐hosted melt inclusions compiled from five ridges with variable spreading rates. Both major element and vapor‐saturation pressures increase and become more variable with decreasing spreading rate. Vapor saturation pressures indicate that crystallization occurs in the lower crust and upper mantle at all ridges, even when a melt lens is present. We suggest that the broad peaks in major element crystallization pressures at all spreading rates reflects significant crystallization of on and off‐axis magmas along the base of a sloping lithosphere. Combining our observations with ridge thermal models we show that crystallization occurs over a range of pressures at all ridges, but it is enhanced at thermal/rheologic boundaries, such as the melt lens and the base of the lithosphere. Finally, we suggest that the remarkable similarity in the maximum vapor‐saturation pressures (～3 kbars) recorded in melt inclusions from a wide range of spreading rates reflects a relatively uniform CO <sub>2</sub> content of 50–85 ppm for the depleted upper mantle feeding the global mid‐ocean ridge system. </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”> <标题类型=“main”>抽象</ title> > 我们通过将来自中海脊玄武岩（Morb）眼镜（Morb）眼镜（Morb）眼镜（Morb）眼镜（Morb）和Morb眼镜的气相饱和压力组合来调查中海脊在中海脊的地壳吸收。具体而言，我们使用的主要元件气压计和压力从192分数结晶趋势估计，从而计算来自＆gt的结晶压力。在全球中海岭传播速率的全球范围内的9000个Morb眼镜。另外，我们估计来自PetdB的蒸汽饱和压力。来自PetdB的400天变量玻璃和400个终端封锁400个终端宿主的熔体夹杂物，从五个脊，具有可变扩散速率。主要元素和气相饱和度压力增加并随着降低的扩散速率而变得更大。蒸汽饱和压力表明，即使存在熔体透镜，也可以在所有脊处的下地壳和上部罩中发生结晶。我们认为，所有展开率的主要元素结晶压力中的宽峰反映了沿着斜坡斜率底座的轴上和轴外岩浆的显着结晶。将我们的观察结果与脊热模型相结合，我们表明结晶在所有脊的压力范围内发生，但它在热/流变界限下增强，例如熔体透镜和岩石圈的基部。最后，我们建议从广泛的扩频率记录在熔体夹杂物中的最大蒸汽饱和压力（〜3 kbars）的显着相似性反映了相对统一的CO <sub> 2 </ sub> 耗尽全球中海脊系统的耗尽上部地幔含量为50-85ppm。 </ 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>2017年第8期</span><b style="margin: 0 2px;">|</b><span>共18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=Wanless V. Dorsey&option=202" target="_blank" rel="nofollow">Wanless V. Dorsey;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Behn Mark D.&option=202" target="_blank" rel="nofollow">Behn Mark D.;</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 GeosciencesBoise State UniversityBoise Idaho USA;</p> <p>Department of Geology and GeophysicsWoods Hole Oceanographic InstitutionWoods Hole Massachusetts 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=mid‐ocean ridges&option=203" rel="nofollow">mid‐ocean ridges;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=crustal accretion&option=203" rel="nofollow">crustal accretion;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=crystallization&option=203" rel="nofollow">crystallization;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=volatiles&option=203" rel="nofollow">volatiles;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=melt inclusions&option=203" rel="nofollow">melt inclusions;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=thermal models&option=203" rel="nofollow">thermal models;</a> </p> <div class="translation"> 机译：中海脊;地壳吸收;结晶;挥发物;熔体夹杂物;热模型; </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/0704025950162.html">Spreading rate-dependent variations in crystallization along the global mid-ocean ridge system</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wanless V. 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href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=马传桃&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 马传桃</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=许建平&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,许建平</a> <span> <a href="/journal-cn-53611/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 湖南医科大学学报 </a> </span> <span> . 1993</span><span>,第002期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-34388_thesis/020221096882.html">地球自转速率变化引起全球应力场的有限元分析</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王连捷&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 王连捷</a> <span> <a href="/conference-cn-34388/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 中国地球物理学会第13届年会 </a> <span> <span> . 1997</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020311817999.html">非输血依赖性β-地中海贫血患者γ-珠蛋白基因的表达及调控研究</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=黄语妹&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 黄语妹</a> <span> . 2017</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06120402487.html">结合通用移动通信系统/全球移动通信系统/全球演进增强资料速率无线系统的控制方法及装置</a> <b>[P]</b> . <span> 中国专利： CN100397928C </span> <span> . 2008.06.25</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120104852357.html">结合通用移动通信系统/全球移动通信系统/全球演进增强资料速率无线系统的控制方法及装置</a> <b>[P]</b> . <span> 中国专利： CN1659912A </span> <span> . 2005-08-24</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130420365607.html">The combination of energy generated from ocean currents, including a major floating body, orientated through the direction of ocean currents, depends on the rotor medium of the floating body, at least one stabilizer, anchor line; crystallization. NTO is used to generate energy from ocean currents, including a major floating body parallel to the direction of ocean currents.</a> <b>[P]</b> . <span> 外国专利：  CL2012000870A1 </span> <span> . 2012-12-14</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：洋流产生的能量的组合，包括一个主要的浮体，通过海流的方向定向，取决于浮体的转子介质，至少一条稳定器，锚固线;结晶。 NTO用于从洋流中产生能量，包括与洋流方向平行的主要漂浮体。 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130421290543.html">MID-OCEAN RIDGES IN ATLANTIC AND INDIAN OCEANS, AND CONTINENTAL DRIFT</a> <b>[P]</b> . <span> 外国专利：  JP2013110931A </span> <span> . 2013-06-06</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：大西洋和印度洋中的洋脊和大陆漂移 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130427913006.html">I grew up on a farm, preparing to transition from a freshwater to a saltwater settlement, including providing a food component for the Global Ocean Observing System (GOOS) and feeding it to the Global Ocean Observing System (GOOS) and/or Parr.</a> <b>[P]</b> . <span> 外国专利：  CL2009001164A1 </span> <span> . 2010-04-09</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：我在一个农场长大，准备从淡水过渡到咸水定居点，包括为全球海洋观测系统（GOOS）提供食物成分并将其提供给全球海洋观测系统（GOOS）和/或Parr。 </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" 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