Nature and Genesis of the Xiaobeigou Fluorite Deposit, Inner Mongolia, Northeast China: Evidence from Fluid Inclusions and Stable Isotopes

Pei Qiuming; Zhang Shouting; Hayashi Ken‐ichiro; Wang Liang; Cao Huawen; Zhao Yu; Hu Xinkai; Song Kairui; Chao Weiwei

摘要

Abstract > The recently discovered Xiaobeigou fluorite deposit is situated in the southern part of the Southern Great Xing'an Range metallogenic belt. Fluorite‐bearing veins are rather common over the whole area. So far, 11 mineralized veins have been delineated at the Xiaobeigou deposit. Orebodies of the deposit are mainly hosted in Permian and Jurassic volcano‐sedimentary rocks. The orebodies in this mining district exhibit a well‐developed vertical zonation: from top to bottom, the orebodies can be divided into upper, central, and lower zones. The central zone is the most important part for mining operations, and it shows lateral zonation of fluorite mineralization. Rare earth element (REE) contents of the investigated samples are relatively low (less than 30.2?ppm). Furthermore, the REE contents of the fluorite grains from early to late ore stages exhibit a decreasing trend. All the fluorite samples show no or slightly positive Eu anomalies. Three types of fluid inclusions (FIs) are distinguished in the quartz and fluorite samples, including pure‐liquid single‐phase (PL‐type), liquid‐rich two‐phase (L‐Type), and vapor‐rich two‐phase (V‐type) FIs. The FIs hosted in early‐stage quartz were homogenized at 159.5–260.7°C (mainly 160–240°C); their salinities range from 0.18 to 1.22?wt.% NaCl eqv. The FIs hosted in early‐stage fluorite yield slightly lower homogenization temperatures of 144.4–266.8°C (peaking at 140–220°C), which correspond to salinities of 0.18–0.88?wt.% NaCl eqv. Homogenization temperatures and salinities for the late stage are 132.5–245.8°C (mainly 160–180°C) and 0.18–1.40?wt.% NaCl eqv., respectively. Laser Raman spectroscopy of FIs shows that both the vapor and liquid compositions of the inclusions are dominated by H <sub>2</sub> O. The H–O isotopic compositions at Xiaobeigou suggest that the ore‐forming fluids are predominantly of meteoric water origin. The Xiaobeigou deposit can be classified as a typical low‐temperature hydrothermal vein‐type fluorite deposit. Combined with regional data, we infer that the fluorite mineralization occurred during the Late Mesozoic in an extensional setting. </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> > 最近发现的Xiaobeigou Fluorite沉积物位于南方Xing'an范围内成熟带的南部。含氟杆菌静脉在整个区域上相当常见。到目前为止，在萧叶沟矿床上划定了11个矿化静脉。矿床的矿体主要托管在二叠纪和侏罗纪火山 - 沉积岩石中。本矿区的矿物展示了一个发达的垂直区划：从上到下，矿体可以分为上部，中央和下部区域。中央区是采矿业务最重要的部分，它显示出萤石矿化的横向区划。稀土元素（REE）所研究的样品的含量相对较低（小于30.2μpm）。此外，从早期到晚期矿石阶段的萤石颗粒的REE含量表现出降低趋势。所有萤石样品都显示出没有或略微正面的EU异常。在石英和萤石样品中区分三种类型的液体夹杂物（FIS），包括纯液体单相（PL型），富含液体的两相（L型）和富含蒸汽的两相（ V型）FIS。早期石英中托管的FIS在159.5-260.7°C（主要是160-240°C）均匀化;他们的盐度范围为0.18至1.22？wt。％NaCl EQV。在早期氟钛矿的FIS载入均匀较低的均质化温度为144.4-266.8℃（在140-220℃下达到峰值），其对应于0.18-0.88的盐度。％NaCl EQV。晚期均质化温度和盐度为132.5-245.8°C（主要是160-180℃）和0.18-1.40〜0.18-1.40℃％NaCl EQV。 FIS的激光拉曼光谱表明，夹杂物的蒸气和液体组合物均以H主导 <sub> 2 </ sub> o.萧叶沟的H-O同位素组合物表明，矿石形成液主要是陨石来源。萧叶榫矿床可归类为典型的低温水热静脉型萤石矿床。结合区域数据，我们推断萤石矿化在延伸环境中的后期中生代期间发生。 </ 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>2019年第2期</span><b style="margin: 0 2px;">|</b> <span>共19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=Pei Qiuming&option=202" target="_blank" rel="nofollow">Pei Qiuming;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Shouting&option=202" target="_blank" rel="nofollow">Zhang Shouting;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hayashi Ken‐ichiro&option=202" target="_blank" rel="nofollow">Hayashi Ken‐ichiro;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wang Liang&option=202" target="_blank" rel="nofollow">Wang Liang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cao Huawen&option=202" target="_blank" rel="nofollow">Cao Huawen;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhao Yu&option=202" target="_blank" rel="nofollow">Zhao Yu;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hu Xinkai&option=202" target="_blank" rel="nofollow">Hu Xinkai;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Song Kairui&option=202" target="_blank" rel="nofollow">Song Kairui;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chao Weiwei&option=202" target="_blank" rel="nofollow">Chao Weiwei;</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>Faculty of Geosciences and Environmental EngineeringSouthwest Jiaotong UniversityChengdu China;</p> <p>School of Earth Sciences and ResourcesChina University of GeosciencesBeijing China;</p> <p>Graduate School of Life and Environmental Sciences (Earth Evolution Sciences)University of TsukubaIbaraki Japan;</p> <p>School of Earth Sciences and ResourcesChina University of GeosciencesBeijing China;</p> <p>Chengdu CenterChina Geological SurveyChengdu China;</p> <p>School of Earth Sciences and ResourcesChina University of GeosciencesBeijing China;</p> <p>School of Earth Sciences and ResourcesChina University of GeosciencesBeijing China;</p> <p>School of Earth Sciences and ResourcesChina University of GeosciencesBeijing China;</p> <p>School of Earth Sciences and ResourcesChina University of GeosciencesBeijing 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=fluid inclusions&option=203" rel="nofollow">fluid inclusions;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=fluorite deposit&option=203" rel="nofollow">fluorite deposit;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=H–O isotope compositions&option=203" rel="nofollow">H–O isotope compositions;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ore genesis&option=203" rel="nofollow">ore genesis;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=vertical zonation&option=203" rel="nofollow">vertical zonation;</a> </p> <div class="translation"> 机译：流体夹杂物;萤石沉积物;H-O同位素组合物;矿石创世纪;垂直区分; </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/0704024044030.html">Nature and Genesis of the Xiaobeigou Fluorite Deposit, Inner Mongolia, 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target="_blank" rel="nofollow" class="tuijian_authcolor"> . 矿产勘查 </a> </span> <span> . 2019</span><span> ,第008期</span> </span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-cn_mineral-exploration_thesis/0201278713790.html">鄂东北金鸡坳金矿成矿流体性质及物质来源:来自矿床地质、流体包裹体及S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=吴昌雄&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 吴昌雄</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=刘永生&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,刘永生</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=刘兴平&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,刘兴平</a> <span> <a href="/journal-cn-20883/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 矿产勘查 </a> </span> <span> . 2019</span><span> ,第008期</span> </span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-cn_acta-geologica-sinica_thesis/0201252700994.html">内蒙古白乃庙铜-金-钼矿床成矿机制——来自流体包裹体和He-Ar同位素的证据</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=周振华&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 周振华</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=车合伟&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,车合伟</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=欧阳荷根&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,欧阳荷根</a> <span> <a href="/journal-cn-4885/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 地质学报 </a> </span> <span> . 2017</span><span> ,第003期</span> </span> </div> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-journal-cn_detail_thesis/0201296724529.html">湘东北地区栗山铅锌铜多金属矿床的成因探讨：来自矿床地质、矿物学和硫同位素的证据</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=郭飞&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 郭飞</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王智琳&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,王智琳</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=许德如&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,许德如</a> <span> <a href="/journal-cn-56805/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 南京大学学报：自然科学版 </a> </span> <span> . 2018</span><span> ,第2期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_geological-review_thesis/0201291549016.html">新疆卡鲁安硬岩型锂矿床成矿流体性质:来自He—Ar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=刘涛&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 刘涛</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=赵悦&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,赵悦</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=秦燕&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,秦燕</a> <span> <a href="/journal-cn-4921/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 地质论评 </a> </span> <span> . 2021</span><span> ,第006期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-14486_thesis/020221159639.html">内蒙古甲乌拉银多金属矿床稳定同位素地球化学及成矿流体性质研究</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=翟德高&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 翟德高</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=刘家军&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,刘家军</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王建平&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,王建平</a> <span> <a href="/conference-cn-14486/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 第四届全国成矿理论与找矿方法学术讨论会 </a> <span> <span> . 2009</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020315118243.html">青海省赛什塘铜多金属矿床稳定同位素、流体包裹体及成矿作用研究</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=毛寅&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 毛寅</a> <span> . 2012</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/061202459161.html">一种斑岩型矿床的石英脉中流体包裹体水中锂同位素的测定方法</a> <b>[P]</b> . <span> 中国专利： CN104655712B </span> <span> . 2017.05.17</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120107150128.html">一种斑岩型矿床的石英脉中流体包裹体水中锂同位素的测定方法</a> <b>[P]</b> . <span> 中国专利： CN104655712A </span> <span> . 2015-05-27</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130411291689.html">ISOTOPIC METHOD FOR WATER NATURE DETERMINATION IN PRODUCT OF GAS AND GAS CONDENSATE DEPOSITS</a> <b>[P]</b> . <span> 外国专利：  RU2571781C1 </span> <span> . 2015-12-20</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：同位素法测定天然气和凝析气产物中的水质 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130435544522.html">Measurement of gluconeogenesis and intermediary metabolism using stable isotopes</a> <b>[P]</b> . <span> 外国专利：  US7256047B2 </span> <span> . 2007-08-14</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：使用稳定同位素测量糖异生和中间代谢 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130444852190.html">Measurement of gluconeogenesis and intermediary metabolism using stable isotopes</a> <b>[P]</b> . <span> 外国专利：  US2003148533A1 </span> <span> . 2003-08-07</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：使用稳定同位素测量糖异生和中间代谢 </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;" 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