Geological and Geochemical Characteristics of Gold Mineralization in the Salu Bulo Prospect, Sulawesi, Indonesia

Tuakia Muhammad Zain; Takahashi Ryohei; Imai Akira

摘要

Abstract > The Salu Bulo prospect is one of the gold prospects in the Awak Mas project in the central part of the western province, Sulawesi, Indonesia. The gold mineralization is hosted by the meta‐sedimentary rocks intercalated with the meta‐volcanic and volcaniclastic rocks of the Latimojong Metamorphic Complex. The ores are approximately three meters thick, consisting of veins, stockwork, and breccias. The veins can be classified into three stages, namely, early, main, and late stages, and gold mineralization is related to the main stage. The mineral assemblage of the matrix of breccia and the veins are both composed of quartz, carbonate (mainly ankerite), and albite. High‐grade gold ores in the Salu Bulo prospect are accompanied by intense alteration, such as carbonatization, albitization, silicification, and sulfidation along the main stage veins and breccia. Alteration mineral assemblage includes ankerite?±?calcite, quartz, albite, and pyrite along with minor sericite. Pyrite is the most abundant sulfide mineral that is spatially related to native gold and electrum (2–42?μm in size). It is more abundant as dissemination in the altered host rocks than those in veins. This suggests that water–rock interaction played a role to precipitate pyrite and Au in the Salu Bulo prospect. The Au contents of intensely altered host rocks and ores have positive correlations with Ag, Ni, Mo, and Na. Fluid inclusions in the veins of the main stage and the matrix of breccia are mainly two‐phase liquid‐rich inclusions with minor two‐phase, vapor‐rich, and single‐phase liquid or vapor inclusions. CO <sub>2</sub> and N <sub>2</sub> gases are detected in the fluid inclusions by Laser Raman microspectrometry. Fluid boiling probably occurred when the fluid was trapped at approximately 120–190?m below the paleo water table. δ 18 O <sub>SMOW</sub> values of fluid, +5.8 and +7.6‰, calculated from δ 18 O <sub>SMOW</sub> of quartz from the main stage vein indicate oxygen isotopic exchange with wall rocks during deep circulation. δ 34 S <sub>CDT</sub> of pyrite narrowly ranges from ?2.0 to +3.4‰, suggesting a single source of sulfur. Gold mineralization in the Salu Bulo prospect occurred in an epithermal condition, after the metamorphism of the host rocks. It formed at a relatively shallow depth from fluids with low to moderate salinity (3.0–8.5?wt% NaCl equiv.). The temperature and pressure of ore formation range from 190 to 210°C and 1.2 to 1.9?MPa, respectively. </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”> <标题类型=“main”>抽象</ title> > Salu Bulo ProSpact是印度尼西亚苏拉威西州苏拉威西州南部Awak MAS项目的黄金前景之一。金矿化由嵌入与拉脱米隆变形复合物的元火山和火山岩岩石插入的荟沉积岩。矿石约3米厚，由静脉，库存和布雷奇累累组成。静脉可以分为三个阶段，即早期，主要和晚期阶段，黄金矿化与主要阶段有关。 Breccia和静脉基质的矿物组合均由石英，碳酸盐（主要是Ankerite）和Albite组成。 Salu Bulo ProSpect中的高档黄金矿石伴随着激烈的改变，如沿着主阶段静脉和Breccia的碳化，剥离，硅化和硫化。改变矿物组合包括α±α？方解石，石英，阿尔巴顿和黄铁矿以及轻微的绢云母。黄铁矿是最丰富的硫化物矿物质，其在空间上与天然金和电 - 电（＆2-42μm尺寸）。在改变的宿主岩石中传播比静脉更浓郁。这表明水岩相互作用在萨鲁的Bulo前景中发挥了沉淀黄铁矿和Au的作用。强烈改变的宿主岩石和矿石的Au含量与Ag，Ni，Mo和Na具有正相关性。在主阶段的静脉和Breccia基质中的流体夹杂物主要是两相富含富含型液体的夹杂物，具有较小的两相，富含蒸汽和单相液体或蒸汽夹杂物。 CO. <sub> 2 </ sub> 和n <sub> 2 </ sub> 通过激光拉曼微穴位测定在流体夹杂物中检测气体。当流体被捕获在古水位下方的120-190μm大约120-190μm时，可能发生流体沸腾。 δ. 18 </ sup> O. <sub> smow </ sub> 流体的值，+ 5.8和+ 7.6‰，从δ计算 18 </ sup> O. <sub> smow </ sub> 来自主阶段静脉的石英表明在深循环期间与壁岩有氧同位素交换。 δ. 34 </ sup> S. <sub> cdt </ sub> 硫铁矿范围从？2.0至+ 3.4‰狭窄，表明单一的硫来源。在主体岩石的变质之后，萨鲁的Bulo ProSpect中的金矿化发生在岩体条件下。它形成在较低的流体中的相对较浅的深度（3.0-8.5〜wt％NaCl时）。矿石形成的温度和压力分别为190至210℃和1.2至1.9℃。 </ 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=Tuakia Muhammad Zain&option=202" target="_blank" rel="nofollow">Tuakia Muhammad Zain;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Takahashi Ryohei&option=202" target="_blank" rel="nofollow">Takahashi Ryohei;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Imai Akira&option=202" target="_blank" rel="nofollow">Imai Akira;</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>Graduate School of Engineering and Resource ScienceAkita UniversityAkita Japan;</p> <p>Graduate School of International Resource SciencesAkita UniversityAkita Japan;</p> <p>Graduate School of International Resource SciencesAkita UniversityAkita Japan;</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=gold mineralization&option=203" rel="nofollow">gold mineralization;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Indonesia&option=203" rel="nofollow">Indonesia;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Salu Bulo&option=203" rel="nofollow">Salu Bulo;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sulawesi&option=203" rel="nofollow">Sulawesi;</a> </p> <div class="translation"> 机译：流体夹杂物;金矿化;印度尼西亚;萨鲁博罗;苏拉威西; </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/0704024043900.html">Geological and Geochemical Characteristics of Gold Mineralization in the Salu Bulo Prospect, Sulawesi, Indonesia</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tuakia Muhammad Zain&option=202" target="_blank" rel="nofollow" class="tuijian_auth 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