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Geology and Fluid Discharge at Dorado Outcrop, a Low Temperature Ridge‐Flank Hydrothermal System

机译:Dorado露头的地质和流体放电,低温脊侧水热系统

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Abstract > Two expeditions to Dorado Outcrop on the eastern flank of the East Pacific Rise and west of the Middle America Trench collected images, video, rocks, and sediment samples and measured temperature and fluid discharge rates to document the physical and biogeochemical characteristics of a regional, low‐temperature (~15?°C) hydrothermal system. Analysis of video and images identified lava morphologies: pillow, lobate, and sheet flows. Glasses from collected lavas were consistent with an off‐axis formation. Hydrothermal discharge generally occurs through pillow lavas but is patchy, sporadic, and sometimes ceases at particular sites of discharge. Yearlong temperature measurements at five of these discharge sites show daily ranges that oscillate with tidal frequencies by 6?°C or more. Instantaneous fluid discharge rates (0.16 to 0.19?L/s) were determined resulting in a calculated discharge of ~200?L/s when integrated over the area defined by the most robust fluid discharge. Such discharge has a power output of 10–12?MW. Hydrothermal seepage through thin sediment adjacent to the outcrop accounts for 3% of this discharge, but seepage may support an oxic sediment column. High extractable Mn concentrations and depleted δ 13 C in the low but variable organic solid phase suggest that hydrothermal fluids provide a source for manganese accumulation and likely enhance the oxidation of organic carbon. Comparisons of the physical and geochemical characteristics at Dorado and Baby Bare Outcrops, the latter being the only other site of ridge‐flank hydrothermal discharge that has been sampled directly, suggest commonalities and differences that have implications for future discoveries. </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> > 两次探险在东太平洋东部侧翼和中西部的东侧露头的探险队收集了图像,视频,岩石和沉积物样品,并测量了温度和流体放电率,以记录区域,低的物理和生物地球化学特征 - 温度(〜15°C)水热系统。视频和图像分析确定了熔岩形态:枕头,裂片和薄片流。来自收集的熔岩的眼镜与轴外形成一致。水热量放电一般通过枕头熔岩发生,但是斑驳,散发性,有时在特定的放电部位停止。这些放电场所五年的长期温度测量显示每天的范围,振荡频率6?°C或更多。确定瞬时流体放电速率(0.16至0.19〜L / s),导致在通过最强大的流体放电定义的区域上集成时的〜200μl/ s的计算排出。这种放电的功率输出为10-12?MW。通过邻近露头的薄沉积物的水热渗流涉及该放电的3%,但渗流可支持氧沉积柱。高萃取的Mn浓度和耗尽δ 13 </ sup> C在低但可变的有机固相中表明,水热流体提供了锰累积的源,并且可能增强有机碳的氧化。 Dorado和Baby Bare露头的物理和地球化学特征的比较,后者是刚刚被直接取样的山脊水热量放电的其他网站,建议对未来发现有影响的共同性和差异。 </ 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1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=Wheat C. Geoffrey&option=202" target="_blank" rel="nofollow">Wheat C. Geoffrey;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hartwell Anne M.&option=202" target="_blank" rel="nofollow">Hartwell Anne M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=McManus James&option=202" target="_blank" rel="nofollow">McManus James;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fisher Andrew T.&option=202" target="_blank" rel="nofollow">Fisher Andrew T.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Orcutt Beth N.&option=202" target="_blank" rel="nofollow">Orcutt Beth N.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Schlicht Lucy E. M.&option=202" target="_blank" rel="nofollow">Schlicht Lucy E. M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Niedenzu Sara&option=202" target="_blank" rel="nofollow">Niedenzu Sara;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bach Wolfgang&option=202" target="_blank" rel="nofollow">Bach Wolfgang;</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 of Marine ScienceUniversity of Alaska FairbanksMoss Landing CA USA;</p> <p>Institute of Marine ScienceUniversity of Alaska FairbanksMoss Landing CA USA;</p> <p>Bigelow Laboratory for Ocean SciencesEast Boothbay ME USA;</p> <p>Earth and Planetary Sciences DepartmentUniversity of CaliforniaSanta Cruz CA USA;</p> <p>Bigelow Laboratory for Ocean SciencesEast Boothbay ME USA;</p> <p>Department of Geosciences and MARUM‐Center for Marine Environmental SciencesUniversity of BremenBremen Germany;</p> <p>Department of Geosciences and MARUM‐Center for Marine Environmental SciencesUniversity of BremenBremen Germany;</p> <p>Department of Geosciences and MARUM‐Center for Marine Environmental SciencesUniversity of BremenBremen Germany;</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=ridge flank&option=203" rel="nofollow">ridge flank;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dorado Outcrop&option=203" rel="nofollow">Dorado Outcrop;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=seafloor geology&option=203" rel="nofollow">seafloor geology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=hydrothermal&option=203" rel="nofollow">hydrothermal;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=fluid discharge&option=203" rel="nofollow">fluid discharge;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sediment&option=203" rel="nofollow">sediment;</a> </p> <div class="translation"> 机译:脊侧;Dorado露头;海底地质;水热;流体放电;沉积物; </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/0704023360526.html">Geology and Fluid Discharge at Dorado Outcrop, a Low Temperature Ridge‐Flank Hydrothermal System</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wheat C. 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