High Pressure Phase Relations of a Depleted Peridotite Fluxed by CO        <sub >2</sub>2        ‐H        <sub >2</sub>2        O‐Bearing Siliceous Melts and the Origin of Mid‐Lithospheric Discontinuity

Saha Sriparna; Dasgupta Rajdeep; Tsuno Kyusei

摘要

Abstract > We present phase equilibria experiments on a depleted peridotite (Mg# 92) fluxed with variable proportions of a slab‐derived rhyolitic melt (with 9.4 wt.% H <sub>2</sub> O, 5 wt.% CO <sub>2</sub> ), envisaging an interaction that could occur during formation of continents by imbrication of slabs/accretion of subarc mantles. Experiments were performed with 5 wt.% ( Bulk 2 ) and 10 wt.% ( Bulk 1 ) melt at 950–1175°C and 2–4 GPa using a piston‐cylinder and a multi‐anvil apparatus, to test the hypothesis that volatile‐bearing mineral‐phases produced during craton formation can cause reduction in aggregate shear‐wave velocities (V <sub>S</sub> ) at mid‐lithospheric depths beneath continents. In addition to the presence of olivine, orthopyroxene, clinopyroxene, and garnet/spinel, phlogopite ( Bulk 1 : 3–7.6 wt.%; Bulk 2 : 2.6–5 wt.%) at 2–4 GPa, and amphibole ( Bulk 1 : 3–9 wt.%; Bulk 2 : 2–6 wt.%) at 2–3 GPa (≤1050°C) are also present. Magnesite ( Bulk 1 : ～1 wt.% and Bulk 2 : ～0.6 wt.%) is present at 2–4 GPa (1000°C at 3 and??1050°C at 4 GPa) and its thermal breakdown coincides with the visual appearance of trace‐melt. However, an extremely small fraction of melt is inferred at all experiments based on the knowledge of fluid‐saturated peridotite solidus and the difference between bulk H <sub>2</sub> O and total H <sub>2</sub> O stored in the hydrous phases. Calculated mineral end‐member volume‐proportions were used to calculate V <sub>S</sub> of the resulting assemblage at experimental conditions and along representative continental geotherms (surface heat flow of 40–50 mWm ?2 ). We note that reactive crystallization of phlogopite?±?amphibole by infiltration of 3–10% slab‐derived hydrous‐silicic melt can cause up to 6% reduction in V <sub>S</sub> and that the estimated reduction in V <sub>S</sub> increases with increasing melt:rock ratio. The presence of phlogopite limits amphibole‐stability, making phlogopite a more likely candidate for MLDs at 100 km depth. </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> > 我们在耗尽的恒星（Mg＃92）上呈现相位平衡实验（Mg＃92），其可变比例的平板衍生的血龙晶熔体（9.4重量％H. <sub> 2 </ sub> o，5％wt.％co <sub> 2 </ sub> ），设想通过对亚级披风的平板/凸起的覆盖物形成在大陆期间可能发生的相互作用。用5重量％进行实验％（批量2 </ i> ）和10重量％（批量1 </ i> ）使用活塞缸和多铁杆装置在950-1175°C和2-4 GPA下熔化，以测试在CRATON地层中产生的含有挥发性矿物相的假设可导致骨料剪切波速度降低（ V. <sub> s </ sub> ）在大陆下部岩石深度深处。除了存在橄榄石，矫形术，Clinopococoxene和Garnet / Spinel，Phlogopite（批量1 </ i> ：3-7.6重量％; 批量2 </ i> ：2.6-5重量％）在2-4GPa和倒话（批量1 </ i> ：3-9重量％; 批量2 </ i> ：2-6重量％）在2-3GPa（≤1050℃）下也存在。菱镁矿（批量1 </ i> ：〜1重量％。％和批量2 </ i> ：〜0.6重量％）以2-4GPa（3℃，3℃，α1，在4GPa的3个）中存在，其热分解与痕量熔体的视觉外观一致。然而，基于流体饱和恒星固体的知识和散装H之间的差异，在所有实验中推断出极小的熔体。 <sub> 2 </ sub> o和总h <sub> 2 </ sub> o储存在含水阶段。计算的矿物端构件体积比例用于计算V. <sub> s </ sub> 在实验条件下产生的组合，沿着代表大陆地区（表面热流为40-50 mWM ？2 </ sup> ）。我们注意到，通过渗透3-10％的晶间碳酸二种硅熔体，蛋白β±αα±ααααααα-ααα-吡啶醇可导致v可导致v达6％ <sub> s </ sub> 并且估计v <sub> s </ sub> 随着熔体的增加而增加：岩石比。植物的存在限制锥形稳定性，使植物更可能是MLD的候选物在＆ 100公里深度。 </ 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3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=Saha Sriparna&option=202" target="_blank" rel="nofollow">Saha Sriparna;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dasgupta Rajdeep&option=202" target="_blank" rel="nofollow">Dasgupta Rajdeep;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tsuno Kyusei&option=202" target="_blank" rel="nofollow">Tsuno Kyusei;</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 Earth Environmental and Planetary SciencesRice UniversityHouston TX USA;</p> <p>Department of Earth Environmental and Planetary SciencesRice UniversityHouston TX USA;</p> <p>Department of Earth Environmental and Planetary SciencesRice UniversityHouston TX 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=cratons&option=203" rel="nofollow">cratons;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=midlithospheric discontinuity (MLD)&option=203" rel="nofollow">midlithospheric discontinuity (MLD);</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=volatile‐bearing silicic melt metasomatism&option=203" rel="nofollow">volatile‐bearing silicic melt metasomatism;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=phlogopite&option=203" rel="nofollow">phlogopite;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=pargasitic amphibole&option=203" rel="nofollow">pargasitic amphibole;</a> </p> <div class="translation"> 机译：Cratons;中型层间不连续性（MLD）;挥发性硅熔体弥扑术;植物;巴脊肉岩; </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/0704023360335.html">High Pressure Phase Relations of a Depleted Peridotite Fluxed by CO <sub >2</sub>2 ‐H <sub >2</sub>2 O‐Bearing Siliceous Melts and the Origin of Mid‐Lithospheric Discontinuity</a> <b>[J]</b> . <span> <a 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style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：在车辆的振动部分中使用的传感器包括壳体，该壳体具有轴承点，该轴承点从轴承表面在与用于固定元件的保持器相对的区域中相对于传感器中线的方向突出 </span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130424312173.html">Method for cleaning exhaust gas e.g. in metal working plant, involves holding bearing of conveyance units of discharging and transferring devices under outside positive pressure in relation to gas pressure in inner side of filter housing</a> <b>[P]</b> . <span> 外国专利：  DE102009043120A1 </span> <span> . 2011-04-07</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：清洁废气的方法，例如在金属加工厂中，涉及将卸料和转移装置的输送装置的轴承保持在相对于过滤器壳体内侧的气压为正的外部正压力下 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: auto;display:none"> <h3 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High Pressure Phase Relations of a Depleted Peridotite Fluxed by CO 22 ‐H 22 O‐Bearing Siliceous Melts and the Origin of Mid‐Lithospheric Discontinuity

摘要

High Pressure Phase Relations of a Depleted Peridotite Fluxed by CO ₂2 ‐H ₂2 O‐Bearing Siliceous Melts and the Origin of Mid‐Lithospheric Discontinuity