3‐D Characterization of Detrital Zircon Grains and its Implications for Fluvial Transport, Mixing, and Preservation Bias

Markwitz V.; Kirkland C. L.; Mehnert A.; Gessner K.; Shaw J.

摘要

Abstract > Detrital zircon studies can suffer from selective loss of provenance information due to U‐Pb age discordance, metamictization, metamorphic overprinting and fluviatile transport processes. The relationship between isotopic composition and zircon grain shape, and how grain shape is modified during transport, is largely unknown. We combine X‐ray tomography with U‐Pb geochronology to quantify how fluvial transport affects 3‐D zircon shape, detrital age signature, and grain density along the Murchison River, whose catchment comprises Eoarchean to Early Paleozoic source rocks in Western Australia. We acquired tomographic volumes and isotopic data from 373 detrital zircons to document changes in size, shape and density in transport direction, and explore how grain shape, age spectra and the proportion of discordant material vary along the channel. Results show that shape characteristics are sensitive to transport distance, stream gradient, proximity to source material, and whether the source consists of primary or recycled zircons. With increasing transport distance, grain lengths decrease more than their widths. Furthermore, the loss of metamict grains occurs at a near constant rate, resulting in a linear increase of mean calculated zircon density by ca. 0.03 g/cm 3 per 100 km transport distance. 3‐D grain shape is therefore strongly linked to detrital age signature, and mean grain density is a function of the absolute transport distance. 3‐D shape characteristics provide valuable information on detrital zircon populations, including the interaction between source materials with fluvial transport processes, which significantly affects preservation bias and, by inference, the representativeness of the sampled data. </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”> <标题类型=“main”>抽象</ title> > 由于U-PB时代的不良，代表性，变质叠印和氟基传输过程，碎屑锆石的研究可能会受到源于源自源的选择性丧失。同位素组合物和锆粒形状的关系，以及如何在运输过程中改变晶粒形状，大大未知。我们将X射线断层扫描与U-PB地质学相结合，以量化河流运输如何影响默奇森河的3D锆石形状，脱杆形状，谷物密度，其集水区包括eoarchean在西澳大利亚的早期古生代源岩。我们从373个拆卸锆石获得了断层摄影卷和同位素数据，以记录运输方向上的尺寸，形状和密度的变化，并探讨谷物形状，年龄谱和不和谐材料的比例沿着通道变化。结果表明，形状特性对运输距离，流梯度，源材料附近敏感，以及源是由主或回收的锆石组成。随着运输距离的增加，粒度比其宽度大幅下降。此外，以近恒定速率发生代谢颗粒的损失，导致CA的平均计算的锆石密度的线性增加。 0.03克/厘米 3 </ sup> 每100公里的运输距离。因此，3-D晶粒形状与脱毒年龄特征强烈连接，平均晶粒密度是绝对传输距离的函数。 3-D形特性提供有关碎屑锆石种群的有价值的信息，包括源材料与河流传输过程之间的相互作用，这显着影响了保存偏差，并通过推论，取样数据的代表性。 </ 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-23285/'>《Geochemistry, geophysics, geosystems》</a> <b style="margin: 0 2px;">|</b><span>2017年第12期</span><b style="margin: 0 2px;">|</b><span>共19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=Markwitz V.&option=202" target="_blank" rel="nofollow">Markwitz V.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kirkland C. L.&option=202" target="_blank" rel="nofollow">Kirkland C. L.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mehnert A.&option=202" target="_blank" rel="nofollow">Mehnert A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gessner K.&option=202" target="_blank" rel="nofollow">Gessner K.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Shaw J.&option=202" target="_blank" rel="nofollow">Shaw J.;</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>School of Earth SciencesThe University of Western AustraliaCrawley WA Australia;</p> <p>Department of Applied GeologyCentre for Exploration Targeting – Curtin Node John de Laeter Centre Institute of Geoscience Research (TIGeR);</p> <p>Curtin UniversityWA Australia;</p> <p>Centre for Microscopy Characterisation and AnalysisThe University of Western AustraliaCrawley WA Australia;</p> <p>Geological Survey of Western AustraliaEast Perth WA Australia;</p> <p>Centre for Microscopy Characterisation and AnalysisThe University of Western AustraliaCrawley WA Australia;</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=X‐ray tomography&option=203" rel="nofollow">X‐ray tomography;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=geochronology&option=203" rel="nofollow">geochronology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=zircon&option=203" rel="nofollow">zircon;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=roughness&option=203" rel="nofollow">roughness;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sphericity&option=203" rel="nofollow">sphericity;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=river transport&option=203" rel="nofollow">river transport;</a> </p> <div class="translation"> 机译：X射线断层扫描;地理学;锆石;粗糙;球形;河流运输; </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/0704023360768.html">3‐D Characterization of Detrital Zircon Grains and its Implications for Fluvial Transport, Mixing, and Preservation Bias</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Markwitz V.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Markwitz V.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kirkland C. 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