Qingping Liu , Wei Chen , Juxing Tang , Yang Song , Jianzhen Zhang , Tengfei Liu , Qiang Wang , Zhuangzhuang Song
{"title":"利用地质和溪流沉积物地球化学数据识别高潜力金矿化:中国西藏拉萨中部地层当惹雍错西部地区案例研究","authors":"Qingping Liu , Wei Chen , Juxing Tang , Yang Song , Jianzhen Zhang , Tengfei Liu , Qiang Wang , Zhuangzhuang Song","doi":"10.1016/j.gexplo.2024.107454","DOIUrl":null,"url":null,"abstract":"<div><p>Northern Tibet exhibits abundant placer gold deposits, with a longstanding history of mining activities. Despite the widespread placer gold occurrences, the reports on the primary rock gold deposits or occurrences remain scarce. The central Lhasa terrane in northern Tibet hosts well-developed Zenong Group volcanic rocks, indicating great potential for the exploration of porphyry-epithermal copper (gold) deposits. Here, we select the Dangreyongcuo area in this region to investigate its metallogenetic potentiality, through a comprehensive 1:50,000 stream sediment geochemical survey, analyzing 12 elements (Au, As, Sb, Ag, Te, Cu, Pb, Zn, W, Sn, Bi, and Mo), and a detailed geological mapping. We aim to identify gold-related mineralization anomalies and provide clues for further bedrock gold exploration in this region. Based on the stream sediment geochemical data, zones 1–4, have been delineated using single-element indicator Au and element association indicator Au + As + Sb, which was determined through robust principal component analysis (RPCA) and using the exploratory data analysis (EDA) method. Subsequent validation exercises evaluating these four delineated zones reveal that Zone 1, Xinlong-Langmeila area, is the most promising prospect due to its high element concentrations, large size, and marked coincidence of element assemblages (also referred to as high-large-coincidence anomalies; HLCAs) and its characteristics are in line with those of epithermal deposits. Notably, the Xinlong deposit represents the first documented epithermal gold deposit hosted within the Zenong Group volcanic rocks. The identification of this deposit offers valuable insights and strategic directions for the broader understanding of Zenong Group volcanic rocks across the central Lhasa terrane. Additionally, subsequent strategies have been proposed for mineral exploration at both Xinlong camp and regional scales.</p></div>","PeriodicalId":16336,"journal":{"name":"Journal of Geochemical Exploration","volume":null,"pages":null},"PeriodicalIF":3.4000,"publicationDate":"2024-03-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Identifying high potential gold mineralization using geological and stream sediment geochemical data: A case study from western Dangreyongcuo area in the central Lhasa terrane, Tibet, China\",\"authors\":\"Qingping Liu , Wei Chen , Juxing Tang , Yang Song , Jianzhen Zhang , Tengfei Liu , Qiang Wang , Zhuangzhuang Song\",\"doi\":\"10.1016/j.gexplo.2024.107454\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Northern Tibet exhibits abundant placer gold deposits, with a longstanding history of mining activities. Despite the widespread placer gold occurrences, the reports on the primary rock gold deposits or occurrences remain scarce. The central Lhasa terrane in northern Tibet hosts well-developed Zenong Group volcanic rocks, indicating great potential for the exploration of porphyry-epithermal copper (gold) deposits. Here, we select the Dangreyongcuo area in this region to investigate its metallogenetic potentiality, through a comprehensive 1:50,000 stream sediment geochemical survey, analyzing 12 elements (Au, As, Sb, Ag, Te, Cu, Pb, Zn, W, Sn, Bi, and Mo), and a detailed geological mapping. We aim to identify gold-related mineralization anomalies and provide clues for further bedrock gold exploration in this region. Based on the stream sediment geochemical data, zones 1–4, have been delineated using single-element indicator Au and element association indicator Au + As + Sb, which was determined through robust principal component analysis (RPCA) and using the exploratory data analysis (EDA) method. Subsequent validation exercises evaluating these four delineated zones reveal that Zone 1, Xinlong-Langmeila area, is the most promising prospect due to its high element concentrations, large size, and marked coincidence of element assemblages (also referred to as high-large-coincidence anomalies; HLCAs) and its characteristics are in line with those of epithermal deposits. Notably, the Xinlong deposit represents the first documented epithermal gold deposit hosted within the Zenong Group volcanic rocks. The identification of this deposit offers valuable insights and strategic directions for the broader understanding of Zenong Group volcanic rocks across the central Lhasa terrane. 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引用次数: 0
摘要
藏北蕴藏着丰富的块状金矿,采矿活动历史悠久。尽管块金矿分布广泛,但有关原生岩金矿床或矿点的报道仍然很少。藏北拉萨中部地层蕴藏着发育良好的增农群火山岩,显示出勘探斑岩热液型铜(金)矿床的巨大潜力。在此,我们选择了该地区的当惹雍错地区,通过全面的 1:50,000 溪流沉积物地球化学调查,分析 12 种元素(Au、As、Sb、Ag、Te、Cu、Pb、Zn、W、Sn、Bi 和 Mo),并绘制详细的地质图,研究其成矿潜力。我们旨在确定与金有关的矿化异常,为该地区进一步的基岩金勘探提供线索。根据溪流沉积物地球化学数据,使用单元素指标 Au 和元素关联指标 Au + As + Sb(通过稳健主成分分析 (RPCA) 和探索性数据分析 (EDA) 方法确定)划分了 1-4 区。随后的验证工作对这四个划分的区域进行了评估,结果表明,1 区(新龙-郎美拉区域)是最有前景的区域,因为该区域元素浓度高、规模大、元素组合明显重合(也称为高大重合异常;HLCAs),其特征与热液矿床的特征一致。值得注意的是,鑫隆矿床是首个被记录在案的、赋存于禅农组火山岩中的热液型金矿床。该矿床的发现为更广泛地了解整个拉萨中部地层的禅荣组火山岩提供了宝贵的见解和战略方向。此外,还为新龙营地和区域范围内的矿产勘探提出了后续战略。
Identifying high potential gold mineralization using geological and stream sediment geochemical data: A case study from western Dangreyongcuo area in the central Lhasa terrane, Tibet, China
Northern Tibet exhibits abundant placer gold deposits, with a longstanding history of mining activities. Despite the widespread placer gold occurrences, the reports on the primary rock gold deposits or occurrences remain scarce. The central Lhasa terrane in northern Tibet hosts well-developed Zenong Group volcanic rocks, indicating great potential for the exploration of porphyry-epithermal copper (gold) deposits. Here, we select the Dangreyongcuo area in this region to investigate its metallogenetic potentiality, through a comprehensive 1:50,000 stream sediment geochemical survey, analyzing 12 elements (Au, As, Sb, Ag, Te, Cu, Pb, Zn, W, Sn, Bi, and Mo), and a detailed geological mapping. We aim to identify gold-related mineralization anomalies and provide clues for further bedrock gold exploration in this region. Based on the stream sediment geochemical data, zones 1–4, have been delineated using single-element indicator Au and element association indicator Au + As + Sb, which was determined through robust principal component analysis (RPCA) and using the exploratory data analysis (EDA) method. Subsequent validation exercises evaluating these four delineated zones reveal that Zone 1, Xinlong-Langmeila area, is the most promising prospect due to its high element concentrations, large size, and marked coincidence of element assemblages (also referred to as high-large-coincidence anomalies; HLCAs) and its characteristics are in line with those of epithermal deposits. Notably, the Xinlong deposit represents the first documented epithermal gold deposit hosted within the Zenong Group volcanic rocks. The identification of this deposit offers valuable insights and strategic directions for the broader understanding of Zenong Group volcanic rocks across the central Lhasa terrane. Additionally, subsequent strategies have been proposed for mineral exploration at both Xinlong camp and regional scales.
期刊介绍:
Journal of Geochemical Exploration is mostly dedicated to publication of original studies in exploration and environmental geochemistry and related topics.
Contributions considered of prevalent interest for the journal include researches based on the application of innovative methods to:
define the genesis and the evolution of mineral deposits including transfer of elements in large-scale mineralized areas.
analyze complex systems at the boundaries between bio-geochemistry, metal transport and mineral accumulation.
evaluate effects of historical mining activities on the surface environment.
trace pollutant sources and define their fate and transport models in the near-surface and surface environments involving solid, fluid and aerial matrices.
assess and quantify natural and technogenic radioactivity in the environment.
determine geochemical anomalies and set baseline reference values using compositional data analysis, multivariate statistics and geo-spatial analysis.
assess the impacts of anthropogenic contamination on ecosystems and human health at local and regional scale to prioritize and classify risks through deterministic and stochastic approaches.
Papers dedicated to the presentation of newly developed methods in analytical geochemistry to be applied in the field or in laboratory are also within the topics of interest for the journal.