Qingqing Yin , Juxing Tang , Qiuming Pei , Inna Safonova , Xinkui Xiang , Jingjing Dai , Aorigele Zhou , Bin Lin , Yumin Xu , Zhendong Yu , Jinling Xie , Ruihua Lin , Bo Peng , Liqiang Wang
{"title":"A vertical reverse zoning in the Kunshan W-Mo-Cu deposit, South China: Insights from mineral paragenesis, zircon geochemistry and S-Pb-O isotopes","authors":"Qingqing Yin , Juxing Tang , Qiuming Pei , Inna Safonova , Xinkui Xiang , Jingjing Dai , Aorigele Zhou , Bin Lin , Yumin Xu , Zhendong Yu , Jinling Xie , Ruihua Lin , Bo Peng , Liqiang Wang","doi":"10.1016/j.gr.2025.03.004","DOIUrl":null,"url":null,"abstract":"<div><div>The identification of reverse zoning in tungsten deposits is crucial, as it represents an atypical distribution of orebodies that may affect exploration and mining strategies. However, the exploration of such deposits remains challengeable due to uncertainties regarding the parageneses of polymetallic mineralization, the upper temperature limit of the formation of wolframite, and the evolutionary path of fluids, all of which influence the patterns of the distribution of ore mineralization. Recently, we have found that the Kunshan W-Mo-Cu deposit situated within the world-class Dahutang tungsten ore district in the middle segment of the Jiangnan Orogen, South China, is special for the vertical reverse zoning of W-Mo-Cu paragenetic mineralization. To trace the evolutionary paths of magmatic and deuteric hydrothermal fluids, estimate the redox conditions of magma crystallization, and determine the sources and temperatures of ore-forming fluids, we conducted a comprehensive study of the geochemical compositions of zircons and the S-Pb-O isotope systematics of quartz, wolframite and sulfide. We investigated the relationships between trace elements, oxygen fugacity (ƒ<sub>O2</sub>) and W-Mo-Cu parageneses, as well as the degree of contamination of parental magma by overlying metasediments. Our results indicate that the paragenetic W-Mo-Cu mineralization was triggered by a moderately reduced initial magma (ΔFMQ = −0.55 ∼ -0.20) containing 41 % <em>meta</em>-igneous-dominated component (δ<sup>18</sup>O<sub>magma</sub> = +9.2 ‰) and metasediments (δ<sup>18</sup>O<sub>WR</sub> = +12.6 ‰). The vertical reverse zoning is characterized by proximal Cu mineralization located beneath the distal high-temperature (394 °C) tungsten mineralization zone and was formed by volatile-rich fluids within an open metallogenic system. We argue that the exploration of deposits with vertical reverse zoning should continue, despite the decrease in the grade of tungsten ore with depth, while the content of metal sulfides may likewise increase.</div></div>","PeriodicalId":12761,"journal":{"name":"Gondwana Research","volume":"142 ","pages":"Pages 236-251"},"PeriodicalIF":7.2000,"publicationDate":"2025-04-03","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/S1342937X25000863","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 0
Abstract
The identification of reverse zoning in tungsten deposits is crucial, as it represents an atypical distribution of orebodies that may affect exploration and mining strategies. However, the exploration of such deposits remains challengeable due to uncertainties regarding the parageneses of polymetallic mineralization, the upper temperature limit of the formation of wolframite, and the evolutionary path of fluids, all of which influence the patterns of the distribution of ore mineralization. Recently, we have found that the Kunshan W-Mo-Cu deposit situated within the world-class Dahutang tungsten ore district in the middle segment of the Jiangnan Orogen, South China, is special for the vertical reverse zoning of W-Mo-Cu paragenetic mineralization. To trace the evolutionary paths of magmatic and deuteric hydrothermal fluids, estimate the redox conditions of magma crystallization, and determine the sources and temperatures of ore-forming fluids, we conducted a comprehensive study of the geochemical compositions of zircons and the S-Pb-O isotope systematics of quartz, wolframite and sulfide. We investigated the relationships between trace elements, oxygen fugacity (ƒO2) and W-Mo-Cu parageneses, as well as the degree of contamination of parental magma by overlying metasediments. Our results indicate that the paragenetic W-Mo-Cu mineralization was triggered by a moderately reduced initial magma (ΔFMQ = −0.55 ∼ -0.20) containing 41 % meta-igneous-dominated component (δ18Omagma = +9.2 ‰) and metasediments (δ18OWR = +12.6 ‰). The vertical reverse zoning is characterized by proximal Cu mineralization located beneath the distal high-temperature (394 °C) tungsten mineralization zone and was formed by volatile-rich fluids within an open metallogenic system. We argue that the exploration of deposits with vertical reverse zoning should continue, despite the decrease in the grade of tungsten ore with depth, while the content of metal sulfides may likewise increase.
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''.