Distinctive Seafloor Fabric Produced Near Western Versus Eastern Ridge‐Transform Intersections of the Northern Mid‐Atlantic Ridge: Possible Influence of Ridge Migration

Cormier Marie‐Helene; Sloan Heather

摘要

Abstract >Multibeam bathymetry compiled along fracture zones of the northern Atlantic reveals a striking morphological asymmetry. Seafloor fabric produced at western ridge‐transform intersections (RTIs) tends to consist of linear ridges, small in amplitude, and regularly spaced, and oceanic core complexes (OCCs) occur infrequently. In contrast, seafloor fabric produced at eastern RTIs is more irregular and blocky and displays characteristics usually associated with melt‐poor accretion: These include more than double the occurrence of OCCs as well as greater seafloor depths, even where seafloor is younger than that on the opposite side of the fracture zone. We propose that this asymmetry is a consequence of the westward migration of the Mid‐Atlantic Ridge. Such migration is expected to result in an enhanced melt supply at leading (western) RTIs compared to trailing (eastern) RTIs. The morphological asymmetry is observed for ridge offsets of ~40 to ~200?km, a range that may be related to the width of melting regimes that supply ridge segments. At slow spreading ridges, contrasting melt supplies across fracture zones may therefore be best expressed in the distinct seafloor fabrics preserved beyond the dynamically maintained relief of the axial rift valley and walls rather than in the contrasting axial depths documented for faster spreading ridges. Although OCCs appear to form preferentially at spreading rates lower than 30?mm/year, their common occurrence along the northern Mid‐Atlantic Ridge may also reflect the significantly higher rates at which it is migrating compared to the southern Mid‐Atlantic Ridge. </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> 沿着北大西洋骨折地区编制的多沟沐浴物揭示了一种引人注目的形态不对称。西脊 - 变换交叉点（RTIS）生产的海底织物倾向于由线性脊，较小的幅度和定期间隔组成，并且海洋核心复合物（OCCS）不经常发生。相比之下，在东部RTIS产生的海底织物更不规则和障碍，并且显示器通常与熔体增生相关的特性：这些包括多次出现OCC的发生以及更大的海底深度，即使是海底较年轻的那么较大骨折区的另一侧。我们建议这种不对称是中大西洋脊的向西迁移的结果。与尾随（东部）RTIS相比，这种迁移预计将导致领先（Western）RTIS的增强熔体供应。对于〜40至200Ωkm的脊偏移观察到形态不对称，可以与供应脊段供应熔融制度的宽度有关的范围。在慢速扩散脊上，横跨裂缝区域的对比熔体供应可以最好地表达在超出动态保持轴向谷和壁的动态维持的浮雕的不同海底织物中，而不是在记录的对比轴向深度以更快地扩散脊。虽然OCCS似乎优先形成低于30？MM /年的扩散率，但它们沿着北部山脊的常见发生也可能反映了与南部大西洋脊相比迁移的显着提高速率。</ 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22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=Cormier Marie‐Helene&option=202" target="_blank" rel="nofollow">Cormier Marie‐Helene;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sloan Heather&option=202" target="_blank" rel="nofollow">Sloan Heather;</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>Graduate School of OceanographyUniversity of Rhode IslandNarragansett RI USA;</p> <p>Department of Earth Environmental and Geospatial Sciences Lehman CollegeCity University of New YorkNew York NY USA;</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=Mid‐Atlantic Ridge&option=203" rel="nofollow">Mid‐Atlantic Ridge;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=seafloor morphology&option=203" rel="nofollow">seafloor morphology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=oceanic core complex&option=203" rel="nofollow">oceanic core complex;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ridge migration&option=203" rel="nofollow">ridge migration;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=fracture zone&option=203" rel="nofollow">fracture zone;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=transform fault&option=203" rel="nofollow">transform fault;</a> </p> <div class="translation"> 机译：中大西洋脊;海底形态;海洋核心复合体;脊迁移;骨折区;变换故障; 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