首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Concentrated, ‘pulsed’ axial glacier flow: structural glaciological evidence from Kvíárj?kull in SE Iceland
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Concentrated, ‘pulsed’ axial glacier flow: structural glaciological evidence from Kvíárj?kull in SE Iceland

机译:集中,'脉冲'轴向冰川流动:来自Kvíárj的结构冰川癖证据?克尔在冰岛

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Abstract > A detailed structural glaciological study carried out on Kvíárj?kull in SE Iceland reveals that recent flow within this maritime glacier is concentrated within a narrow corridor located along its central axis. This active corridor is responsible for feeding ice from the accumulation zone on the south‐eastern side of ?r?faj?kull to the lower reaches of the glacier and resulted in a c . 200 m advance during the winter of 2013–2014 and the formation of a push‐moraine. The corridor comprises a series of lobes linked by a laterally continuous zone of highly fractured ice characterised by prominent flow‐parallel crevasses, separated by shear zones. The lobes form highly crevassed topographic highs on the glacier surface and occur immediately down‐ice of marked constrictions caused by prominent bedrock outcrops located on the northern side of the glacier. Close to the frontal margin of Kvíárj?kull, the southern side of the glacier is relatively smooth and pock‐marked by a number of large moulins. The boundary between this slow moving ice and the active corridor is marked by a number of ice flow‐parallel strike‐slip faults and a prominent dextral shear zone which resulted in the clockwise rotation and dissection of an ice‐cored esker exposed on the glacier surface. It is suggested that this concentrated style of glacier flow identified within Kvíárj?kull has affinities with the individual flow units which operate within pulsing or surging glaciers. ? 2017 The Authors Earth Surface Processes and Landforms ? 2017 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 XMLNS =“http://www.wiley.com/namespaces/wiley”type =“main”> <title type =“main”>抽象</ title> >在Kvíárj进行详细的结构冰川学习在SE冰岛的Kull揭示了该海上冰川内的最近流动集中在沿着其中心轴的狭窄走廊内。这种活跃的走廊负责从冰川向东侧的积聚区喂养冰?kull到冰川的下游,导致 c </ i>。 2013 - 2014年冬季200米提前,并形成了一个推动冰碛。走廊包括一系列由由高度裂缝冰的横向连续区域连接的裂片,其特征在于突出的流动平行的裂隙,由剪切区分离。裂片在冰川表面上形成高度裂隙的地形高度,并立即发生由位于冰川北侧的突出基岩露头引起的标记收缩的下冰。靠近kvíárj的正边缘?kull,冰川的南侧相对光滑,斑纹标记着许多大型麦粉。这种缓慢移动的冰和有源走廊之间的边界标有许多冰流平行的滑动故障和突出的射击区域,导致冰川表面上暴露的冰芯ESKER的顺时针旋转和解剖。建议在Kvíárj中鉴定出这种浓缩的冰川流动风格,kull在脉冲或汹涌的冰川内运行的各个流动单元具有亲和力。还2017年作者地球表面流程和地貌? 2017年John Wiley&amp; SONS,LTD。</ p> </ abstract> </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>2017年第13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=Phillips Emrys&option=202" target="_blank" rel="nofollow">Phillips Emrys;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Everest Jez&option=202" target="_blank" rel="nofollow">Everest Jez;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Evans David J.A.&option=202" target="_blank" rel="nofollow">Evans David J.A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Finlayson Andrew&option=202" target="_blank" rel="nofollow">Finlayson Andrew;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ewertowski Marek&option=202" target="_blank" rel="nofollow">Ewertowski Marek;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Guild Ailsa&option=202" target="_blank" rel="nofollow">Guild Ailsa;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jones Lee&option=202" target="_blank" rel="nofollow">Jones Lee;</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>British Geological SurveyThe Lyell CentreResearch Avenue South Edinburgh EH14 4AP;</p> <p>British Geological SurveyThe Lyell CentreResearch Avenue South Edinburgh EH14 4AP;</p> <p>Department of GeographyDurham UniversitySouth Road Durham DH1 3LE;</p> <p>British Geological SurveyThe Lyell CentreResearch Avenue South Edinburgh EH14 4AP;</p> <p>Department of GeographyDurham UniversitySouth Road Durham DH1 3LE;</p> <p>British Geological SurveyThe Lyell CentreResearch Avenue South Edinburgh EH14 4AP;</p> <p>British Geological SurveyKeyworth Nottingham NG12 5GG 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=structural glaciology&option=203" rel="nofollow">structural glaciology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=concentrated axial glacier flow&option=203" rel="nofollow">concentrated axial glacier flow;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=pulse surge‐like behaviour&option=203" rel="nofollow">pulse surge‐like behaviour;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kvíárj?kull&option=203" rel="nofollow">Kvíárj?kull;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=SE Iceland&option=203" rel="nofollow">SE Iceland;</a> </p> <div class="translation"> 机译:结构冰川;集中轴向冰川流动;脉冲浪涌的行为;kvíárj?kull;se冰岛; 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