Biaobiao Zhu , Yongzhang Zhou , Changyu Zeng , Xinhui Yu , Zhengzhe Wang , Shengtao Cao , Pengpeng Yu
{"title":"Data-driven mining reveals a cross-temperature correlation between gold and tungsten: implications for magmatic controls in Carlin-type gold deposits","authors":"Biaobiao Zhu , Yongzhang Zhou , Changyu Zeng , Xinhui Yu , Zhengzhe Wang , Shengtao Cao , Pengpeng Yu","doi":"10.1016/j.gr.2025.12.001","DOIUrl":null,"url":null,"abstract":"<div><div>Nevada (USA) and the Youjiang Basin (China) are the two largest Carlin-type gold provinces in the world, despite their distinct geological frameworks. The magmatic-hydrothermal model provides a credible explanation for Nevada’s deposits, but the apparent magmatic absence of magmatic rocks in the Youjiang Basin challenges it. To elucidate this enigmatic phenomenon, We integrated 2,210 catchment-derived stream-sediment samples from the Youjiang Basin with 54 lithogeochemical samples from Nevada’s Getchell district, and applied an innovative association-rule graph analysis method.Two findings are revealed: (1) The Au-As-Sb triad constitutes a diagnostic geochemical fingerprint for Carlin-type gold deposits. Metal enrichments (Cu, Mo, Co, Cr, Pb, Zn) exhibit strong co-precipitation with Au anomalies (support = 0.10, confidence = 0.90), indicative of element migration coupled with gold mineralization processes. (2) Topological coupling between low-temperature Au-As-Sb and high-temperature W anomalies is quantitatively established in both regions (support > 0.20, confidence > 0.90), implying a cross-temperature correlation. The magmatic-hydrothermal model can explain the Au-W correlation in Nevada. Thus, the correlation for the Youjiang may also imply a magmatic origin. This is evidenced by the following clues: Hg isotopes indicating a mixture of magmatic and basement-derived sources for Au, deep buried granite bodies temporally overlapping with gold mineralization. Combined with previous studies, we proposed a common magma-driven metallogenic model for Carlin-type deposits: The rising Au-W-bearing magmatic hydrothermal fluids mixed with the magmatically heated meteoric fluids that leached Au from the basement rocks, and subsequently precipitated Au-As-Sb-Hg-rich pyrite and W-bearing mineral assemblages within the carbonate host formations. In this context, the majority of gold is sourced from magmas for Nevada subtype and both of magmas and basement for the Youjiang subtype, respectively. This study highlights data-driven recognition of magmatic signature in sediment-hosted gold systems and establishes a new paradigm for the understanding of metallogenic architecture.</div></div>","PeriodicalId":12761,"journal":{"name":"Gondwana Research","volume":"153 ","pages":"Pages 253-264"},"PeriodicalIF":8.9000,"publicationDate":"2026-05-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Gondwana Research","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1342937X25003806","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"2025/12/25 0:00:00","PubModel":"Epub","JCR":"Q1","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0
Abstract
Nevada (USA) and the Youjiang Basin (China) are the two largest Carlin-type gold provinces in the world, despite their distinct geological frameworks. The magmatic-hydrothermal model provides a credible explanation for Nevada’s deposits, but the apparent magmatic absence of magmatic rocks in the Youjiang Basin challenges it. To elucidate this enigmatic phenomenon, We integrated 2,210 catchment-derived stream-sediment samples from the Youjiang Basin with 54 lithogeochemical samples from Nevada’s Getchell district, and applied an innovative association-rule graph analysis method.Two findings are revealed: (1) The Au-As-Sb triad constitutes a diagnostic geochemical fingerprint for Carlin-type gold deposits. Metal enrichments (Cu, Mo, Co, Cr, Pb, Zn) exhibit strong co-precipitation with Au anomalies (support = 0.10, confidence = 0.90), indicative of element migration coupled with gold mineralization processes. (2) Topological coupling between low-temperature Au-As-Sb and high-temperature W anomalies is quantitatively established in both regions (support > 0.20, confidence > 0.90), implying a cross-temperature correlation. The magmatic-hydrothermal model can explain the Au-W correlation in Nevada. Thus, the correlation for the Youjiang may also imply a magmatic origin. This is evidenced by the following clues: Hg isotopes indicating a mixture of magmatic and basement-derived sources for Au, deep buried granite bodies temporally overlapping with gold mineralization. Combined with previous studies, we proposed a common magma-driven metallogenic model for Carlin-type deposits: The rising Au-W-bearing magmatic hydrothermal fluids mixed with the magmatically heated meteoric fluids that leached Au from the basement rocks, and subsequently precipitated Au-As-Sb-Hg-rich pyrite and W-bearing mineral assemblages within the carbonate host formations. In this context, the majority of gold is sourced from magmas for Nevada subtype and both of magmas and basement for the Youjiang subtype, respectively. This study highlights data-driven recognition of magmatic signature in sediment-hosted gold systems and establishes a new paradigm for the understanding of metallogenic architecture.
期刊介绍:
Gondwana Research (GR) is an International Journal aimed to promote high quality research publications on all topics related to solid Earth, particularly with reference to the origin and evolution of continents, continental assemblies and their resources. GR is an "all earth science" journal with no restrictions on geological time, terrane or theme and covers a wide spectrum of topics in geosciences such as geology, geomorphology, palaeontology, structure, petrology, geochemistry, stable isotopes, geochronology, economic geology, exploration geology, engineering geology, geophysics, and environmental geology among other themes, and provides an appropriate forum to integrate studies from different disciplines and different terrains. In addition to regular articles and thematic issues, the journal invites high profile state-of-the-art reviews on thrust area topics for its column, ''GR FOCUS''. Focus articles include short biographies and photographs of the authors. Short articles (within ten printed pages) for rapid publication reporting important discoveries or innovative models of global interest will be considered under the category ''GR LETTERS''.