首页> 外文期刊>Resource Geology >Two‐Stage Sulfide Mineral Assemblages in the Mineralized Ultramafic Rocks of the Laowangzhai Gold Deposit (Yunnan, SW China): Implications for Metallogenic Evolution

【24h】

Two‐Stage Sulfide Mineral Assemblages in the Mineralized Ultramafic Rocks of the Laowangzhai Gold Deposit (Yunnan, SW China): Implications for Metallogenic Evolution

机译：矿化超空地岩石的两级硫化物矿物组合（云南，SW中国）：对成矿的影响

获取原文

获取原文并翻译 | 示例

掌桥外文数据库（机构版） >>

开具论文收录证明 >>

页面导航

摘要
著录项
相似文献
相关主题

摘要

Abstract > The Laowangzhai gold deposit, located in the Ailaoshan gold belt (SW China), is hosted in various types of rocks, including in quartz porphyry, carbonaceous slate, meta‐sandstone, lamprophyre, and altered ultramafic rocks. In contrast to other wall rocks, the orebodies in altered ultramafic rocks are characterized by the occurrence of a large amount of Ni‐bearing minerals. The ore‐forming process of the orebodies hosted by altered ultramafic rocks can be divided into two stages: pyrite‐vaesite‐native gold and gersdorffite‐violarite stages. The contents of As and Sb increased during the evolution of ore‐forming fluid based on the mineral assemblages. Thermodynamic modeling of the Ni‐Cu‐As‐Fe‐S system using the SUPCRT92 software package with the updated database of slop16.dat indicates the f S <sub>2</sub> in ore‐forming fluid decreases significantly from stage I to stage II. The decreases of f S <sub>2</sub> due to crystallization of sulfides and f O <sub>2</sub> due to fluid–rock reaction were responsible for ore formation in altered ultramafic rocks of the Laowangzhai gold deposit. Geological evidence, the in situ sulfur isotope values of pyrite, and the other published isotopic data suggest that the ore‐forming fluid for ultramafic rock ores was dominantly composed of evolved magmatic fluid with the important input of sediments. </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> > Laowangzhai金矿床位于AilaoShan Gold Belt（SW China），举办了各种类型的岩石，包括石英斑岩，碳质石板，荟砂岩，羊普利和改变的超空地岩石。与其他壁岩相比，改变的超微岩石中的矿体的特征在于发生大量的Ni矿物质。由改变的超微岩石托管的矿石的形成过程可分为两个阶段：硫铁矿 - vaesite - 天然金和Gersdorffite-vigrArite阶段。基于矿物组合的矿石形成流体的演变期间，AS和Sb的含量增加。使用SUPCRT92软件包使用SUPCRT92软件包的NI-CU-AS-FE-S系统的热力学建模.DAT的更新数据库表示 f </ i> S. <sub> 2 </ sub> 在矿石中，在矿石中，从阶段I至II阶段显着降低。减少 f </ i> S. <sub> 2 </ sub> 由于硫化物结晶和 f </ i> O. <sub> 2 </ sub> 由于流体岩石反应，对拉曼寨金矿床的改变超微岩石中的矿石形成负责。地质证据，原位硫磷黄铁矿同位素值，另一个公开的同位素数据表明，超岩石岩体的矿石形成液主要由进化的岩浆流体组成，具有沉积物的重要输入。 </ 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>2019年第3期</span><b style="margin: 0 2px;">|</b><span>共17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=Zhang Huichao&option=202" target="_blank" rel="nofollow">Zhang Huichao;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chai Peng&option=202" target="_blank" rel="nofollow">Chai Peng;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Hongrui&option=202" target="_blank" rel="nofollow">Zhang Hongrui;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hou Zengqian&option=202" target="_blank" rel="nofollow">Hou Zengqian;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chen Shouming&option=202" target="_blank" rel="nofollow">Chen Shouming;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sun Yanbin&option=202" target="_blank" rel="nofollow">Sun Yanbin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Peng Qing&option=202" target="_blank" rel="nofollow">Peng Qing;</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>Institute of GeologyChinese Academy of Geological SciencesBeijing China;</p> <p>Institute of GeologyChinese Academy of Geological SciencesBeijing China;</p> <p>Institute of GeologyChinese Academy of Geological SciencesBeijing China;</p> <p>Institute of GeologyChinese Academy of Geological SciencesBeijing China;</p> <p>Institute of GeologyChinese Academy of Geological SciencesBeijing China;</p> <p>Zhenyuan Company of Yunnan Gold Co. Ltd.Zhenyuan China;</p> <p>Zhenyuan Company of Yunnan Gold Co. Ltd.Zhenyuan 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/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=Ailaoshan Gold Belt&option=203" rel="nofollow">Ailaoshan Gold Belt;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gold Deposit&option=203" rel="nofollow">Gold Deposit;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nano‐SIMS Analysis&option=203" rel="nofollow">Nano‐SIMS Analysis;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Thermodynamic Modeling&option=203" rel="nofollow">Thermodynamic Modeling;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ultramafic Rock Ores&option=203" rel="nofollow">Ultramafic Rock Ores;</a> </p> <div class="translation"> 机译：Ailaoshan金带;金矿床;纳米SIMS分析;热力学造型;超空地岩石矿石; </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/0704024043917.html">Two‐Stage Sulfide Mineral Assemblages in the Mineralized Ultramafic Rocks of the Laowangzhai Gold Deposit (Yunnan, SW China): Implications for Metallogenic Evolution</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Huichao&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Zhang Huichao,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chai Peng&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Chai Peng,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Hongrui&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Zhang Hongrui,</a> <a href="/journal-foreign-26853/" target="_blank" rel="nofollow" class="tuijian_authcolor">Resource Geology .</a> <span>2019</span><span>,第3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：矿化超空地岩石的两级硫化物矿物组合（云南，SW中国）：对成矿的影响</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704024181284.html">Microbial structures and possible bacterial sulfide fossils in the giant Jinding Zn-Pb deposit, Yunnan, SW-China: Insights into the genesis of Zn-Pb sulfide mineralization</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yaxiaer Yalikun&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Yaxiaer Yalikun,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chun-Ji Xue&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Chun-Ji Xue,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhi-Jie Dai&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Zhi-Jie Dai,</a> <a href="/journal-foreign-27769/" target="_blank" rel="nofollow" class="tuijian_authcolor">Ore Geology Reviews: Journal for Comprehensive Studies of Ore Genesis and Ore Exploration .</a> <span>2018</span><span>,第期</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：微生物结构和可能的细菌硫化物化石，云南，云南，云南：Zn-PB硫化物矿化的成因见解</span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704024181727.html">Microbial structures and possible bacterial sulfide fossils in the giant Jinding Zn-Pb deposit, Yunnan, SW-China: Insights into the genesis of Zn-Pb sulfide mineralization</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yaxiaer Yalikun&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Yaxiaer Yalikun,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chun-Ji Xue&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Chun-Ji Xue,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhi-Jie Dai&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Zhi-Jie Dai,</a> <a href="/journal-foreign-27769/" target="_blank" rel="nofollow" class="tuijian_authcolor">Ore Geology Reviews: Journal for Comprehensive Studies of Ore Genesis and Ore Exploration .</a> <span>2018</span><span>,第期</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：微生物结构和可能的细菌硫化物化石，云南，云南，云南：Zn-PB硫化物矿化的成因见解</span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-conference-foreign_acta-geologica-sinica_thesis/020511624405.html">The Occurrence of Iron Sulfide Minerals and Their Indication Significance of Mineralization Process in the Panzhihua Fe-Ti-V Oxide Deposit, SW China</a> <b>[C]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=GAO Wenyuan&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">GAO Wenyuan,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=HUANG Fei&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">HUANG Fei,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=PENG Yandong&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">PENG Yandong,</a> <a href="/conference-foreign-24082/" target="_blank" rel="nofollow" class="tuijian_authcolor">Quadrennial International Association on the Genesis of Ore Deposits Symposium;Geological Society of China .</a> <span>2014</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：中国攀枝花铁钛铁钒氧化物矿床中硫化铁矿物的赋存状态及成矿过程的指示意义</span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-degree-foreign_mphd_thesis/0206168812.html">Mineral paragenesis, geochemistry and geochronology investigations of the Carlin-type gold deposits at the Goldstrike property, northern Nevada: Implications for ore genesis, igneous petrogenesis and mineral exploration.</a> <b>[D] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Almeida, Carolina Michelin de.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Almeida, Carolina Michelin de. </a> <span>2009</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：内华达州北部Goldstrike矿区的Carlin型金矿的矿物共生，地球化学和年代学研究：对矿床成因，火成岩成因和矿物勘探的影响。</span> </p> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-journal-foreign-pmc_detail_thesis/040003982872.html">Novel Microbial Assemblages Dominate Weathered Sulfide-Bearing Rock from Copper-Nickel Deposits in the Duluth Complex Minnesota USA</a> <b>[O] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Daniel S. Jones&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Daniel S. Jones,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kim A. Lapakko&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Kim A. Lapakko,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zachary J. Wenz&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Zachary J. Wenz,</a> <span>2017</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：美国明尼苏达州德卢斯综合体的铜-镍矿床中新型微生物组合主导着风化的含硫硫化岩</span> </p> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/open-access_resources_thesis/0100060713893.html ">Emplacement age and PGE geochemistry of lamprophyres in the Laowangzhai gold deposit, Yunnan, SW China</a> <b>[O] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wang Jianghai (ฆߞں&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Wang Jianghai (ฆߞں,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Qi Liang ୠ&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Qi Liang ୠ,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yin An ̝&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Yin An ̝,</a> <span>2001</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：云南老王寨金矿床中煌斑岩的侵位年龄和pGE地球化学特征</span> </p> </li> <li> <div> <b>8. </b><a class="enjiyixqcontent" href="/ntis-science-report_pb_thesis/0207168838.html">Occurrence Model for Magmatic Sulfide-Rich Nickel-Copper-(Platinum-Group Element) Deposits Related to Mafic and Ultramafic Dike-Sill Complexes. Chapter I of Mineral Deposit Models for Resource Assessment.</a> <b>[R] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Schulz, K. J.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Schulz, K. J.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext= Woodruff, L. G.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> Woodruff, L. G.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext= Nicholson, W. W.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> Nicholson, W. W.,</a> <span>2014</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：与镁铁质和超镁铁质沥青复合物相关的富含岩浆硫化物的镍 - 铜 - （铂族元素）矿床的发生模型。第一章资源评估矿床模型。</span> </p> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/academic-journal-cn_acta-petrologica-sinica_thesis/0201252029212.html">江西宜春黄玉-锂云母花岗岩石中的铍矿化作用:铍磷酸盐矿物组合</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=车旭东&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 车旭东</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王汝成&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,王汝成</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=胡欢&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,胡欢</a> <span> <a href="/journal-cn-4795/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 岩石学报 </a> </span> <span> . 2007</span><span>,第006期</span> </span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-cn_acta-geologica-sinica_thesis/0201291548704.html">湘南地区钨锡多金属矿床矿石矿物组合、矿化蚀变特征及成矿流体组成</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李厚民&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 李厚民</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李立兴&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,李立兴</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=余金杰&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,余金杰</a> <span> <a href="/journal-cn-4885/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 地质学报 </a> </span> <span> . 2021</span><span>,第010期</span> </span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-cn_journal-geology_thesis/0201253949396.html">河南舞阳铁矿赵案庄组含矿层的岩石矿物组合特征及成矿作用</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=涂恩照&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 涂恩照</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=张洪武&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,张洪武</a> <span> <a href="/journal-cn-4985/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 地质学刊 </a> </span> <span> . 2016</span><span>,第004期</span> </span> </div> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-journal-cn_mineral-deposits_thesis/0201254127891.html">云南兰坪北部铜多金属矿化区成矿流体流动与矿化分带--矿石铅同位素和特征元素组成依据</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=徐启东&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 徐启东</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=周炼&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,周炼</a> <span> <a href="/journal-cn-5005/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 矿床地质 </a> </span> <span> . 2004</span><span>,第004期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_mineral-deposits_thesis/0201254128084.html">云南兰坪北部铜多金属矿化区成矿流体流动与矿化分带--流体包裹体和稳定同位素依据</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=徐启东&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 徐启东</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李建威&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,李建威</a> <span> <a href="/journal-cn-5005/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 矿床地质 </a> </span> <span> . 2003</span><span>,第004期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-24756_thesis/020221216865.html">江西宜春黄玉-锂云母花岗岩石中的铍矿化作用:铍磷酸盐矿物组合</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=车旭东&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 车旭东</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王汝成&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,王汝成</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=胡欢&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,胡欢</a> <span> <a href="/conference-cn-24756/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 2006年全国岩石学与地球动力学研讨会 </a> <span> <span> . 2006</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020311556030.html">东昆仑造山带夏日哈木铜镍硫化物矿床成矿岩浆作用：岩石及流体地球化学制约</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李建平&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 李建平</a> <span> . 2016</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06130471627345.html">still for the extraction of minerals from ultramafic rocks</a> <b>[P]</b> . <span> 外国专利：  SE442828B </span> <span> . 1986-02-03</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：仍用于从超镁铁质岩石中提取矿物 </span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06130417737091.html">The process of recovering gold and copper from the mixture of oxidized minerals and copper sulfide ores includes a series of floatation, discharge and leaching stages.</a> <b>[P]</b> . <span> 外国专利：  CL2013003024A1 </span> <span> . 2014-08-18</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：从氧化的矿物和硫化铜矿石的混合物中回收金和铜的过程包括一系列浮选，排出和浸出阶段。 </span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130432824438.html">Method for leaching Gold from sulfide ore of Copper containing Gold and / or silicate mineral containing Gold leaching cu comprising up to 7.9 or less content of cuContact The residue leaching the Ore with a s</a> <b>[P]</b> . <span> 外国专利：  CL2007002723A1 </span> <span> . 2008-04-18</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：从含铜量高达7.9％或以下的含铜金和/或硅酸盐矿物的硫化矿石中浸提金的方法 </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('0704024043917','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 src="https://cdn.zhangqiaokeyan.com/img/loginclose.png" alt="" onclick="$('.journalsub-pop-up').hide()"> <p class="pardon">抱歉，该期刊暂不可订阅，敬请期待！</p> <p class="current">目前支持订阅全部北京大学中文核心（2020）期刊目录。</p> <div style="display: flex;margin-top: 69px;justify-content: space-between;"> <div class="no-sub" onclick="$('.journalsub-pop-up').hide()">暂不订阅</div> <div class="other-sub" onclick="continueSub('from=pc-detail')">继续订阅其他期刊</div> </div> </div> </div> <div class="right_btn"> <ul> <li class="gouwuche">  </li> <li class="yijian"> <a href="javascript:void(0);" onclick="link_analysis('/mycenter/auth/complaint.html',this)">意见反馈</a> </li> <li class="top"> <a href="javascript:scrollTo(0,0);">回到顶部</a> </li> <li class="shouye"> <a href="/">回到首页</a> </li> </ul> </div> <div class="xllindexfooter"> <div class="xllindexfootercenter"> <div class="xllindexfooterleft left" > <div class="xllindexfooterleftli"> <ul> <li><a href="/about.html">关于掌桥</a></li> <li><a href="/help/helpmap.html">资源导航</a></li> <li><a href="/help/helpguide.html">新手指南</a></li> <li><a href="/help/helpcenter.html">常见问题</a></li> <li><a href="/sitemap.html">网站地图</a></li> <li><a href="/help/helpcenter.html?type=9">版权声明</a></li> </ul> </div> <div class="xllindexfooterleft"> <p class="xllindexfooterlefteamil">客服邮箱：kefu@zhangqiaokeyan.com</p> <div class="xllindexfooterlefttcp"> <div class="xllindexfooterpoliceiimg"></div> <div class="xllindexfooterpoliceispan"> <span>京公网安备：11010802029741号 </span> <span>ICP备案号：<a href="https://beian.miit.gov.cn" rel="nofollow" target="_blank">京ICP备15016152号-6</a></span> <span>六维联合信息科技 (北京) 有限公司©版权所有</span> </div> </div> </div> </div> <div class="xllindexfooterright left"> <ul> <li> <p style="font-weight: bold;">客服微信</p> <div></div> </li> <li> <p style="font-weight: bold;">服务号</p> <div></div> </li> </ul> </div> </div> </div> <span id="0704024043917down" data-source="7," data-out-id="tQ67A3NAodpJtkOsggEMTg8xfbZfHZQCvFkQ3oWVdlX/+ceSIEflmEUxqbpUEG8w," data-f-source-id="7" data-title="Two‐Stage Sulfide Mineral Assemblages in the Mineralized Ultramafic Rocks of the Laowangzhai Gold Deposit (Yunnan, SW China): Implications for Metallogenic Evolution" data-price="20" data-site-name="" data-transnum="24" style="display:none;"></span> <input type="hidden" value="4" id="sourcetype"> <input type="hidden" value="26853" id="journalid"> <input type="hidden" value="https://cdn.zhangqiaokeyan.com" id="imgcdn"> <input type="hidden" value="1" id="isdeatail"> <input type="hidden" value="" id="syyn_indexed_database"> <input type="hidden" value="" id="servicetype"> <input type="hidden" id="pagename" value="Two‐Stage Sulfide Mineral Assemblages in the Mineralized Ultramafic Rocks of the Laowangzhai Gold Deposit (Yunnan, SW China): Implications for Metallogenic Evolution"/> <input type="hidden" value="thesis_get_original" id="pageIdentification"> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/jquery-1.12.4.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/lwlh_ajax.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/zq.js?v=5.7.6"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/common.js?v=5.7.6"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/jquery.cookie.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/top.js?v=5.7.6"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/tip.js?v=5.7.6"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/login.js?v=5.7.6"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/down.js?v=5.7.6"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/search.js?v=5.7.6"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/searchtype.js?v=5.7.6"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/user/regist.js?v=5.7.6"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/zxs_solor/detail.js?v=5.7.6"></script> <script type="text/javascript" src="https://www.zhangqiaokeyan.com/statistics/static/pagecollection.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/tj.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/pushbaidu.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/history.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/util/cookie.js?v=5.7.6"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/weipu/weipu.js?v=5.7.6"></script> </body> <script> $(function(){ var weiPuStatus = getCookie('WeiPuStatus'); if(weiPuStatus){ tipWeiPuStatus(weiPuStatus); delCookie('WeiPuStatus'); } getFacetKeywordVoInId(); var sourcetype = $("#sourcetype").val(); if(sourcetype ==1||sourcetype==4){ getJournal(); } }) </script> </html>