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首页> 外文期刊>Journal of geophysical research. Earth Surface: JGR >The Role of Lithospheric Flexure in the Landscape Evolution of the Wilkes Subglacial Basin and Transantarctic Mountains, East Antarctica
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The Role of Lithospheric Flexure in the Landscape Evolution of the Wilkes Subglacial Basin and Transantarctic Mountains, East Antarctica

机译：岩石弯曲在威尔克斯底峡流域景观演变中的作用，东南南极洲

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Abstract >Reconstructions of the bedrock topography of Antarctica since the Eocene‐Oligocene Boundary (approximately 34?Ma) provide important constraints for modeling Antarctic ice sheet evolution. This is particularly important in regions where the bedrock lies below sea level, since in these sectors the overlying ice sheet is thought to be most susceptible to past and future change. Here we use 3‐D flexural modeling to reconstruct the evolution of the topography of the Wilkes Subglacial Basin (WSB) and Transantarctic Mountains (TAM) in East Antarctica. We estimate the spatial distribution of glacial erosion beneath the East Antarctic Ice Sheet, and restore this material to the topography, which is also adjusted for associated flexural isostatic responses. We independently constrain our post‐34 Ma erosion estimates using offshore sediment stratigraphy interpretations. Our reconstructions provide a better‐defined topographic boundary condition for modeling early East Antarctic Ice Sheet history. We show that the majority of glacial erosion and landscape evolution occurred prior to 14?Ma, which we interpret to reflect more dynamic and erosive early ice sheet behavior. In addition, we use closely spaced 2‐D flexural models to test previously proposed hypotheses for a flexural origin of the TAM and WSB. The pre‐34 Ma topography shows lateral variations along the length of the TAM and WSB that cannot be explained by uniform flexure along the front of the TAM. We show that some of these variations may be explained by additional flexural uplift along the south‐western flank of the WSB and the Rennick Graben in northern Victoria Land. </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> >南极洲基岩地形的重建，因为南极洲边界（约34？ma）为建模南极冰纸进化提供重要的约束。这在基石位于海平面的地区尤其重要，因为在这些部门中，覆盖的冰板被认为是最容易受到过去和未来变化的影响。在这里，我们使用3-D弯曲建模来重建威尔克斯底冰盆地（WSB）和Transantarctic山脉（TAM）的地形的演变。我们估计东南极冰盖下面的冰川侵蚀的空间分布，并将这种材料恢复到地形，这也调整了相关的弯曲等静压反应。我们独立限制了使用海上沉积物地层解释的34次硕侵蚀估计。我们的重建为建模早期的南极冰盖历史提供了更好义的地形边界条件。我们展示了大部分冰川侵蚀和景观进化发生在14岁之前，我们解释了更加动态和腐蚀的早期冰板行为。此外，我们使用紧密间隔的2-D弯曲模型来测试先前提出的TAM和WSB的弯曲起源的假设。预先34 mA的地形显示沿着TAM和WSB的长度的横向变化，其无法通过沿TAM的前部均匀的弯曲来解释。我们表明，这些变化中的一些变化可以通过沿着WSB的西南侧翼和维多利亚州北部地区的RennickGraben进行额外的弯曲隆起来解释。</ 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-34664/'>《Journal of geophysical research. Earth Surface: JGR》</a> <b style="margin: 0 2px;">|</b><span>2019年第3期</span><b style="margin: 0 2px;">|</b><span>共18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=Paxman Guy J. G.&option=202" target="_blank" rel="nofollow">Paxman Guy J. G.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jamieson Stewart S. R.&option=202" target="_blank" rel="nofollow">Jamieson Stewart S. R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ferraccioli Fausto&option=202" target="_blank" rel="nofollow">Ferraccioli Fausto;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bentley Michael J.&option=202" target="_blank" rel="nofollow">Bentley Michael J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ross Neil&option=202" target="_blank" rel="nofollow">Ross Neil;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Watts Anthony B.&option=202" target="_blank" rel="nofollow">Watts Anthony B.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Leitchenkov German&option=202" target="_blank" rel="nofollow">Leitchenkov German;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Armadillo Egidio&option=202" target="_blank" rel="nofollow">Armadillo Egidio;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Young Duncan A.&option=202" target="_blank" rel="nofollow">Young Duncan 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 GeographyDurham UniversityDurham UK;</p> <p>Department of GeographyDurham UniversityDurham UK;</p> <p>British Antarctic SurveyCambridge UK;</p> <p>Department of GeographyDurham UniversityDurham UK;</p> <p>School of Geography Politics and SociologyNewcastle UniversityNewcastle upon Tyne UK;</p> <p>Department of Earth SciencesOxford UniversityOxford UK;</p> <p>Institute for Geology and Mineral Resources of the World OceanSt. Petersburg Russia;</p> <p>Dipartimento di Scienze della Terra dell'Ambiente e della VitaUniversità di GenovaGenoa Italy;</p> <p>Institute for GeophysicsUniversity of TexasAustin TX 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>TP79:P3; </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=flexure&option=203" rel="nofollow">flexure;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=landscape evolution&option=203" rel="nofollow">landscape evolution;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=East Antarctica&option=203" rel="nofollow">East Antarctica;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=paleotopography&option=203" rel="nofollow">paleotopography;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=glacial erosion&option=203" rel="nofollow">glacial erosion;</a> </p> <div class="translation"> 机译：柔性;景观进化;东南极洲;古图谱;冰川侵蚀; </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/0704025586818.html">The Role of Lithospheric Flexure in the Landscape Evolution of the Wilkes Subglacial Basin and Transantarctic Mountains, East Antarctica</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Paxman Guy J. 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