Genesis of Pb–Zn Mineralization Beneath the Xiangshan Uranium Orefield, South China: Constraints from H–O–S–Pb Isotopes and Rb–Sr Dating

Guo Jian; Li Ziying; Nie Jiangtao; Huang Zhizhang; Wang Jian; Lai Chun‐Kit

摘要

Abstract > The volcanic‐hosted Xiangshan uranium orefield is the largest uranium deposit in South China. Recent exploration has discovered extensive Pb–Zn mineralization beneath the uranium orebodies. Detailed geological investigation reveals that the major metallic minerals include pyrite, sphalerite, galena, and chalcopyrite, whilst the major non‐metallic minerals include quartz, sericite, and calcite. New δ 18 O <sub>fluid</sub> and δD <sub>fluid</sub> data indicate that the ore‐forming fluids were mainly derived from magmatic, and the sulfide δ 34 S values (2.2–6.9‰) suggest a dominantly magmatic sulfur source. The Pb isotope compositions are homogeneous ( 206 Pb/ 204 Pb?=?18.120–18.233, 207 Pb/ 204 Pb?=?15.575–15.698, and 208 Pb/ 204 Pb?=?37.047–38.446). The 87 Sr/ 86 Sr ratios of sulfide minerals range from 0.7197 to 0.7204, which is much higher than volcanic rocks and fall into the range of metamorphic basement. Lead and strontium isotopic compositions indicate that the metallogenic materials probably were derived from metamorphic basement. Pyrite Rb–Sr dating of the ores yielded 131.3?±?4.0?Ma, indicating that the Pb–Zn mineralization occurred in the Early Cretaceous. </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”> <标题类型=“main”>抽象</ title> > 火山托管的象山铀厄菲尔德是华南地区最大的铀矿床。最近的探索已经发现了铀矿石下方广泛的PB-ZN矿化。详细的地质调查显示，主要金属矿物质包括硫铁矿，斯普利特，加利纳和核黄素，同时主要的非金属矿物质包括石英，绢云母和方解石。新δ. 18 </ sup> O. <sub>流体</ sub> 和Δd <sub>流体</ sub> 数据表明矿石形成的流体主要来自岩浆，以及硫化物δ 34 </ sup> S值（2.2-6.9‰）建议是一个主要的岩石硫磺源。 PB同位素组合物是均质的（ 206 </ sup> PB / 204 </ sup> PB？=？18.120-18.233， 207 </ sup> PB / 204 </ sup> pb？=？15.575-15.698，和 208 </ sup> PB / 204 </ sup> PB？=？37.047-38.446）。这 87 </ sup> SR / 86 </ sup> 硫化物矿物质的SR比率范围为0.7197至0.7204，远远高于火山岩，并落入变质地下室的范围内。铅和锶同位素组合物表明，成矿材料可能是衍生自变质地下室。黄铁矿RB-SR的矿石的约会，产生131.3？±4.0？mA，表明PB-Zn矿化在早期的白垩纪中发生。 </ 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-26853/'>《Resource Geology》</a> <b style="margin: 0 2px;">|</b><span>2018年第3期</span><b style="margin: 0 2px;">|</b><span>共12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=Guo Jian&option=202" target="_blank" rel="nofollow">Guo Jian;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Ziying&option=202" target="_blank" rel="nofollow">Li Ziying;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nie Jiangtao&option=202" target="_blank" rel="nofollow">Nie Jiangtao;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Huang Zhizhang&option=202" target="_blank" rel="nofollow">Huang Zhizhang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wang Jian&option=202" target="_blank" rel="nofollow">Wang Jian;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lai Chun‐Kit&option=202" target="_blank" rel="nofollow">Lai Chun‐Kit;</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>Beijing Research Institute of Uranium GeologyBeijing China;</p> <p>Beijing Research Institute of Uranium GeologyBeijing China;</p> <p>Beijing Research Institute of Uranium GeologyBeijing China;</p> <p>Beijing Research Institute of Uranium GeologyBeijing China;</p> <p>Beijing Research Institute of Uranium GeologyBeijing China;</p> <p>Faculty of ScienceUniversiti Brunei DarussalamGadong Brunei Darussalam;</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=H–O–S–Pb isotopes&option=203" rel="nofollow">H–O–S–Pb isotopes;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pb–Zn mineralization&option=203" rel="nofollow">Pb–Zn mineralization;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pyrite Rb–Sr dating&option=203" rel="nofollow">Pyrite Rb–Sr dating;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=South China&option=203" rel="nofollow">South China;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Xiangshan&option=203" rel="nofollow">Xiangshan;</a> </p> <div class="translation"> 机译：H-O-S-PB同位素;PB-ZN矿化;黄铁矿RB-SR约会;华南;象山; </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"> 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RADIOACTIVE ELEMENTS</a> <b>[P]</b> . <span> 外国专利：  RU2457468C1 </span> <span> . 2012-07-27</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：铀和T放射性元素矿物集中体的电子探针化学U-Th-Pb定年方法 </span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06130421852682.html">METHOD OF CHEMICAL Electron-microprobe U-Th-Pb-DATING MINERALS Hub RADIOACTIVE ELEMENTS URANIUM AND THORIUM</a> <b>[P]</b> . <span> 外国专利：  RU2010149572A </span> <span> . 2012-06-10</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：化学电子探针U-Th-Pb定年矿物毂中放射性元素铀和HOR的方法 </span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130479905710.html">isotopbytesforfarande for enrichment of uranium on one of its isotopes jemte apparatus for implementation of</a> <b>[P]</b> . <span> 外国专利：  SE405652B </span> <span> . 1978-12-18</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：isotopbytesforfarande，用于在同位素同位素装置之一上富集铀，用于实施 </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" style="bottom: 19px;z-index: 999;" onclick="ywcd('0704024044032','4',7,2,1,'',this,24)" class="delivery" prompt="010401" title="通过人工服务将文献原文发送至邮箱" >获取原文</div> <div class="journalsub-pop-up" style="display: none"> <div class="journal-sub"> <h2>期刊订阅</h2> <img 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