Deciphering topographic signals of glaciation and rock uplift in an active orogen: a case study from the Olympic Mountains, USA

Adams B. A.; Ehlers T. A.

摘要

Abstract >Estimating recent patterns of erosion and rock uplift within Cenozoic orogens has proven difficult as signals of these processes have been obfuscated by Plio‐Pleistocene glaciation. The topography of many mountain ranges integrates the effects of long‐lived rock uplift, Late‐Cenozoic climate variation, and post‐glacial landscape adjustment. In this study, we employ a suite of topographic analyses to study the relief of an active mountain range on a sub‐catchment scale in an effort to the separate the long‐term signal of rock uplift from perturbations due to shorter‐lived climate signals. We focus on the Olympic Mountains, USA, where patterns of exhumation and glaciation have been previously estimated; however, our methods and results are broadly applicable to other orogens. >Our analysis shows that Plio‐Pleistocene alpine glaciers and the Cordilleran Ice Sheet have reduced the elevations of channel profiles and created anomalously low channel relief in the Olympic Mountains. Large low‐gradient areas formed at lower elevations where ice sheets were present and alpine glaciers widened and deepened valleys. In the more rugged core of the range, near‐threshold hillslopes along the margins of the oversteepened glacially‐carved valleys, dominate the range. This implies a strong Plio‐Pleistocene glacial climate control on the topography over the more recent evolution of the Olympic Mountains. However, the broad relief structure of the range appears to still record the regional rock uplift pattern and is suggestive of an east‐plunging antiform, consistent with folding of the subducting plate or underplating of accreted rocks. Copyright ? 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> >估计最近的侵蚀和摇滚隆起模式由于这些过程的信号被Plio-epleistocene冰川混淆，新生代OROGens已经证明是困难的。许多山脉的地形整合了长期摇滚隆起，晚新生代气候变化和冰川后景观调整的影响。在这项研究中，我们采用了一套地形分析，以研究由于较短的气候信号，将岩石隆起的长期信号分离岩石隆起的长期信号，以研究积极山脉的浮雕。我们专注于美国奥运山脉，之前已经估计了挖掘和冰川模式;但是，我们的方法和结果广泛适用于其他OROGENS。我们的分析表明，Plio-epleistocene alpine冰川和Cordilleran冰盖已经降低了通道曲线的高度，并在奥运会中创造了异常的低通道浮雕山脉。在较低的升高的低梯度区域，存在冰盖的较低海拔，并且高山冰川加宽和加深的山谷。在更坚固的核心范围内，沿着超透明的冰川雕刻山谷的边缘近阈值山坡，主导了范围。这意味着对奥林匹克山脉更新演变的地形上的强大的Plioiscente冰川气候控制。然而，该范围的广泛浮雕结构似乎仍然记录了区域岩石隆起的图案，并且暗示了东坠落的抗椎间型，与折叠塌陷板的折叠或膨胀的岩石覆盖。版权？ 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11期</span><b style="margin: 0 2px;">|</b> <span>共13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=Adams B. A.&option=202" target="_blank" rel="nofollow">Adams B. A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ehlers T. A.&option=202" target="_blank" rel="nofollow">Ehlers T. A.;</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>Department of GeosciencesUniversity of TübingenGermany;</p> <p>Department of GeosciencesUniversity of TübingenGermany;</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;"> </p> </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/0704023139089.html">Deciphering topographic signals of glaciation and rock uplift in an active orogen: a case study from the Olympic Mountains, USA</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Adams B. 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class="enjiyixqcontent" href="/patent-detail/06120113620006.html">扩散型信号分子DSF在提升厌氧氨氧化絮状污泥活性中的应用</a> <b>[P]</b> . <span> 中国专利： CN113651419A </span> <span> . 2021-11-16</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120100195190.html">用于推断对象中的信号转导途径的转录因子的活性的方法</a> <b>[P]</b> . <span> 中国专利： CN109313196A </span> <span> . 2019-02-05</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130464385206.html">acoustic measuring device to study the permeabilitaet and klueftigkeit of rocks in the durchteuften mountains.</a> <b>[P]</b> . <span> 外国专利：  DE3582692D1 </span> <span> . 1991-06-06</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：声学测量装置，研究durchteuften山区的岩石的渗透性和klueftigkeit。 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130455970148.html">device for examination of the danger rock mountain massif of shock acoustic emission signals, according to the device for monitoring the rock mass risk bump by the acoustic emission signals</a> <b>[P]</b> . <span> 外国专利：  MD710B1 </span> <span> . 1997-04-30</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：一种用于根据冲击声发射信号监测岩体危险颠簸的装置，用于检查冲击声发射信号的危险岩山地块的装置 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: auto;display:none"> <h3 class="all_title" id="enpatent55">相关主题</h3> <ul id="subject"> </ul> </div> </div> </div> </div> <div class="right rightcon"> <div class="details_img cardcommon clearfix" style="margin-bottom: 10px;display:none;" > </div> </div> </div> <div id="thesis_get_original1" class="downloadBth" style="bottom: 19px;z-index: 999;" 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