首页> 外文期刊>Journal of quaternary science: JQS >Characterizing formation processes of Rimrock Lake, a Late Pleistocene–Holocene playa, Harney Basin, south‐eastern Oregon, USA, using an end‐member mixing analysis
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Characterizing formation processes of Rimrock Lake, a Late Pleistocene–Holocene playa, Harney Basin, south‐eastern Oregon, USA, using an end‐member mixing analysis

机译:利用末端成员混合分析

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ABSTRACT <section xml:id="jqs3048-sec-0001"> > Playas collect sediments from different transported processes, producing grain‐size distributions (GSDs) reflecting changes in environment. End‐member mixing analysis (EMMA) was used to derive end‐members (EMs) from 256 sediment samples from Rimrock Lake (Harney Basin, Oregon, USA) and a nearby relict channel. EMMA identified six EMs representing deposition in fluvial, lacustrine, littoral and colluvial environments. Stratigraphy was time‐correlated using nine radiocarbon dates. Results show that Rimrock Lake existed by ~ 18?535?cal a <sc>BP</sc> . A relict playa surface also was exposed along its margin and indicates lake contraction ~ 6190–5990?cal a <sc>BP</sc> . In the relict channel, a dominant eolian environment is identified at ~ 8000?cal a <sc>BP</sc> . These results represent a shift to a more arid environment in the Harney Basin beginning around the mid‐Holocene and are in general agreement with other studies reported in the Great Basin. This study demonstrates the application of EMMA for analyzing complex playa sediments and for linking environmental response across separate but related geomorphic environments. Our results provide a paleoenvironmental record along Harney Basin's western margin between ~ 18 500 and 6000?cal a <sc>BP</sc> and demonstrate the use of small playas in the basin as environmental archives. </section> </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”xml:lang =“en”> <title type =“main”>抽象</ title> <section XML:ID =“JQS3048-SEC-0001”> <P> Playas收集来自不同运输过程的沉积物,产生反映环境变化的晶粒尺寸分布(GSD)。结束成员混合分析(EMMA)用于从Rimrock Lake(Harney Basin,Oregon,USA)和附近的relict渠道的256个沉积物样本中获得最终成员(EMS)。 Emma确定了六个EMS,代表河流,湖泊,沿着陆运动环境中的沉积。使用九个radiocarbon日期是时间相关的地层。结果表明,Rimrock Lake〜18?535?CAL A <SC> BP </ SC>。依赖于依赖的Playa表面沿着其边缘暴露,并表示湖收缩〜6190-5990?Cal a <sc> bp </ sc>。在Relicc频道中,在〜8000℃下鉴定了主导的Eolian环境?CAL A <SC> BP </ SC>。这些结果代表了哈尼盆地在中东地区开始的更具干旱的环境,并与大盆地报道的其他研究一致。本研究表明EMMA在分析复杂的Playa沉积物中的应用,并在不同但相关的地貌环境中连接环境反应。我们的结果提供了沿着哈尼盆地的西部边缘的古环境记录〜18 500和6000?CAL A <SC> BP </ SC>,并展示了盆地中的小游戏作为环境档案。 </ p> </ section> </ 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-35770/'>《Journal of quaternary science: JQS》</a> <b style="margin: 0 2px;">|</b><span>2018年第6期</span><b style="margin: 0 2px;">|</b><span>共17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=Collins Joe D.&option=202" target="_blank" rel="nofollow">Collins Joe D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gill Thomas E.&option=202" target="_blank" rel="nofollow">Gill Thomas E.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Langford Richard&option=202" target="_blank" rel="nofollow">Langford Richard;</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 GeosciencesMiddle Tennessee State UniversityMurfreesboro TN USA;</p> <p>Department of Geological Sciencesthe University of Texas‐El PasoEl Paso TX USA;</p> <p>Department of Geological Sciencesthe University of Texas‐El PasoEl Paso 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><a href="https://www.zhangqiaokeyan.com/clc/27341.html" title="第四纪(系)">第四纪(系);</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=EMMA&option=203" rel="nofollow">EMMA;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=end‐member mixing analysis&option=203" rel="nofollow">end‐member mixing analysis;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Harney Basin&option=203" rel="nofollow">Harney Basin;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=playa sediments&option=203" rel="nofollow">playa sediments;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rimrock Lake&option=203" rel="nofollow">Rimrock Lake;</a> </p> <div class="translation"> 机译:Emma;终点混合分析;哈尼盆地;Playa沉积物;Rimrock湖; 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