Lower Crustal Strength Controls on Melting and Serpentinization at Magma‐Poor Margins: Potential Implications for the South Atlantic

Ros Elena; Pérez‐Gussinyé Marta; Araújo Mario; Thoaldo Romeiro Marco; Andrés‐Martínez Miguel; Morgan Jason P.

摘要

Abstract >Rifted continental margins may present a predominantly magmatic continent‐ocean transition (COT), or one characterized by large exposures of serpentinized mantle. In this study we use numerical modeling to show the importance of the lower crustal strength in controlling the amount and onset of melting and serpentinization during rifting. We propose that the relative timing between both events controls the nature of the COT. Numerical experiments for half‐extension velocities =10 mm/yr suggest there is a genetic link between margin tectonic style and COT nature that strongly depends on the lower crustal strength. Our results imply that very slow extension velocities ( 5 mm/yr) and a strong lower crust lead to margins characterized by large oceanward dipping faults, strong syn‐rift subsidence and abrupt crustal tapering beneath the continental shelf. These margins can be either narrow symmetric or asymmetric and present a COT with exhumed serpentinized mantle underlain by some magmatic products. In contrast, a weak lower crust promotes margins with a gentle crustal tapering, small faults dipping both ocean‐ and landward and small syn‐rift subsidence. Their COT is predominantly magmatic at any ultra‐slow extension velocity and perhaps underlain by some serpentinized mantle. These margins can also be either symmetric or asymmetric. Our models predict that magmatic underplating mostly underlies the wide margin at weak asymmetric conjugates, whereas the wide margin is mainly underlain by serpentinized mantle at strong asymmetric margins. Based on this conceptual template, we propose different natures for the COTs in the South Atlantic. </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> >裂缝的大陆边缘可能出现主要的岩浆大陆 - 海洋转型（婴儿床），或者一种以蛇形的锯齿的大暴露为特征。在这项研究中，我们使用数值模拟来表明在河流期间控制熔融和蛇形化的量和发作较低的地壳强度的重要性。我们建议两种事件之间的相对时间控制婴儿床的性质。半延伸速度的数值实验＆ = 10 mm / yr表明，边缘构造风格和婴儿床之间存在遗传联系，强烈取决于地壳强度较低。我们的结果意味着延长速度非常慢的延长速度（＆ 5 mm / yr）和强大的下地壳导致利润率，以巨大的海洋倾斜故障，强大的裂缝沉降和大陆架下方的地壳逐渐变细。这些边缘可以是狭窄的对称或不对称，并且通过一些岩浆产品展示了一个带有膨胀的蛇纹石的搭桥的婴儿床。相比之下，弱低地壳促使利润率温和的地壳逐渐变细，小故障浸泡了海洋和陆地和小的同步沉降。他们的婴儿床主要在任何超低延长速度下晃动，也许是一些蛇形的地幔的下层。这些边缘也可以是对称的或不对称的。我们的模型预测，岩石底层大部分地下层宽阔的不对称缀合物的宽边缘，而宽边缘主要受到强烈的不对称利润率的蛇形地幔。基于这种概念模板，我们为南大西洋的婴儿床提出了不同的自然。</ 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12期</span><b style="margin: 0 2px;">|</b><span>共20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=Ros Elena&option=202" target="_blank" rel="nofollow">Ros Elena;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pérez‐Gussinyé Marta&option=202" target="_blank" rel="nofollow">Pérez‐Gussinyé Marta;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Araújo Mario&option=202" target="_blank" rel="nofollow">Araújo Mario;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Thoaldo Romeiro Marco&option=202" target="_blank" rel="nofollow">Thoaldo Romeiro Marco;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Andrés‐Martínez Miguel&option=202" target="_blank" rel="nofollow">Andrés‐Martínez Miguel;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Morgan Jason P.&option=202" target="_blank" rel="nofollow">Morgan Jason P.;</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>COMPASS Department of Earth SciencesRoyal Holloway University of LondonEgham UK;</p> <p>MARUM – Center for Marine Environmental Sciences University of BremenGermany;</p> <p>Petrobras R&</p> <p>D CenterHorácio Macedo Avenue 950 Rio de Janeiro Brazil;</p> <p>Petrobras R&</p> <p>D CenterHorácio Macedo Avenue 950 Rio de Janeiro Brazil;</p> <p>MARUM – Center for Marine Environmental Sciences University of BremenGermany;</p> <p>COMPASS Department of Earth SciencesRoyal Holloway University of LondonEgham 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=continent‐ocean transition&option=203" rel="nofollow">continent‐ocean transition;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=serpentinization&option=203" rel="nofollow">serpentinization;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=melting&option=203" rel="nofollow">melting;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=continental rifting&option=203" rel="nofollow">continental rifting;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=geodynamic modeling&option=203" rel="nofollow">geodynamic modeling;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=magma‐poor margins of South Atlantic&option=203" rel="nofollow">magma‐poor margins of South Atlantic;</a> </p> <div class="translation"> 机译：大陆 - 海洋过渡;蛇形化;熔化;大陆河流;地球动力学造型;南大西洋的岩浆利润率差; </div> </li> </ul> </div> </div> <div class="literature cardcommon"> <div class="similarity "> <h3 class="all_title" id="enpatent66">相似文献</h3> <div 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