Development of push moraines in deeply frozen sediment adjacent to a cold‐based glacier in the McMurdo Dry Valleys, Antarctica

机译：南极洲McMurdo Dryalys冷藏冰川邻近的深冷沉积物在深冷泥沙的发展

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Abstract > Previous studies of push moraines have concluded that structural architecture is controlled by a combination of stress exerted by flowing ice and the rheology of the deforming sediment. However, the relationship between deformation processes and the thermal/hydrologic conditions within the sediment remains ambiguous. Using a combination of surface mapping, logging exposures and ground penetrating radar we examine the relationships between surface morphology, material properties and development of deformation structures in deeply frozen sediment that has been deformed by Joyce Glacier, a cold‐based glacier in the McMurdo Dry Valleys. The structural architecture of the push moraines is characterized by a combination of brittle and ductile deformation structures that have produced a structurally complex pattern of thrust faults, low angle listric thrusts and recumbent folds that extend 400?m beyond the glacier margin. Deformation is ductile where the ice concentration exceeds c . 65% volume and predominantly brittle where the ice concentration is less than c . 65%. The change in rheology reflects transition in behaviour from the material having a predominantly frictional character when the ice is limited to pore spaces to a non‐frictional character in which strength is primarily determined by the cohesive strength of the ice. This work shows that glaciotectonic deformation can occur in deeply frozen permafrost where there is no liquid pore water. We conclude that the presence of liquid porewater is not a necessary condition for the development of glaciotectonic deformation or for the formation of push moraines. ? 2019 John Wiley & Sons, Ltd. </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> > 以前的推动冰莴苣的研究得出结论，结构架构通过流动冰和变形沉积物的流变来控制结构架构。然而，变形过程与沉积物内的热/水文条件之间的关系仍然存在含糊不清。使用表面映射的组合，测井曝光和地面穿透雷达，我们研究了在深深的冷冻沉积物中的表面形态，材料特性和变形结构的发展之间的关系，这是由McMurdo Dryalys中的冷冰川变形的深深冻结沉积物。推动冰片的结构架构的特征在于脆性和延展性变形结构的组合，所述脆性和延展性变形结构产生了结构复杂的推力故障，低角度列出的推力和斜面折叠，其延伸超过冰川边缘。变形是粘液超过的延性 c </ i> 。 65％的体积，主要是冰浓度小于的脆性 c </ i> 。 65％。流变术的变化反映了当冰限于孔隙空间到非摩擦性特征的主要摩擦特性的材料中的行为转变，其中强度主要由冰的粘性强度决定。这项工作表明，在深度冷冻的永久冻土中可能发生冰川癖变形，其中没有液体孔隙水。我们得出结论，液体沉积物的存在不是发育恐怖症变形的必要条件或用于形成推性衣原体。还2019年John Wiley＆amp; SONS，LTD. </ 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-22319/'>《Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group》</a> <b style="margin: 0 2px;">|</b><span>2020年第3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=Fitzsimons Sean&option=202" target="_blank" rel="nofollow">Fitzsimons Sean;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Howarth Jamie&option=202" target="_blank" rel="nofollow">Howarth Jamie;</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>School of Geography Te IhowhenuaUniversity of OtagoDunedin New Zealand;</p> <p>School of Geography Geology and Environmental ScienceVictoria University of WellingtonNew Zealand;</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=glacitectonic deformation&option=203" rel="nofollow">glacitectonic deformation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=push moraines&option=203" rel="nofollow">push moraines;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=thrust block moraines&option=203" rel="nofollow">thrust block moraines;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=deformation of permafrost&option=203" rel="nofollow">deformation of permafrost;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=cold‐based glacier&option=203" rel="nofollow">cold‐based glacier;</a> </p> <div class="translation"> 机译：盖架凝视变形;推乱性;推力阻塞冰片;永久冻土的变形;冷冰川; </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/0704023138787.html">Development of push moraines in deeply frozen sediment adjacent to a cold‐based glacier in the McMurdo Dry Valleys, Antarctica</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fitzsimons Sean&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Fitzsimons Sean,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Howarth Jamie&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Howarth Jamie </a> <a href="/journal-foreign-22319/" target="_blank" rel="nofollow" class="tuijian_authcolor">Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group .</a> <span>2020</span><span>,第3期</span> </span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：南极洲McMurdo Dryalys冷藏冰川邻近的深冷沉积物在深冷泥沙的发展</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-foreign_detail_thesis/0204119499100.html">Draft Genome Sequence of Paenisporosarcina sp. 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