Ancient Martian aeolian processes and palaeomorphology reconstructed from the Stimson formation on the lower slope of Aeolis Mons, Gale crater, Mars

Banham Steven G.; Gupta Sanjeev; Rubin David M.; Watkins Jessica A.; Sumner Dawn Y.; Edgett Kenneth S.; Grotzinger John P.; Lewis Kevin W.; Edgar Lauren A.; Stack‐Morgan Kathryn M.; Barnes Robert; Bell James F.; Day Mackenzie D.; Ewing Ryan C.; Lapotre Mathieu G.A.; Stein Nathan T.; Rivera‐Hernandez Frances; Vasavada Ashwin R.

摘要

Abstract > Reconstruction of the palaeoenvironmental context of Martian sedimentary rocks is central to studies of ancient Martian habitability and regional palaeoclimate history. This paper reports the analysis of a distinct aeolian deposit preserved in Gale crater, Mars, and evaluates its palaeomorphology, the processes responsible for its deposition, and its implications for Gale crater geological history and regional palaeoclimate. Whilst exploring the sedimentary succession cropping out on the northern flank of Aeolis Mons, Gale crater, the Mars Science Laboratory rover Curiosity encountered a decametre‐thick sandstone succession, named the Stimson formation, unconformably overlying lacustrine deposits of the Murray formation. The sandstone contains sand grains characterized by high roundness and sphericity, and cross‐bedding on the order of 1?m in thickness, separated by sub‐horizontal bounding surfaces traceable for tens of metres across outcrops. The cross‐beds are composed of uniform thickness cross‐laminations interpreted as wind‐ripple strata. Cross‐sets are separated by sub‐horizontal bounding surfaces traceable for tens of metres across outcrops that are interpreted as dune migration surfaces. Grain characteristics and presence of wind‐ripple strata indicate deposition of the Stimson formation by aeolian processes. The absence of features characteristic of damp or wet aeolian sediment accumulation indicate deposition in a dry aeolian system. Reconstruction of the palaeogeomorphology suggests that the Stimson dune field was composed largely of simple sinuous crescentic dunes with a height of ca 10?m, and wavelengths of ca 150?m, with local development of complex dunes. Analysis of cross‐strata dip azimuths indic </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：id =“sed12469-abs-0001”xml：lang =“en”> <title type =“main” >摘要</ title> > Martian沉积岩的古环境背景下的重建是古代火星居住地和区域古古怪历史研究的核心。本文报告了对大风陨石坑，火星保存的独特的Aeolian沉积物分析，并评估其古代，负责其沉积的流程，以及对大风陨石坑地质史和区域古群体的影响。虽然探索了山脉北侧的沉积连续，但火星科学实验室Rover 好奇心</ i>遇到了一种顽固的砂岩连续，命名为Stizson的形成，不合适地覆盖的湖泊沉积物默里形成。砂岩含有具有高圆度和球形的砂粒，以及厚度为1Ω·m的交叉床上用品，由横跨横跨露节划痕的子水平边界表面分开。横床由均匀的厚度交叉层压构成，被解释为风波层。交叉组通过诸如横跨露头的次横向边界表面来分开，该露头被解释为沙丘迁移表面。风纹纹层的晶粒特征和存在表示风神经过程沉积Stizson形成。没有潮湿或湿法沉积物积累特征特征，表明干燥的天气系统中的沉积。古神经形态的重建表明，Stimson Dune领域主要由简单的蜿蜒新月形沙丘组成，高度 Ca </ i> 10？m，波长为 Ca </ i> 150？m，有地方发展复杂沙丘。分析跨层滴角倾向表示 </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-28547/'>《Sedimentology: Journal of the International Association of Sedimentologists》</a> <b style="margin: 0 2px;">|</b><span>2018年第4期</span><b style="margin: 0 2px;">|</b><span>共50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=Banham Steven G.&option=202" target="_blank" rel="nofollow">Banham Steven G.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gupta Sanjeev&option=202" target="_blank" rel="nofollow">Gupta Sanjeev;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rubin David M.&option=202" target="_blank" rel="nofollow">Rubin David M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Watkins Jessica A.&option=202" target="_blank" rel="nofollow">Watkins Jessica A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sumner Dawn Y.&option=202" target="_blank" rel="nofollow">Sumner Dawn Y.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Edgett Kenneth S.&option=202" target="_blank" rel="nofollow">Edgett Kenneth S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Grotzinger John P.&option=202" target="_blank" rel="nofollow">Grotzinger John P.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lewis Kevin W.&option=202" target="_blank" rel="nofollow">Lewis Kevin W.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Edgar Lauren A.&option=202" target="_blank" rel="nofollow">Edgar Lauren A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Stack‐Morgan Kathryn M.&option=202" target="_blank" rel="nofollow">Stack‐Morgan Kathryn M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Barnes Robert&option=202" target="_blank" rel="nofollow">Barnes Robert;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bell James F.&option=202" target="_blank" rel="nofollow">Bell James F.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Day Mackenzie D.&option=202" target="_blank" rel="nofollow">Day Mackenzie D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ewing Ryan C.&option=202" target="_blank" rel="nofollow">Ewing Ryan C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lapotre Mathieu G.A.&option=202" target="_blank" rel="nofollow">Lapotre Mathieu G.A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Stein Nathan T.&option=202" target="_blank" rel="nofollow">Stein Nathan T.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rivera‐Hernandez Frances&option=202" target="_blank" rel="nofollow">Rivera‐Hernandez Frances;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Vasavada Ashwin R.&option=202" target="_blank" rel="nofollow">Vasavada Ashwin R.;</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 Earth Science and EngineeringImperial CollegeLondon SW7 2AZ UK;</p> <p>Department of Earth Science and EngineeringImperial CollegeLondon SW7 2AZ UK;</p> <p>Department of Earth and Planetary SciencesUniversity of California1156 High Street Santa Cruz CA 95064 USA;</p> <p>Division of Geological and Planetary SciencesCalifornia Institute of Technology1200 East California Boulevard Pasadena CA 91125 USA;</p> <p>Earth and Planetary SciencesUniversity of CaliforniaDavis CA 95616 USA;</p> <p>Malin Space Science SystemsP.O. Box 910148 San Diego CA 92191‐0148 USA;</p> <p>Division of Geological and Planetary SciencesCalifornia Institute of Technology1200 East California Boulevard Pasadena CA 91125 USA;</p> <p>Department of Earth and Planetary SciencesJohns Hopkins University301 Olin Hall 3400?N. Charles Street Baltimore MD 21218 USA;</p> <p>U.S. Geological Survey Astrogeology Science Center2255?N. Gemini Dr. Flagstaff AZ 86001 USA;</p> <p>Jet Propulsion LaboratoryCalifornia Institute of Technology4800 Oak Grove Drive Pasadena CA 91109 USA;</p> <p>Department of Earth Science and EngineeringImperial CollegeLondon SW7 2AZ UK;</p> <p>School of Earth and Space ExplorationArizona State UniversityTempe AZ 85287 USA;</p> <p>Department of Earth &</p> <p>Space SciencesUniversity of WashingtonSeattle WA 98195 USA;</p> <p>Department of Geology and GeophysicsTexas A&</p> <p>M UniversityCollege Station TX 77843 USA;</p> <p>Department of Earth and Planetary SciencesHarvard UniversityCambridge MA 02138 USA;</p> <p>Division of Geological and Planetary SciencesCalifornia Institute of Technology1200 East California Boulevard Pasadena CA 91125 USA;</p> <p>Earth and Planetary SciencesUniversity of CaliforniaDavis CA 95616 USA;</p> <p>Jet Propulsion LaboratoryCalifornia Institute of Technology4800 Oak Grove Drive Pasadena CA 91109 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/165.html" title="地质学">地质学;</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=Aeolian&option=203" rel="nofollow">Aeolian;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Curiosity rover&option=203" rel="nofollow">Curiosity rover;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=dune field&option=203" rel="nofollow">dune field;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gale crater&option=203" rel="nofollow">Gale crater;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mars&option=203" rel="nofollow">Mars;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mars Science Laboratory&option=203" rel="nofollow">Mars Science Laboratory;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=remote sensing&option=203" rel="nofollow">remote sensing;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Stimson&option=203" rel="nofollow">Stimson;</a> </p> <div class="translation"> 机译：风暴;好奇漫游者;沙丘田地;大风陨石坑;火星;火星科学实验室;遥感;Stimson; </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> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704024308611.html">Ancient Martian aeolian processes and palaeomorphology reconstructed from the Stimson formation on the lower slope of Aeolis Mons, Gale crater, Mars</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Banham Steven G.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Banham Steven G.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gupta Sanjeev&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Gupta Sanjeev,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rubin David M.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Rubin David M.,</a> <a href="/journal-foreign-28547/" target="_blank" rel="nofollow" class="tuijian_authcolor">Sedimentology: Journal of the International Association of Sedimentologists .</a> <span>2018</span><span>,第4期</span> </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：古老的火星Aeolian进程和古代从Aeolis Mons，Gale Crater，Mars的下坡中的Stizson形成重建。</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/070403646503.html">Comparing orbiter and rover image-based mapping of an ancient sedimentary environment, Aeolis Palus, Gale crater, Mars</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Stack K. 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