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U‐PB Detrital Zircon Geochronology of the Lower Danube and Its Tributaries: Implications for the Geology of the Carpathians

机译：u-pb甲板替代锆石，较低的多瑙河及其支流：对喀尔巴阡山脉地质的影响

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Abstract >We performed a detrital zircon (DZ) U‐Pb geochronologic survey of the lower parts of the Danube River approaching its Danube delta, Black Sea sink, and a few large tributaries (Tisza, Jiu, Olt, and Siret) originating in the nearby Carpathian Mountains. Samples are modern sediments. DZ age spectra reflect the geology and specifically the crustal age formation of the source area, which in this case is primarily the Romanian Carpathians and their foreland with contributions from the Balkan Mountains to the south of Danube and the East European Craton. The zircon cargo of these rivers suggests a source area that formed during the latest Proterozoic and mostly into the Cambrian and Ordovician as island arcs and back‐arc basins in a Peri‐Gondwanan subduction setting (~600–440?Ma). The Inner Carpathian units are dominated by a U‐Pb DZ peak in the Ordovician (460–470?Ma) and little inheritance from the nearby continental masses, whereas the Outer Carpathian units and the foreland have two main peaks, one Ediacaran (570–610?Ma) and one in the earliest Permian (290–300?Ma), corresponding to granitic rocks known regionally. A prominent igneous Variscan peak (320–350?Ma) in the Danube's and tributaries DZ zircon record is difficult to explain and points out to either an extra Carpathian source or major unknown gaps in our understanding of Carpathian geology. Younger peaks corresponding to arc magmatism during the Alpine period make up as much as about 10% of the DZ archive, consistent with the magnitude and surface exposure of Mesozoic and Cenozoic arcs. </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> >我们进行了一个替代锆石（DZ）U-PB地理学调查，即多瑙河的下半年接近其多瑙河三角洲，黑海水槽和一些大型支流（Tisza，Jiu，Olt和Siret）起源于附近的喀尔巴阡山脉。样品是现代沉积物。 DZ年龄光谱反映了地质学，特别是源地区的地壳年龄形成，在这种情况下主要是罗马尼亚喀尔巴阡山脉及其前沿，从巴尔干山脉到多瑙河南部和东欧Craton的贡献。这些河流的锆石货物建议在最新的正面形成的源区，主要是在乡村弧线和壁球弧和后弧盆地中形成的寒武纪和奥陶艺术者（〜600-440？MA）。内部喀尔巴阡山脉的单位由奥陶诺维安（460-470？MA）的U-PB DZ峰统治，以及附近的大陆群众的遗传性很少，而外部喀尔巴阡山脉单位和前陆有两个主要峰，一个埃德克兰（570- 610？ma）和最早的二叠纪（290-300？ma）中的一个，对应于区域已知的花岗岩。在多瑙河和支流DZ锆石记录中突出的火成岩峰（320-350？MA）很难解释，并指出在我们对喀尔巴阡山地地质学的理解中额外的喀尔巴阡山脉来源或主要的未知差距。在高山期间对应于弧形岩浆活动的较小峰值，占DZ存档的约10％，与中生代和新生型弧的幅度和表面暴露一致。</ 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>2018年第9期</span><b style="margin: 0 2px;">|</b><span>共16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=Ducea Mihai N.&option=202" target="_blank" rel="nofollow">Ducea Mihai N.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Giosan Liviu&option=202" target="_blank" rel="nofollow">Giosan Liviu;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Carter Andrew&option=202" target="_blank" rel="nofollow">Carter Andrew;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Balica Constantin&option=202" target="_blank" rel="nofollow">Balica Constantin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Stoica Adriana M.&option=202" target="_blank" rel="nofollow">Stoica Adriana M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Roban Relu D.&option=202" target="_blank" rel="nofollow">Roban Relu D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Balintoni Ion&option=202" target="_blank" rel="nofollow">Balintoni Ion;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Filip Florin&option=202" target="_blank" rel="nofollow">Filip Florin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Petrescu Lucian&option=202" target="_blank" rel="nofollow">Petrescu Lucian;</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>University of ArizonaTucson AZ USA;</p> <p>Woods Hole Oceanographic InstitutionWoods Hole MA USA;</p> <p>University of LondonLondon UK;</p> <p>Babes‐Bolyai UniversityCluj Napoca Romania;</p> <p>University of ArizonaTucson AZ USA;</p> <p>Faculty of Geology and GeophysicsUniversity of BucharestBucharest Romania;</p> <p>Babes‐Bolyai UniversityCluj Napoca Romania;</p> <p>Institute for Fluvial and Marine SystemsRomania;</p> <p>Faculty of Geology and GeophysicsUniversity of BucharestBucharest Romania;</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=Danube&option=203" rel="nofollow">Danube;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Carpathians&option=203" rel="nofollow">Carpathians;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=detrital zircon&option=203" rel="nofollow">detrital zircon;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=U‐Pb geochronology&option=203" rel="nofollow">U‐Pb geochronology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=continental crust&option=203" rel="nofollow">continental crust;</a> </p> <div class="translation"> 机译：多瑙河;喀尔巴阡山脉;碎屑锆石;U-PB地理学;大陆地壳; </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> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704023360487.html">U‐PB Detrital Zircon Geochronology of the Lower Danube and Its Tributaries: Implications for the Geology of the Carpathians</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ducea Mihai N.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Ducea Mihai N.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Giosan Liviu&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Giosan Liviu,</a> <a 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