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Hydrothermal Venting at Hinepuia Submarine Volcano, Kermadec Arc: Understanding Magmatic‐Hydrothermal Fluid Chemistry

机译：Hinepuia潜艇火山的水热通风，Kermadec Arc：了解岩浆 - 水热流体化学

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Abstract > The Hinepuia volcanic center is made up of two distinct edifices aligned northwest to southeast, with an active cone complex in the SE. Hinepuia is one of several active volcanoes in the northern segment of the Kermadec arc. Regional magnetic data show no evidence for large‐scale hydrothermal alteration at Hinepuia, yet plume data confirm present‐day hydrothermal discharge, suggesting that the hydrothermal system may be too young to have altered the host rocks with respect to measurable changes in magnetic signal. Gravity data are consistent with crustal thinning and shallow mantle under the volcanic center. Following the discovery of hydrothermal plumes over Hinepuia, the submersible Shinkai 6500 was used to explore the SE cone and sample hydrothermal fluids. The chemistry of hydrothermal fluids from submarine arc and backarc volcanoes is typically dominated by water‐rock interactions and/or magmatic degassing. Chemical analyses of vent fluids show that Hinepuia does not quite fit either traditional model. Moreover, the Hinepuia samples fall between those typically ascribed to both end‐member fluid types when plotted on a K‐Mg‐SO <sub>4</sub> ternary diagram. Due to evidence of strong degassing, abundant native sulfur deposition, and H <sub>2</sub> S presence, the vent sampled at Hinepuia is ultimately classified as a magmatic‐hydrothermal system with a water‐rock influence. This vent is releasing water vapor and magmatic volatiles with a notable lack of salinity due to subcritical boiling and phase separation. Magmatic‐hydrothermal fluid chemistry appears to be controlled by a combination of gas flux, phase separation processes, and volcano evolution and/or distance from the magma source. </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> > Hinepuia火山中心由两种不同的果实组成，在西北地区对齐，在SE中有一个活跃的锥形综合体。 Hinepuia是Kermadec弧北部的几座活性火山之一。区域磁性数据显示亨弥敦的大规模水热改变的证据，但羽流数据确认当前的水热量放电，表明水热系统可能太小而无法改变磁信号的可测量变化的主体岩石。重力数据与火山中心下的地壳变薄和浅层罩一致。在发现水热羽毛上，潜水 shinkai 6500 </ i> 用于探索SE锥和样品热流体。来自潜水弧和后弧火山的水热流体的化学通常由水岩相互作用和/或岩浆脱气为主。排气流体的化学分析表明，Hinepuia不太适合传统模式。此外，当绘制在K-MG-SO上时，Hinepuia样品落在通常均匀均匀的那些。 <sub> 4 </ sub> 三元图。由于证据具有强烈脱气，富含原生硫沉积和H. <sub> 2 </ sub> 在Hinepuia上采样的通风口最终被归类为具有水岩体影响的岩浆水热系统。由于亚临界沸腾和相分离，该通风口释放水蒸气和岩浆挥发物，具有显着的缺乏盐度。岩浆 - 水热流体化学似乎通过气体通量，相分离过程和火山进化和/或距岩浆源的距离来控制。 </ 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10期</span><b style="margin: 0 2px;">|</b><span>共16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=Stucker Valerie K.&option=202" target="_blank" rel="nofollow">Stucker Valerie K.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Walker Sharon L.&option=202" target="_blank" rel="nofollow">Walker Sharon L.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=de Ronde Cornel E. J.&option=202" target="_blank" rel="nofollow">de Ronde Cornel E. J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Caratori Tontini Fabio&option=202" target="_blank" rel="nofollow">Caratori Tontini Fabio;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tsuchida Shinji&option=202" target="_blank" rel="nofollow">Tsuchida Shinji;</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>Marine Geosciences GNS ScienceLower Hutt New Zealand;</p> <p>National Oceanic and Atmospheric Administration Pacific Marine Environmental LaboratorySeattle WA USA;</p> <p>Marine Geosciences GNS ScienceLower Hutt New Zealand;</p> <p>Marine Geosciences GNS ScienceLower Hutt New Zealand;</p> <p>Japan Agency for Marine‐Earth Science and TechnologyYokosuka Japan;</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=Hinepuia volcanic center&option=203" rel="nofollow">Hinepuia volcanic center;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=water‐rock interactions&option=203" rel="nofollow">water‐rock interactions;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=magmatic‐hydrothermal systems&option=203" rel="nofollow">magmatic‐hydrothermal systems;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kermadec arc&option=203" rel="nofollow">Kermadec arc;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ternary diagram&option=203" rel="nofollow">ternary diagram;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=end‐member fluids&option=203" rel="nofollow">end‐member fluids;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Shinkai 6500 submersible&option=203" rel="nofollow">Shinkai 6500 submersible;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=phase separation&option=203" rel="nofollow">phase separation;</a> </p> <div class="translation"> 机译：Hinepuia火山中心;水岩相互作用;岩浆 - 水热系统;Kermadec弧;三元图;末端成员流体;Shinkai 6500潜水;相分离; </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/0704023360502.html">Hydrothermal Venting at Hinepuia Submarine Volcano, Kermadec Arc: Understanding Magmatic‐Hydrothermal Fluid Chemistry</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Stucker Valerie K.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Stucker Valerie K.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Walker Sharon L.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Walker Sharon L.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=de Ronde Cornel E. 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