Milos Velojic, D. Klimentyeva, Quadt von, M. Guillong, F. Melcher, T. Meisel, D. Prelević
{"title":"New insights on the geochemical affinity and age of mineralized rocks in Timok magmatic complex, East Serbia","authors":"Milos Velojic, D. Klimentyeva, Quadt von, M. Guillong, F. Melcher, T. Meisel, D. Prelević","doi":"10.2298/gabp230330004v","DOIUrl":null,"url":null,"abstract":"Bor and Cukaru Peki are world-class porphyry deposits spatially and\n genetically associated with the Cretaceous Timok magmatic complex. This\n research was conducted to determine the age and geochemical affinity of the\n magmatic rocks that formed these ore deposits. Our new geochemical analyses\n of magmatic rocks from Bor and Cukaru Peki deposits imply they comprise\n adakite-like compositions that have undergone the amphibole fractionation\n and sulphide saturation processes. The zircon ages indicate that the Bor\n system was formed in the age span between 84.5-82 Ma, while the Cukaru Peki\n system was created in the age span between 86.5-85 Ma.","PeriodicalId":378337,"journal":{"name":"Annales g?ologiques de la Peninsule balkanique","volume":"42 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Annales g?ologiques de la Peninsule balkanique","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.2298/gabp230330004v","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
Bor and Cukaru Peki are world-class porphyry deposits spatially and
genetically associated with the Cretaceous Timok magmatic complex. This
research was conducted to determine the age and geochemical affinity of the
magmatic rocks that formed these ore deposits. Our new geochemical analyses
of magmatic rocks from Bor and Cukaru Peki deposits imply they comprise
adakite-like compositions that have undergone the amphibole fractionation
and sulphide saturation processes. The zircon ages indicate that the Bor
system was formed in the age span between 84.5-82 Ma, while the Cukaru Peki
system was created in the age span between 86.5-85 Ma.
京公网安备 11010802042870号
京ICP备2023020795号-1
分享
求助内容：
应助结果提醒方式：
扫码关注我们
