Relationship Between Orogenic Gold Mineralization and Crustal Shearing Along Ailaoshan‐Red River Belt, Southeastern Tibetan Plateau: New Constraint From Paleomagnetism

Gao Liang; Wang Qingfei; Deng Jun; Zhang Shihong; Yang Zhenyu

摘要

Abstract >A new perspective on the relationship between orogenic gold mineralization and crustal shearing is presented in this case study on the gold deposits along Ailaoshan‐Red River shear zone (ARSZ), southeastern Tibetan Plateau. The sinistral ductile shearing along the zone occurred from ca. 31 to 17?Ma resulting in a displacement of ~1,000?km. A series of orogenic gold deposits, represented by the Zhenyuan and Chang'an deposits, occur on western margin of the ARSZ. The timing of mineralization and its relationship to shearing continues to be debated despite extensive geological and geochemical studies. Here we try to clarify this issue by using paleomagnetism to constrain the paleolatitude of mineralized rocks. High temperature magnetization components were isolated from the mineralized rocks, and they record modification by ore‐forming fluid. Their magnetization yields a paleolatitude of 19.9°?±?3.6°N for the Zhenyuan deposit and 16.2°?±?2.9°N for the Chang'an deposit. The paleolatitudes from these deposits are similar to those of ca. 20?Ma strata (19.0°?±?3.6°N), deposited after the large‐scale shearing. By contrast, they differ significantly from the paleolatitude obtained from ca. 130 to 40?Ma strata (28.4°?±?1.1°N), which formed long before the onset of large‐scale shearing. These observations imply that the orogenic gold mineralization occurred after the main offset and associated ductile deformation of the ARSZ. Gold mineralization is thought to be related to ore‐forming fluids and metals derived from the subcrust, rather than from fluids released from shearing‐induced metamorphism of regional strata. </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> >在泰国东南部的藏山红河剪切区（ARSZ）沿着山东山红河剪切区（ARSZ）的金矿床，提出了一种新的敌人金矿化和地壳剪切的关系。沿着该区域的Sinistral韧性剪切发生在该区域。 31至17？MA导致位移〜1,000 km。一系列由振园和长安存款代表的奥林族金矿床发生在阿斯兹西部边缘。尽管大广泛的地质和地球化学研究，但矿化的时间及其与剪切的关系仍然是争论。在这里，我们试图通过使用古磁石来限制矿化岩石的歌剧性来澄清这个问题。从矿化岩石中分离高温磁化组分，并通过形成矿石流体进行改性。它们的磁化强度产生19.9°的古孔，±3.6°N为Zhenyuan沉积物，16.2°θ≤2.9°N为长安矿床。来自这些沉积物的苍间穴与CA的苍榈。 20？MA STRATA（19.0°？±3.6°N），在大规模剪切后沉积。相比之下，它们与从加利福尼亚州获得的古孔差异有显着差异。 130至40？mA层（28.4°？±1.1°N），在大规模剪切开始之前长时间形成。这些观察结果暗示奥林斯金矿化在主偏移后发生和轴突的相关延性变形。认为金矿化被认为与矿石形成流体和衍生自组落的金属，而不是从剪切诱导的区域地层的变质释放的流体。</ 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-23285/'>《Geochemistry, geophysics, geosystems》</a> <b style="margin: 0 2px;">|</b><span>2018年第7期</span><b style="margin: 0 2px;">|</b><span>共18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=Gao Liang&option=202" target="_blank" rel="nofollow">Gao Liang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wang Qingfei&option=202" target="_blank" rel="nofollow">Wang Qingfei;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Deng Jun&option=202" target="_blank" rel="nofollow">Deng Jun;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Shihong&option=202" target="_blank" rel="nofollow">Zhang Shihong;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yang Zhenyu&option=202" target="_blank" rel="nofollow">Yang Zhenyu;</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>State Key Laboratory of Geological Processes and Mineral ResourcesChina University of GeosciencesBeijing China;</p> <p>State Key Laboratory of Geological Processes and Mineral ResourcesChina University of GeosciencesBeijing China;</p> <p>State Key Laboratory of Geological Processes and Mineral ResourcesChina University of GeosciencesBeijing China;</p> <p>State Key Laboratory of Geological Processes and Mineral ResourcesChina University of GeosciencesBeijing China;</p> <p>College of Resources Environment and TourismCapital Normal UniversityBeijing 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/163.html" title="地球物理学">地球物理学;</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=orogenic gold deposit&option=203" rel="nofollow">orogenic gold deposit;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ailaoshan‐Red River shear zone&option=203" rel="nofollow">Ailaoshan‐Red River shear zone;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=paleomagnetism&option=203" rel="nofollow">paleomagnetism;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhenyuan gold deposit&option=203" rel="nofollow">Zhenyuan gold deposit;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chang'an gold deposit&option=203" rel="nofollow">Chang'an gold deposit;</a> </p> <div class="translation"> 机译：orengenic金矿床;山山红河剪切区;古磁石;镇园金矿床;长安金矿床; </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> 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