Spatially Variable        <fc >CO</fc>CO        <sub >2</sub>2        Degassing in the Main Ethiopian Rift: Implications for Magma Storage, Volatile Transport, and Rift‐Related Emissions

Hunt Jonathan A.; Zafu Amdemichael; Mather Tamsin A.; Pyle David M.; Barry Peter H.

摘要

Abstract > Deep carbon emissions from historically inactive volcanoes, hydrothermal, and tectonic structures are among the greatest unknowns in the long‐term (～Myr) carbon cycle. Recent estimates of diffuse CO <sub>2</sub> flux from the Eastern Rift of the East African Rift System (EARS) suggest this could equal emissions from the entire mid‐ocean ridge system. We report new CO <sub>2</sub> surveys from the Main Ethiopian Rift (MER, northernmost EARS), and reassess the rift‐related CO <sub>2</sub> flux. Since degassing in the MER is concentrated in discrete areas of volcanic and off‐edifice activity, characterization of such areas is important for extrapolation to a rift‐scale budget. Locations of hot springs and fumaroles along the rift show numerous geothermal areas away from volcanic edifices. With these new data, we estimate total CO <sub>2</sub> emissions from the central and northern MER as 0.52–4.36 Mt?yr ?1 . Our extrapolated flux from the Eastern Rift is 3.9–32.7 Mt?yr ?1 CO <sub>2</sub> , overlapping with lower end of the range presented in recent estimates. By scaling, we suggest that 6–18 Mt?yr ?1 CO <sub>2</sub> flux can be accounted for by magmatic extension, which implies an important role for volatile‐enriched lithosphere, crustal assimilation, and/or additional magmatic intrusion to account for the upper range of flux estimates. Our results also have implications for the nature of volcanism in the MER. Many geothermal areas are found 10 km from the nearest volcanic center, suggesting ongoing hazards associated with regional volcanism. </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> > 来自历史无活性的火山，水热和构造结构的深度碳排放是长期（MYR）碳循环中最大的未知数。最近的弥漫性有限公司估计 <sub> 2 </ sub> 来自东非裂谷系统的东部裂缝（耳朵）的助焊剂表明这可以等于整个中海山脊系统的排放量。我们报告新的CO <sub> 2 </ sub> 从埃塞俄比亚主要裂口（MER，最眠耳）的调查，并重新评估裂谷相关的CO <sub> 2 </ sub> 助焊剂。由于MER中的脱气集中在火山和偏美活动的离散区域中，因此这些区域的表征对于推断到裂缝规模预算是重要的。沿着裂谷的热弹簧和富马摩尔的地点显示出众多远离火山的地热区域。通过这些新数据，我们估计总有限公司 <sub> 2 </ sub> 中央和北方的排放为0.52-4.36 mt？YR ？1 </ sup> 。我们来自东部裂谷的外推通量是3.9-32.7 mt？？1 </ sup> CO. <sub> 2 </ sub> ，与最近估计中呈现的范围的下端重叠。通过缩放，我们建议6-18吨？是？1 </ sup> CO. <sub> 2 </ sub> 磁共振延伸可以占磁悬浮局部，这意味着富含挥发性的岩石圈，地壳同化和/或额外的岩石侵入的重要作用，以考虑助焊剂估计的上限。我们的结果也对MER中的火山主义性质产生了影响。找到许多地热区域＆距离最近的火山中心10公里，表明与区域火山有关的持续危险。 </ 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24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=Hunt Jonathan A.&option=202" target="_blank" rel="nofollow">Hunt Jonathan A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zafu Amdemichael&option=202" target="_blank" rel="nofollow">Zafu Amdemichael;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mather Tamsin A.&option=202" target="_blank" rel="nofollow">Mather Tamsin A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pyle David M.&option=202" target="_blank" rel="nofollow">Pyle David M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Barry Peter H.&option=202" target="_blank" rel="nofollow">Barry Peter H.;</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 SciencesUniversity of OxfordOxford UK;</p> <p>School of Earth SciencesAddis Ababa UniversityAddis Ababa Ethiopia;</p> <p>Department of Earth SciencesUniversity of OxfordOxford UK;</p> <p>Department of Earth SciencesUniversity of OxfordOxford UK;</p> <p>Department of Earth SciencesUniversity of OxfordOxford UK;</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=carbon dioxide&option=203" rel="nofollow">carbon dioxide;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=degassing&option=203" rel="nofollow">degassing;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=geothermal&option=203" rel="nofollow">geothermal;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Main Ethiopian Rift&option=203" rel="nofollow">Main Ethiopian Rift;</a> </p> <div class="translation"> 机译：二氧化碳;脱气;地热;主要埃塞俄比亚裂痕; 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Spatially Variable COCO 22 Degassing in the Main Ethiopian Rift: Implications for Magma Storage, Volatile Transport, and Rift‐Related Emissions

摘要

Spatially Variable COCO ₂2 Degassing in the Main Ethiopian Rift: Implications for Magma Storage, Volatile Transport, and Rift‐Related Emissions