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首页> 外文期刊>Resource Geology >Mineralogy, Fluid Inclusion, and Hydrogen and Oxygen Isotope Studies of the Intrusion‐Related Yangla Cu Deposit in the Sanjiang Region, SW China: Implications for Metallogenesis and Deposit Type
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Mineralogy, Fluid Inclusion, and Hydrogen and Oxygen Isotope Studies of the Intrusion‐Related Yangla Cu Deposit in the Sanjiang Region, SW China: Implications for Metallogenesis and Deposit Type

机译：矿物学，流体包容性和氢气和氧同位素和氧同位素研究在三江地区，SW中国的入侵相关yangla Cu矿床：对金属生成和沉积物的影响

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Abstract >The Yangla deposit is an intrusion‐related Cu deposit in the Jinshajiang tectonic belt (eastern Sanjiang region, SW China). Despite extensive studies that have been conducted on this deposit, the relationship between the granitic magma and Cu mineralization is still unclear, and hence, the genesis is debated. To answer this question, we conducted an integrated study of mineralogy, fluid inclusions (FIs), and hydrogen and oxygen (H‐O) isotopes. Three mineralization stages were identified based on the ore textures, alteration zonation, and crosscutting relationships: (i) pre‐ore prograde skarn (stage I), with the garnet and pyroxene dominated by andradite and diopside, respectively; (ii) syn‐ore retrograde alteration (stage II), which is subdivided into the early syn‐ore stage (stage IIa) marked by retrograde hydrated mineral assemblages and significant Fe‐Cu‐Mo‐Pb‐Zn sulfide mineralization, and the late syn‐ore stage (stage IIb) featured by quartz‐calcite veins; and (iii) late supergene mineralization (stage III), which is characterized by secondary azurite and malachite. These results of mineralogy, FIs, and H‐O isotopes indicate that: (i) Cu mineralization has a close temporal, spatial, and genetic relationship with skarn alteration; (ii) the ore fluids were magmatic dominated with late‐stage meteoric water incursion; and (iii) Type‐S (halite‐bearing) and Type‐V (vapor‐rich) FIs coexisted in garnet and clinopyroxene of stage I, indicating that fluid boiling might have occurred during this stage. From stage I to stage IIa, the FI type transformed from Type‐S?+?Type‐V?+?Type‐L (liquid‐rich) to Type‐V?+?Type‐L with the conduct of mineralization and was accompanied by the disappearance of Type‐S, and homogenization temperature and salinity also tended to decrease dramatically, which may be caused by the deposition of skarn minerals. At stage IIa, boiling of the ore fluids still continued due to the change from lithostatic to hydrostatic pressure, which triggered the precipitation of abundant quartz‐Cu‐Mo‐Fe sulfides. Furthermore, fluid mixing between a high‐temperature magmatic fluid and a low‐temperature meteoric water might cause a considerable drop in temperature and the deposition of Cu‐bearing quartz/calcite veins during stage IIb. Hence, we consider the Yangla deposit to be of a skarn type, genetically related to the Mesozoic magmatism in the Sanjiang region. </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> >杨拉矿床是金沙江构造带（Sw江地区，SW中国东部）的入侵相关的Cu矿床。尽管在该矿床上进行了广泛的研究，但花岗岩岩浆和Cu矿化之间的关系仍然尚不清楚，因此起因是争论。为了回答这个问题，我们进行了对矿物学，流体夹杂物（FIS）和氢气和氧（H-O）同位素的综合研究。基于矿石纹理，改变区划和横切关系鉴定了三个矿化阶段：（i）预矿石预剥离矽卡岩（阶段I），分别由Andradite和Diopside主导的石榴石和辉石; （ii）Syn-Ote逆行改变（阶段II），其被细分为由逆行水合矿物组合和显着的Fe-Cu-Mo-Pb-Zn硫化物矿化和晚期石英 - 方解石静脉特征的同步矿阶段（舞台IIB）; （iii）晚期叠加矿化（第三阶段），其特征在于二级硫酸盐和孔雀石。矿物学，FIS和H-O同位素的这些结果表明：（i）Cu矿化具有与矽卡岩改变的密切时间，空间和遗传关系; （ii）矿石液体是用后期陨石侵袭的岩浆岩。 （iii）型（核心轴承）和型型（富含蒸汽）FIS，其在石榴石和阶段I的Closococoxene中共存，表明在该阶段可能发生流体沸腾。从阶段I到IIA阶段，从Type-S？+ + + + + + +型（富含液体）到型-V？+？Type-L的行为，并伴随着矿化通过型号的消失，均质化温度和盐度也倾向于显着降低，这可能是由矽卡岩矿物的沉积引起的。在IIA阶段，由于从岩石静静压压力的变化，矿石流体的沸腾仍然继续，这引发了丰富的石英-CU-FE硫化物的沉淀。此外，在高温岩浆流体和低温易流水之间的流体混合可能在阶段IIB期间温度下降和Cu承载石英/方解石静脉的沉积。因此，我们认为杨拉矿床是矽卡型型，与三江地区中生代岩浆广告遗传有关。</ 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>2020年第1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=Du Li‐Juan&option=202" target="_blank" rel="nofollow">Du Li‐Juan;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Bo&option=202" target="_blank" rel="nofollow">Li Bo;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Huang Zhi‐Long&option=202" target="_blank" rel="nofollow">Huang Zhi‐Long;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chen Jun&option=202" target="_blank" rel="nofollow">Chen Jun;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhou Jia‐Xi&option=202" target="_blank" rel="nofollow">Zhou Jia‐Xi;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zou Guo‐Fu&option=202" target="_blank" rel="nofollow">Zou Guo‐Fu;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yan Zai‐Fei&option=202" target="_blank" rel="nofollow">Yan Zai‐Fei;</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>College of Resources and Environmental EngineeringGuizhou UniversityGuiyang China;</p> <p>Faculty of Land Resources EngineeringKunming University of Science and TechnologyKunming China;</p> <p>State Key Laboratory of Ore Deposit Geochemistry Institute of GeochemistryChinese Academy of SciencesGuiyang China;</p> <p>State Key Laboratory of Ore Deposit Geochemistry Institute of GeochemistryChinese Academy of SciencesGuiyang China;</p> <p>State Key Laboratory of Ore Deposit Geochemistry Institute of GeochemistryChinese Academy of SciencesGuiyang China;</p> <p>Yunnan Copper GroupKunming Prospecting Design Inst China NonferrousKunming China;</p> <p>State Key Laboratory of Ore Deposit Geochemistry Institute of GeochemistryChinese Academy of SciencesGuiyang 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=fluid source and evolution&option=203" rel="nofollow">fluid source and evolution;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=H‐O isotopes&option=203" rel="nofollow">H‐O isotopes;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sanjiang region (SW China)&option=203" rel="nofollow">Sanjiang region (SW China);</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yangla Cu skarn deposit&option=203" rel="nofollow">Yangla Cu skarn deposit;</a> </p> <div class="translation"> 机译：流体夹杂物;流体源和进化;H-O同位素;三江地区（SW中国）;杨拉铜矽卡岩; </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/0704024043908.html">Mineralogy, Fluid Inclusion, and Hydrogen and Oxygen Isotope Studies of the Intrusion‐Related Yangla Cu Deposit in the Sanjiang Region, SW China: Implications for Metallogenesis and Deposit Type</a> <b>[J]</b> . <span> <a 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