• 主题
高级搜索  >
历史搜索 清空历史
首页> 外文期刊>Resource Geology >Fluid Inclusions and C, H, O, S, and Pb Isotopic Compositions of the Dabaoshan Cu Polymetallic Deposit, Northern Guangdong Province, South China
【24h】

Fluid Inclusions and C, H, O, S, and Pb Isotopic Compositions of the Dabaoshan Cu Polymetallic Deposit, Northern Guangdong Province, South China

机译：南方北部德巴山铜山Cu多金属矿床的流体夹杂物和C，H，O，S和Pb同位素组合物

获取原文
获取原文并翻译 | 示例
           
页面导航
  • 摘要
  • 著录项
  • 相似文献
  • 相关主题

摘要

Abstract >The Dabaoshan deposit in Northern Guangdong Province, South China, is a Cu–Mo–W–Pb–Zn polymetallic deposit, located in the southern part of the Qin–Hang porphyry–skarn Cu–Mo ore belt. The deposit mainly comprises porphyry Mo and stratiform skarn Cu ore deposits. The genesis of the Cu ore deposit has been ascribed to a typical skarn ore deposit formed by the metasomatism of Devonian carbonate rock layers or to a volcanic rock‐hosted massive sulfide deposit formed by marine exhalation. In this paper, we report on the homogenization temperatures and salinities of fluid inclusions and C, H, O, S, and Pb isotopic compositions of fluids and minerals in this deposit. Homogenization temperatures and salinities of fluid inclusions in garnet, diopside, quartz, and calcite provide information on the skarnification, mineralization, and postmineralization stages. The data show that ore‐forming fluids experienced a continuous transition from high temperatures and salinities to low temperatures and salinities over the entire period of mineralization. C, H, and O isotopic compositions indicate that ore‐forming fluids were derived mainly from magmatic water. O isotopic compositions indicate that ore‐forming fluids mingled with atmospheric water during the last stage of mineralization. Sulfur in the ore came mainly from deep magmatic sources. Pb isotopic compositions in the orebody show that almost all the lead in the ore was derived from magma with a crustal source. Combined geological, geophysical, and geochemical data were achieved before we proposed that the Dabaoshan porphyry–skarn Cu–Mo–W–Pb–Zn deposit, as one member of the Qin–Hang porphyry–skarn Cu–Mo ore belt, formed during the Jurassic subduction of the paleo‐Pacific plate beneath the Eurasian continent at quite low angle. NE‐ and EW‐trending structures controlled the emplacement of magmatic rocks in the South China region. In the mining area, the Xiangguanping Fault and its branches were the main conduits for magmatic crystallization and mineralization. The many subfaults, folds, and interlayer fracture zones on both sides of the main fault provided the requisite space for the ore and, together, were the controlling structures of the orebody. </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> >南方广东省北部的DabaoShan矿床是一种Cu-Mo-W-PB-ZN多金属矿床，位于秦悬斑岩 - 斯科恩铜矿座的南部。矿床主要包括斑岩Mo和层状矽卡岩Cu矿床。 Cu矿床的成因已经归因于由德国碳酸盐岩层的偏定术或通过海洋呼气形成的火山岩载体的火山锁定的大规模硫化物沉积物形成的典型矽卡岩矿床。在本文中，我们报告了该沉积物中流体夹杂物和C，H，O，S和Pb同位素组成的均质化温度和盐度。石榴石，缩孔，石英和方解石中流体夹杂物的均质化温度和盐度提供了有关矽卡型，矿化和后髓中异性阶段的信息。数据显示，在整个矿化期间，形成矿石流体在高温和盐度到低温和盐度的连续转变。 C，H和O同位素组合物表明，形成矿石的流体主要来自岩浆水。 o同位素组合物表明，在矿化的最后阶段，形成矿石的流体与大气水混合。矿石中的硫主要来自深岩石来源。矿石中的Pb同位素组合物表明，矿石中几乎所有的铅源自具有地壳源的岩浆。在我们提出Dabaoshan斑岩矽卡克-MB-W-W-PB-Zn沉积物之前实现了地质，地球物理和地球化学数据，作为秦悬浮斑岩 - 矽卡岩Cu-Mo矿带的一个成员侏罗纪俯冲了欧亚大陆在欧亚大陆下的古太平洋板块相当低。 Ne-and EW-Trowing结构控制了南方地区岩石岩石的施加。在矿区，Xiangguanping故障及其分支是岩浆结晶和矿化的主要导管。主要故障两侧的许多子凹槽，折叠和层间骨折区域为矿石提供了必要的空间，并且在一起是矿体的控制结构。</ 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=Qu Hongying&option=202" target="_blank" rel="nofollow">Qu Hongying;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mao Jingwen&option=202" target="_blank" rel="nofollow">Mao Jingwen;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhou Shumin&option=202" target="_blank" rel="nofollow">Zhou Shumin;</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>MLR Key Laboratory of Metallogeny and Mineral AssessmentInstitute of Mineral Resources Chinese Academy of Geological SciencesBeijing China;</p> <p>MLR Key Laboratory of Metallogeny and Mineral AssessmentInstitute of Mineral Resources Chinese Academy of Geological SciencesBeijing China;</p> <p>Department of Geological EngineeringQinghai UniversityXining 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=C&option=203" rel="nofollow">C;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=H&option=203" rel="nofollow">H;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=O&option=203" rel="nofollow">O;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=S&option=203" rel="nofollow">S;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=and Pb isotopes&option=203" rel="nofollow">and Pb isotopes;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cu mineralization&option=203" rel="nofollow">Cu mineralization;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dabaoshan deposit&option=203" rel="nofollow">Dabaoshan deposit;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=fluid inclusion&option=203" rel="nofollow">fluid inclusion;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=homogenization temperature and salinity&option=203" rel="nofollow">homogenization temperature and salinity;</a> </p> <div class="translation"> 机译：C;H;O;S;和Pb同位素;Cu矿化;Dabaoshan沉积物;流体包裹物;均质化温度和盐度; </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/0704024043912.html">Fluid Inclusions and C, H, O, S, and Pb Isotopic Compositions of the Dabaoshan Cu Polymetallic Deposit, Northern Guangdong Province, South China</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Qu Hongying&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Qu Hongying,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mao Jingwen&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Mao Jingwen,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhou Shumin&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Zhou Shumin </a> <a href="/journal-foreign-26853/" target="_blank" rel="nofollow" class="tuijian_authcolor">Resource Geology .</a> <span>2018</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：南方北部德巴山铜山Cu多金属矿床的流体夹杂物和C，H，O，S和Pb同位素组合物</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704025550563.html">Metallogenesis of stratiform Cu mineralization in the Dabaoshan polymetallic deposit, Northern Guangdong Province, South China</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> </a> <a href="/journal-foreign-34473/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geochemical Exploration: Journal of the Association of Exploration Geochemists .</a> <span>2020</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：南方北广东省达巴山多金属矿床层状Cu矿化的成矿</span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-foreign_journal-asian-earth-sciences_thesis/0204112271834.html">Petrogenesis of bismuth minerals in the Dabaoshan Pb-Zn polymetallic massive sulfide deposit, northern Guangdong Province, China</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lin Ye&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Lin Ye,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tiegeng Liu&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Tiegeng Liu,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yulong Yang&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Yulong Yang,</a> <a href="/journal-foreign-858/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Asian earth sciences .</a> <span>2014</span><span>,第mara15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：中国广东省北部大宝山铅锌多金属块状硫化物矿床中铋矿物的成因</span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-conference-foreign_quadrennial-internatial-associati-the-g_thesis/020512692409.html">He-Ar Isotopic Compositions of Ore-Forming Fluid from the Yushui Copper -polymetallic Deposit in Eastern Guangdong Province, South China</a> <b>[C]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=HUANG Yi&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">HUANG Yi,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext= SUN Xiaoming&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> SUN Xiaoming,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext= SHI Guiyong&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> SHI Guiyong,</a> <a href="/conference-foreign-82187/" 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：中国广东省东部东部雨水铜多金属矿床成矿流体的He-Ar同位素组成</span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-degree-foreign_mphd_thesis/02061452089.html">Genesis of strata-bound ore deposits in central Guangxi, South China: Fluid inclusion and isotope constraints.</a> <b>[D] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rao, Xuefeng.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Rao, Xuefeng. </a> <span>1997</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：华南中部地区地层约束矿床成因：流体包裹体和同位素约束。</span> </p> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-journal-foreign-pmc_detail_thesis/040004649761.html">Source Spatial Distribution and Pollution Assessment of Pb Zn Cu and Pb Isotopes in urban soils of Ahvaz City a semi-arid metropolis in southwest Iran</a> <b>[O] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ahad Nazarpour&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Ahad Nazarpour,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Michael J. Watts&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Michael J. Watts,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ayoub Madhani&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Ayoub Madhani,</a> <span>-1</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：伊朗西南半干旱大都市阿瓦兹市城市土壤中铅锌铜和铅同位素的来源空间分布和污染评估</span> </p> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/open-access_resources_thesis/01000128029457.html">Fluid Inclusions and C, H, O, S, and Pb Isotopic Compositions of the Dabaoshan Cu Polymetallic Deposit, Northern Guangdong Province, South China</a> <b>[O] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hongying Qu&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Hongying Qu,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jingwen Mao&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Jingwen Mao,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Shumin Zhou&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Shumin Zhou </a> <span>2018</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：南方北部达巴山铜铜铜铜铜铜铜铜铜铜铜金多金属矿床的流体夹杂物和C，H，O，S和PB同位素组成</span> </p> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/academic-journal-cn_chinese-journal-nonferrous-metals-english_thesis/0201298497959.html">宝山Cu-Pb-Zn多金属矿床流体演化证据:来自黄铁矿原位硫同位素和微量元素组成的制约</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=张俊柯&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 张俊柯</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=邵拥军&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,邵拥军</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=陈可&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,陈可</a> <span> <a href="/journal-cn-17995/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 中国有色金属学报:英文版 </a> </span> <span> . 2021</span><span>,第11期</span> </span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-cn_acta-petrologica-mineralogica_thesis/0201279722837.html">滇西镇康放羊山Cu-Pb-Zn多金属矿床流体包裹体和C-O同位素研究</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=陈伟&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 陈伟</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=邓明国&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,邓明国</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=耿齐卫&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,耿齐卫</a> <span> <a href="/journal-cn-5038/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 岩石矿物学杂志 </a> </span> <span> . 2020</span><span>,第006期</span> </span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-cn_geological-bulletin-china_thesis/0201252278304.html">湘东南铜山岭铅锌多金属矿床成矿时代与成矿物质来源——Sm-Nd等时线年龄和Pb同位素证据</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王云峰&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 王云峰</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=杨红梅&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,杨红梅</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=张利国&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,张利国</a> <span> <a href="/journal-cn-4820/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 地质通报 </a> </span> <span> . 2017</span><span>,第005期</span> </span> </div> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-journal-cn_acta-geologica-sinica_thesis/0201252703417.html">湘南铜山岭铜多金属矿床成矿物质来源的S、Pb、C同位素约束</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=蔡应雄&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 蔡应雄</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=谭娟娟&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,谭娟娟</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=杨红梅&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,杨红梅</a> <span> <a href="/journal-cn-4885/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 地质学报 </a> </span> <span> . 2015</span><span>,第010期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_mineral-deposits_thesis/0201289407070.html">小兴安岭西北部永新金矿床成矿流体来源与矿床成因:流体包裹体和H-O-S-Pb同位素证据</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=赵忠海&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 赵忠海</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=陈俊&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,陈俊</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=乔锴&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,乔锴</a> <span> <a href="/journal-cn-5005/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 矿床地质 </a> </span> <span> . 2021</span><span>,第002期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-497_thesis/02022947082.html">湖南铜山岭矽卡岩型多金属矿床成矿金属物质来源:Pb同位素的证据</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王云峰&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 王云峰</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=杨红梅&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,杨红梅</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=卢山松&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,卢山松</a> <span> <a href="/conference-cn-497/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 第十三届全国矿床会议 </a> <span> <span> . 2016</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020315118356.html">大巴山前陆带中生代构造活动流体同位素示踪及有机包裹体研究</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王显莹&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 王显莹</a> <span> . 2012</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06120473059.html">基本上包括锡(Sn)、银(Ag)、铜(Cu)和磷(P)的无Pb焊料合金组合物</a> <b>[P]</b> . <span> 中国专利： CN100467192C </span> <span> . 2009.03.11</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120105045479.html">基本上包括锡(Sn)、银(Ag)、铜(Cu)和磷(P)的无Pb焊料合金组合物</a> <b>[P]</b> . <span> 中国专利： CN1840282A </span> <span> . 2006-10-04</span> </div> </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('0704024043912','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"> <!-- <a href="javascript:void(0);" onclick="link_analysis('/shoppingcart/auth/list.html',this)">购物车</a>--> </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="0704024043912down" data-source="7," data-out-id="TPloCV6GvGk3D8RJElxgU73IGqq1hfCP4oo95sPkpoYJU7HaqDmLcdrBmmf75knF," data-f-source-id="7" data-title="Fluid Inclusions and C, H, O, S, and Pb Isotopic Compositions of the Dabaoshan Cu Polymetallic Deposit, Northern Guangdong Province, South China" 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="1" id="inyn_provide_service_level"> <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="Fluid Inclusions and C, H, O, S, and Pb Isotopic Compositions of the Dabaoshan Cu Polymetallic Deposit, Northern Guangdong Province, South China"/> <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=5.7.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/common.js?v=5.7.7"></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=5.7.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/tip.js?v=5.7.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/login.js?v=5.7.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/down.js?v=5.7.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/search.js?v=5.7.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/searchtype.js?v=5.7.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/user/regist.js?v=5.7.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/zxs_solor/detail.js?v=5.7.7"></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=5.7.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/weipu/weipu.js?v=5.7.7"></script> </body> <script> $(function(){ var weiPuStatus = getCookie('WeiPuStatus'); if(weiPuStatus){ tipWeiPuStatus(weiPuStatus); delCookie('WeiPuStatus'); } getFacetKeywordVoInId(); var sourcetype = $("#sourcetype").val(); var inyn_provide_service_level = $("#inyn_provide_service_level").val(); if((sourcetype ==1||sourcetype==4)&&inyn_provide_service_level!=4){ getJournal(); } }) </script> </html>