Rb–Sr Dating of Gold‐Bearing Pyrite in the Jinchang Porphyry Cu–Au Deposit, Heilongjiang Province, NE China

Zhang Peng; Kou Linlin; Bi Zhongwei; Han Renping; Zhao Yan; Sha Deming

摘要

Abstract >The Jinchang Cu–Au deposit in Heilongjiang Province, NE China, is located in the easternmost part of the Central Asian Orogenic Belt. Rb–Sr analyses of auriferous pyrite from the deposit yielded an isochron age of 113.7?±2.5?Ma, consistent with previously reported Re–Os ages. Both sets of ages represent the timing of Cu–Au mineralization because (i) the pyrite was separated from quartz–sulfide veins of the mineralization stage in granite porphyry; (ii) fluid inclusions have relatively high Rb, Sr, and Os content, allowing precise measurement; (iii) there are no other mineral inclusions or secondary fluids in pyrite to disturb the Rb–Sr or Re–Os decay systems; and (iv) the closure temperatures of the two decay systems are ≥500°C (compared with the homogenization temperatures of fluid inclusions of 230–510°C). It is proposed that ore‐forming components were derived from mantle–crust mixing, with ore‐forming fluids being mainly exsolved from magmas with minor amounts of meteoric water. The age of mineralization at Jinchang and in the adjacent regions, combined with the tectonic evolution of the northeast China epicontinental region, indicates that the formation of the Jinchang porphyry Cu–Au deposit was associated with Early Cretaceous subduction of the paleo‐Pacific Plate. </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”> <标题类型=“main”>抽象</ title> >黑龙江省尼龙江省尼克省，位于中亚造山带的东部最东部。来自沉积物的AuRiferes黄铁矿RB-SR分析产生了同种六年级113.7？±2.5？mA，与先前报道的RE-OS年龄一致。两组年龄代表了Cu-Au矿化的时序，因为（i）将吡钛体与花岗岩斑岩中的矿化阶段的石英 - 硫化物静脉分离; （ii）流体夹杂物具有相对高的Rb，Sr和OS含量，允许精确测量; （iii）黄铁矿中没有其他矿物质夹杂物或二次流体以干扰RB-SR或RE-OS衰减系统; （iv）两种衰减系统的闭合温度≥500℃（与230-510℃的流体夹杂物的均质温度相比）。提出，矿石成分衍生自甲壳物 - 地壳混合，形成矿石的流体，主要从磁带渗透，具有少量的陨石。金昌和邻近地区的矿化年龄与东北地区的构造演变相结合，表明金昌斑岩Cu-Au沉积物的形成与古太平洋板的早期白垩纪俯冲有关。< / 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9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 Peng&option=202" target="_blank" rel="nofollow">Zhang Peng;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kou Linlin&option=202" target="_blank" rel="nofollow">Kou Linlin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bi Zhongwei&option=202" target="_blank" rel="nofollow">Bi Zhongwei;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Han Renping&option=202" target="_blank" rel="nofollow">Han Renping;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhao Yan&option=202" target="_blank" rel="nofollow">Zhao Yan;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sha Deming&option=202" target="_blank" rel="nofollow">Sha Deming;</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>Shenyang Geological Survey CenterChina Geological SurveyShenyang China;</p> <p>Shenyang Geological Survey CenterChina Geological SurveyShenyang China;</p> <p>Shenyang Geological Survey CenterChina Geological SurveyShenyang China;</p> <p>Shenyang Geological Survey CenterChina Geological SurveyShenyang China;</p> <p>Shenyang Geological Survey CenterChina Geological SurveyShenyang China;</p> <p>Shenyang Geological Survey CenterChina Geological SurveyShenyang 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=Heilongjiang Province&option=203" rel="nofollow">Heilongjiang Province;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jinchang Cu–Au deposit&option=203" rel="nofollow">Jinchang Cu–Au deposit;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=NE China&option=203" rel="nofollow">NE China;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pyrite&option=203" rel="nofollow">Pyrite;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rb–Sr dating&option=203" rel="nofollow">Rb–Sr dating;</a> </p> <div class="translation"> 机译：he i龙江province;jin场Cu–AU deposit;NE China;pyrite;RB–SR大厅; 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. 2012</span><span>,第S1期</span> </span> </div> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-journal-cn_acta-geologica-sichuan_thesis/0201216741560.html">首次在冈底斯发现主碰撞期斑岩铜矿——来自西藏吉如斑岩铜矿辉钼矿Re-Os同位素年龄的证据</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=龚福志&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 龚福志</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=郑有业&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,郑有业</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=张刚阳&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,张刚阳</a> <span> <a href="/journal-cn-7828/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 四川地质学报 </a> </span> <span> . 2008</span><span>,第004期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_detail_thesis/0201294351471.html">斑岩铜矿床成模式新探——以西范坪斑岩铜矿床为例</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李泽琴&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 李泽琴</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王奖臻&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,王奖臻</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=倪师军&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,倪师军</a> <span> <a href="/journal-cn-57151/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 矿物学报 </a> </span> <span> . 2007</span><span>,第z1期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-59864_thesis/020222646601.html">冈底斯两期叠加斑岩铜矿化:以西藏吉如斑岩铜矿床为例</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=孙祥&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 孙祥</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=郑有业&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,郑有业</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=游智敏&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,游智敏</a> <span> <a href="/conference-cn-59864/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 第十一届全国矿床会议 </a> <span> <span> . 2012</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020314579638.html">斑岩铜矿遥感蚀变信息重现性与优选研究——以西藏自治区典型斑岩铜矿为例</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=张廷斌&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 张廷斌</a> <span> . 2014</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06120108065970.html">基于遥感蚀变异常的斑岩铜矿预测系统及方法</a> <b>[P]</b> . <span> 中国专利： CN105574621A </span> <span> . 2016-05-11</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/061201373698.html">多光谱遥感斑岩铜矿床蚀变分带信息提取方法及装置</a> <b>[P]</b> . <span> 中国专利： CN102749296B </span> <span> . 2014.05.14</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130432809764.html">application of water soluble u0430u043bu043au0430u043du0441u0443u043bu044cu0444u043eu043au0438u0441u043bu043eu0442 for increasing the permeability of underground.carbonate oil and / or gas bearing rock formations and for the dissolution of carbonate and / or u043au0430u0440u0431u043eu043du0430u0442u0441u043eu0434u0435u0440u0436u0430u0449u0438u0445 impurities in the oil</a> <b>[P]</b> . <span> 外国专利：  EA200701784A1 </span> <span> . 2008-04-28</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：水溶性 u0430 u043b u043a u0430 u043d u0441 u0443 u043b u044b u044c u0444 u043e u043a u0438 u0441 u043b u043b u043e u0442的应用增加地下碳酸盐油和 /的渗透性或含气体的岩层，以及碳酸盐和/或 u043a u0430 u0440 u0431 u043e u043e u043d u0430 u0442 u0441 u0431 u043e u0434 u0435 u0440 u0436 u0430 u0430 u0449 u0438 u0445油中的杂质 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130405820300.html">method of obtaining buttermilk, containing extract of chinese u043du0430u043du043eu0441u0442u0440u0443u043au0442u0443u0440u0438u0440u043eu0432u0430u043du043du044bu0439 u043bu0438u043cu043eu043du043du0438u043au0430</a> <b>[P]</b> . <span> 外国专利：  RU2016150596A </span> <span> . 2018-06-22</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：包含中文提取物的酪乳的获取方法 u043d u0430 u043d u043e u0441 u0442 u0440 u0443 u043a u0442 u0443 u0440u u0439 u043b u0438 u043c u043e u043d u043d u0438 u043a u0430 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130405820299.html">method of obtaining buttermilk, containing extract of chinese u043du0430u043du043eu0441u0442u0440u0443u043au0442u0443u0440u0438u0440u043eu0432u0430u043du043du044bu0439 u043bu0438u043cu043eu043du043du0438u043au0430</a> <b>[P]</b> . <span> 外国专利：  RU2016150596A3 </span> <span> . 2018-06-22</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：包含中文提取物的酪乳的获取方法 u043d u0430 u043d u043e u0441 u0442 u0440 u0443 u043a u0442 u0443 u0440u u0439 u043b u0438 u043c u043e u043d u043d u0438 u043a u0430 </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 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