Deformation of the Pacific/North America Plate Boundary at Queen Charlotte Fault: The Possible Role of Rheology

机译：女王夏洛特故障的太平洋/北美板材边界的变形：流变学的作用

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Abstract >The Pacific/North America (PA/NA) plate boundary between Vancouver Island and Alaska is similar to the PA/NA boundary in California in its kinematic history and the rate and azimuth of current relative motion, yet their deformation styles are distinct. The California plate boundary shows a broad zone of parallel strike slip and thrust faults and folds, whereas the 49‐mm/yr PA/NA relative plate motion in Canada and Alaska is centered on a single, narrow, continuous ~900‐km‐long fault, the Queen Charlotte Fault (QCF). Using gravity analysis, we propose that this plate boundary is centered on the continent/ocean boundary (COB), an unusual location for continental transform faults because plate boundaries typically localize within the continental lithosphere, which is weaker. Because the COB is a boundary between materials of contrasting elastic properties, once a fault is established there, it will probably remain stable. We propose that deformation progressively shifted to the COB in the wake of Yakutat terrane's northward motion along the margin. Minor convergence across the plate boundary is probably accommodated by fault reactivation on Pacific crust and by an eastward dipping QCF. Underthrusting of Pacific slab under Haida Gwaii occurs at convergence angles >14°–15° and may have been responsible for the emergence of the archipelago. The calculated slab entry dip (5°–8°) suggests that the slab probably does not extend into the asthenosphere. The PA/NA plate boundary at the QCF can serve as a structurally simple site to investigate the impact of rheology and composition on crustal deformation and the initiation of slab underthrusting. </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> >温哥华岛和阿拉斯加之间的太平洋/北美（PA / NA）板边界是相似的在加利福尼亚州的PA / NA边界，在其运动历史和当前相对运动的速率和方位角，但它们的变形样式是截然不同的。加州板边界显示了一块平行撞击滑动和推力故障和褶皱的宽带，而加拿大和阿拉斯加的49毫米/ yr pa / na相对板运动以单一，窄，连续〜900公里长故障，女王夏洛特故障（QCF）。使用重力分析，我们建议将该板材边界以大陆/海洋边界（COB）为中心，这是欧陆变换故障的不寻常位置，因为板边界通常在大陆岩石圈内定位，这较弱。因为玉米棒是对比弹性特性的材料之间的边界，一旦在那里建立了故障，它就可能保持稳定。我们建议在雅库特地区沿着边缘的北方运动之后逐渐转向玉米棒。在太平洋地壳上的故障再激活和东方浸渍QCF时，横跨板边界的轻微收敛可能会被容纳。在Haida Gwaii下的太平洋平板削弱在收敛角下发生> 14°-15°，并且可能对群岛的出现负责。计算的平板条目浸渍（5°-8°）表明板坯可能不会延伸到哮喘圈。 QCF的PA / Na板边界可以用作结构简单的部位，以研究流变学和组成对地壳变形的影响以及板坯的启动。</ 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-34677/'>《Journal of geophysical research. Solid earth: JGR》</a> <b style="margin: 0 2px;">|</b><span>2018年第5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=Brink U. S.&option=202" target="_blank" rel="nofollow">Brink U. S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Miller N. C.&option=202" target="_blank" rel="nofollow">Miller N. C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Andrews B. D.&option=202" target="_blank" rel="nofollow">Andrews B. D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Brothers D. S.&option=202" target="_blank" rel="nofollow">Brothers D. S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Haeussler P. J.&option=202" target="_blank" rel="nofollow">Haeussler P. J.;</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>U.S. Geological SurveyWoods Hole MA USA;</p> <p>U.S. Geological SurveyWoods Hole MA USA;</p> <p>U.S. Geological SurveyWoods Hole MA USA;</p> <p>U.S. Geological SurveySanta Cruz CA USA;</p> <p>U.S. Geological SurveyAnchorage AK 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=ocean‐continent boundary&option=203" rel="nofollow">ocean‐continent boundary;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=strike‐slip fault&option=203" rel="nofollow">strike‐slip fault;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=subduction initiation&option=203" rel="nofollow">subduction initiation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=bimaterial interface&option=203" rel="nofollow">bimaterial interface;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yakutat terrane&option=203" rel="nofollow">Yakutat terrane;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Haida Gwaii&option=203" rel="nofollow">Haida Gwaii;</a> </p> <div class="translation"> 机译：海洋大陆边界;防滑断层;俯冲启动;双层界面;yakutat terrane;海达gwaii; </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/0704025591122.html">Deformation of the Pacific/North America Plate Boundary at Queen Charlotte Fault: The Possible Role of Rheology</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Brink U. 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</li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-journal-cn_recent-developments-world-seismology_thesis/0201253432570.html">岩石变形所反映的地震作用过程--第13届国际变形机理、流变学和构造学学术会议概述</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=姚大全&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 姚大全</a> <span> <a href="/journal-cn-4935/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 国际地震动态 </a> </span> <span> . 2001</span><span>,第007期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_recent-developments-world-seismology_thesis/0201253422479.html">2011年5月中俄边界深震震源机制所展示的太平洋板块俯冲动力作用</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=陈棋福&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 陈棋福</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李圣强&option=202" target="_blank" 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class="tuijian_auth tuijian_authcolor">,高金哲</a> <span> <a href="/conference-cn-8747/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 中国地震学会第14次学术大会 </a> <span> <span> . 2012</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06130424317193.html">Automatic movable floor dust plate collecting device, has cover including fixed impact-boundary area whose deformation is detected by electrical or opto-electrical device during minimizing occurrence of impact and is analyzed by sensors</a> <b>[P]</b> . <span> 外国专利：  DE102009035149A1 </span> <span> . 2011-02-03</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：自动活动地板吸尘板收集装置，其盖子包括固定的冲击边界区域，在最小化冲击的发生期间，该边界通过电动或光电装置检测变形，并通过传感器进行分析 </span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06130422067086.html">ULTRASONIC PROBE AND AN ULTRASONIC PROBE DEVICE FOR PREVENTING DETECTION FAULT DUE TO THE DEFORMATION OF A PLATE</a> <b>[P]</b> . <span> 外国专利：  KR20120032970A </span> <span> . 2012-04-06</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：用于防止由于板的变形而引起的检测不良的超声波探头和超声波探头装置 </span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130445876878.html">Side impact detection device for automobile uses deformation sensor with sensor element mounted on base plate provided with temperature sensor for detection of rivetting fault</a> <b>[P]</b> . <span> 外国专利：  DE10103047C1 </span> <span> . 2002-07-25</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> 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