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Structures and Implications for Fluid Migration in the Jiadi Carlin‐Type Gold Deposit, Guizhou Province, Southwest China

机译:西南贵州省贵州省嘉迪卡林型金矿床液体迁移的结构和影响

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Abstract >The Jiadi gold deposit is a newly discovered Carlin‐type gold deposit in the Guizhou Province, Southwest China. This deposit is structurally controlled by a shallow fold–fault superimposed system along the Lianhuashan trend. Field geological investigations, structural analysis, and mathematical research are conducted to study its structures and hydrothermal fluid flow process. Geological investigations (i.e. sections, stope, and drill hole) indicate that the structures are dominated by NE‐trending folds, NWW‐trending folds, and faults. A trend‐surface analysis of the low interformational fracture zone suggests that the overall distribution of the Lianhuashan trend is controlled by the NE‐trending Lianhuashan anticline. Nearly all primary Carlin‐type gold deposits are distributed along the southeastern flank where the fold axis changes from NE to EW. Gold orebodies are hosted by the interformational fracture zones and primarily situated at the transitions from the high‐value areas to the low‐value areas of the interformational fracture zones. A stress analysis on the hydrothermal veins indicates that they are of tenso‐shear properties. The ore‐forming elements (Au, As, Sb, Hg, and Tl) of the hydrothermal veins from the interformational fracture zones and intrusive breccia body present strong positive anomalies compared with those from the adjacent wall rocks. According to the development patterns of the ore‐forming elements and hydrothermal veins, a migration process of the ore‐forming fluids is proposed: the deeply sourced ore‐forming fluids migrated vertically to shallow crust along an intrusive breccia body, subsequently flowed horizontally along the interformational fracture zones accompanied by gold precipitation in the early stage, and finally migrated outward along steep micro‐fractures during following stages. </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> <P>嘉迪金矿床是贵州省的新发现的Carlin型金矿床,中国西南部。该矿床由沿连风山潮流的浅折叠故障叠加系统结构控制。进行现场地质调查,结构分析和数学研究,以研究其结构和水热流体流动过程。地质调查(即部分,突起和钻孔)表明该结构由NE-趋势折叠,NWW趋势折叠和故障主导。低交织骨折区的趋势曲面分析表明,连日山趋势的总体分布是由Ne-Trenchan Antilline控制的。几乎所有主要的Carlin型金矿床沿着东南部侧翼分布,其中折叠轴从NE到EW发生变化。金矿石由各种骨折区域托管,主要位于从高价值区域的转换到可交织骨折区域的低值区域。水热静脉的应力分析表明它们具有抗剪切性能。与来自相邻墙岩岩石的相比,来自互联骨折区域和侵入性Breccia体的热热静脉的形成元素(Au,As,Sb,Hg和T1)存在强烈的正异常。根据矿石形成元件和水热静脉的显影图案,提出了一种形成矿石流体的迁移过程:沿着侵入性Breccia体垂直迁移到浅地壳的深度源矿石,随后水平流动在早期阶段伴随着金沉淀的结构骨折区域,最后在下降期间沿着陡微骨折向外迁移。</ 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4期</span><b style="margin: 0 2px;">|</b><span>共22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=Zeng Guoping&option=202" target="_blank" rel="nofollow">Zeng Guoping;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Luo Diwei&option=202" target="_blank" rel="nofollow">Luo Diwei;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gong Yongjun&option=202" target="_blank" rel="nofollow">Gong Yongjun;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hu Xinlu&option=202" target="_blank" rel="nofollow">Hu Xinlu;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Hang&option=202" target="_blank" rel="nofollow">Li Hang;</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>Wuhan Center of China Geological SurveyWuhan China;</p> <p>Faculty of Earth ResourcesChina University of GeosciencesWuhan China;</p> <p>Faculty of Earth ResourcesChina University of GeosciencesWuhan China;</p> <p>Faculty of Earth ResourcesChina University of GeosciencesWuhan China;</p> <p>Faculty of Earth ResourcesChina University of GeosciencesWuhan 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=Carlin‐type gold deposit&option=203" rel="nofollow">Carlin‐type gold deposit;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=fluid migration&option=203" rel="nofollow">fluid migration;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jiadi gold deposit&option=203" rel="nofollow">Jiadi gold deposit;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Southwest China&option=203" rel="nofollow">Southwest China;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=structures&option=203" rel="nofollow">structures;</a> </p> <div class="translation"> 机译:Carlin型金矿床;流体迁移;嘉迪金矿床;中国西南;结构; </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 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