Distant Taklimakan Desert as an Important Source of Aeolian Deposits on the Chinese Loess Plateau as Evidenced by Carbonate Minerals

Meng Xianqiang; Liu Lianwen; Zhao Wancang; He Tong; Chen Jun; Ji Junfeng

摘要

Abstract >It is generally agreed that the aeolian loess on the Chinese Loess Plateau (CLP) is derived from adjacent upwind arid areas, mainly including the Qaidam Desert, Alxa arid area, and Ordos Desert. However, the mineralogical and geochemical compositions of aeolian materials show several inconsistencies between these adjacent source areas and the CLP. Here, we compare the distribution of carbonate minerals in bulk samples and the 63‐μm fraction from upwind deserts to six loess sections from the CLP. The results show that the detrital dolomite and total carbonate, which are abundant in the loess of the CLP, are concentrated in the Taklimakan Desert rather than adjacent source areas. This finding suggests that the distant Taklimakan Desert is an important source of aeolian deposits on the CLP, reconciling the mineralogical and geochemical inconsistencies between CLP and adjacent areas. </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><抽象类型=“主要”的xml：郎=“EN”> <标题类型=“主”>抽象</ TITLE> <P>人们普遍认为，在中国黄土高原（CLP）的风成黄土源自相邻的逆风干旱地区，主要包括柴达木沙漠，阿拉善干旱地区，和鄂尔多斯沙漠。然而，风成材料的矿物学和地球化学组合物显示出这些相邻的源极区域和CLP之间的若干不一致。从上风沙漠63微米级分从CLP 6个黄土段;在这里，我们比较碳酸盐矿物的散装样品中的分布和＆lt。结果表明，碎屑白云石和总碳酸盐，它们是在中电的黄土丰富，都集中在塔克拉玛干沙漠，而不是相邻的源极区域。这一发现表明，遥远的塔克拉玛干沙漠是风成沉积物在CLP的重要来源，调和CLP和相邻区域之间的矿物学和地球化学不一致。</ p> </抽象> </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-23539/'>《Geophysical Research Letters》</a> <b style="margin: 0 2px;">|</b><span>2019年第9期</span><b style="margin: 0 2px;">|</b><span>共9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=Meng Xianqiang&option=202" target="_blank" rel="nofollow">Meng Xianqiang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Liu Lianwen&option=202" target="_blank" rel="nofollow">Liu Lianwen;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhao Wancang&option=202" target="_blank" rel="nofollow">Zhao Wancang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=He Tong&option=202" target="_blank" rel="nofollow">He Tong;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chen Jun&option=202" target="_blank" rel="nofollow">Chen Jun;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ji Junfeng&option=202" target="_blank" rel="nofollow">Ji Junfeng;</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>Ministry of Education Key Laboratory of Surficial Geochemistry School of Earth Sciences and EngineeringNanjing UniversityNanjing China;</p> <p>Ministry of Education Key Laboratory of Surficial Geochemistry School of Earth Sciences and EngineeringNanjing UniversityNanjing China;</p> <p>Chongqing Key Laboratory of Karst Environment School of Geographical SciencesSouthwest UniversityChongqing China;</p> <p>Ministry of Education Key Laboratory of Surficial Geochemistry School of Earth Sciences and EngineeringNanjing UniversityNanjing China;</p> <p>Ministry of Education Key Laboratory of Surficial Geochemistry School of Earth Sciences and EngineeringNanjing UniversityNanjing China;</p> <p>Ministry of Education Key Laboratory of Surficial Geochemistry School of Earth Sciences and EngineeringNanjing UniversityNanjing China;</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=Chinese Loess Plateau&option=203" rel="nofollow">Chinese Loess Plateau;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Taklimakan Desert&option=203" rel="nofollow">Taklimakan Desert;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=carbonate&option=203" rel="nofollow">carbonate;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=dolomite&option=203" rel="nofollow">dolomite;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=provenance&option=203" rel="nofollow">provenance;</a> </p> <div class="translation"> 机译：中国黄土高原;塔克拉玛坎沙漠;碳酸盐;白云岩;物质; </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> 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carbonates into porous materials is through microbiological reactions, including the provision of a liquid substrate material containing an organic carbon source that can be oxidized by microorganisms, an electronic receiver, and an antigen that can be deposited by carbonates and oxidized by microorganisms.</a> <b>[P]</b> . <span> 外国专利：  CL2008000952A1 </span> <span> . 2009-03-27</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：将碳酸盐沉淀到多孔材料中的方法是通过微生物反应，包括提供一种液体基质材料，该材料包含一种可以被微生物氧化的有机碳源，一个电子接收器以及一个可以被碳酸盐沉积并被微生物氧化的抗原。。 </span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06130468879122.html">METHOD OF AND APPARATUS FOR CHANGING MACHINABLITY AND MINEABILITY OF MINERAL DEPOSITS</a> <b>[P]</b> . <span> 外国专利：  PL143012B1 </span> <span> . 1987-12-31</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：改变矿床的可加工性和可矿性的方法和装置 </span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130472988345.html">METHOD OF AND APPARATUS FOR CHANGING MACHINABLITY AND MINEABILITY OF MINERAL DEPOSITS</a> <b>[P]</b> . <span> 外国专利：  PL246849A1 </span> <span> . 1985-09-24</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：改变矿床的可加工性和可矿性的方法和装置 </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" 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