Outgassing of Mantle Volatiles in Compressional Tectonic Regime Away From Volcanism: The Role of Continental Delamination

Caracausi Antonio; Sulli Attilio

摘要

Abstract > In this study we discuss the occurrence of mantle‐derived heat and volatiles (i.e., helium and CO <sub>2</sub> ) feeding hydrothermal systems in a seismically active margin between two convergent plates (African and European) without any signals of volcanism. The helium (He) isotopes clearly indicate a mantle‐derived component in the outgassing volatiles. The estimated mantle‐derived He fluxes are up to two to three orders of magnitude greater than those in a stable continental area. Such high He fluxes cannot be provided by a long‐lasting diffusion, thereby implying a more efficient transport (i.e., advective transport through faults). He data coupled to heat‐He relationship suggest the occurrence of active degassing of magmatic intrusions in this area of continental collisional. Geophysical data indicate the presence of a hot mantle wedge below the outgassing of mantle volatiles and a system of faults cutting the continental crust down to the hot mantle wedge. Here we discuss the hot mantle wedge and possible associated magmatic intrusions as the source of the mantle‐derived volatiles outgassing in the region. We also assessed the output of mantle‐derived CO <sub>2</sub> from the investigated hydrothermal basins. The possible occurrence of magma at depth as well as the geometry of the thick‐skinned deformed wedge unambiguously indicates delamination processes that are related to continental subduction. Hence, we show that delamination processes can really produce magma at depth without evidences of volcanism at the surface. Finally, we have also provided the fault systems that work as a network of pathways and actively sustain the advective transfer of the mantle fluids toward the surface. </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> > 在这项研究中，我们讨论了披露的热和挥发物的发生（即氦气和CO <sub> 2 </ sub> ）在两个会聚板（非洲和欧洲）之间的地震活动边缘中喂养水热系统，没有任何火山的信号。氦（He）同位素清楚地表明除了除气挥发物中的披风衍生的组分。估计的地幔衍生的HE助熔剂高于稳定的大陆区域中的尺寸高达两到三个数量级。这种高的He助熔剂不能通过长持久的扩散来提供，从而暗示更有效的运输（即，通过故障的平流运输）。他的数据耦合到热统治关系表明，在大陆碰撞的这一领域的岩浆入侵的活跃脱气的发生。地球物理数据表明，低于地幔挥发物的排出的热部队楔形的存在和将大陆外壳切割到热幔楔的故障系统。在这里，我们讨论了热的地幔楔和可能的岩石侵入性，作为该区域的披风衍生挥发物的来源。我们还评估了地幔衍生的CO的产量 <sub> 2 </ sub> 从研究的水热盆地。深度可能发生的岩浆以及厚皮的变形楔的几何形状明确表示与大陆俯冲有关的分层过程。因此，我们表明分层过程可以在深度中真正生产岩浆，而不会在表面上的火山证据。最后，我们还提供了作为途径网络的故障系统，并积极地维持地幔流体对表面的平移转移。 </ 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14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=Caracausi Antonio&option=202" target="_blank" rel="nofollow">Caracausi Antonio;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sulli Attilio&option=202" target="_blank" rel="nofollow">Sulli Attilio;</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>Istituto Nazionale di Geofisica e VulcanologiaPalermo Italy;</p> <p>Dipartimento di Scienze della Terra e del MareUniversità di PalermoPalermo Italy;</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 volatiles&option=203" rel="nofollow">mantle volatiles;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=helium&option=203" rel="nofollow">helium;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=output CO 2&option=203" rel="nofollow">output CO 2;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=delamination&option=203" rel="nofollow">delamination;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=mantle wedge&option=203" rel="nofollow">mantle wedge;</a> </p> <div class="translation"> 机译：地幔挥发物;氦气;产量CO 2;分层;地幔楔形; 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