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RAS Earth ScienceГеология рудных месторождений Geology of Ore Deposits

  • ISSN (Print) 0016-7770
  • ISSN (Online) 3034-5073

U-Pb AGE AND ZIRCON GEOCHEMISTRY OF FERTILITY-REDUCED GRANITE ON EXAMPLE OF THE TAM DAO TIN ORE DISTRICT, NORTHEAST VIETNAM

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PII
S30345073S0016777025030053-1
DOI
10.7868/S3034507325030053
Publication type
Article
Status
Published
Authors
P. A. Nevolko
  • Affiliation: VS Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences
T. V. Svetlitskaya
  • Affiliation: VS Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences
Thi Dung Pham
  • Affiliation: Institute of Geological Sciences, Vietnam Academy of Science and Technology
The Hau Nguyen
  • Affiliation: Institute of Geological Sciences, Vietnam Academy of Science and Technology
Trong Hoa Tran
  • Affiliation: Institute of Geological Sciences, Vietnam Academy of Science and Technology
P. A. Fominykh
  • Affiliation: VS Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences
Thi Phuong Ngo
  • Affiliation: Institute of Geological Sciences, Vietnam Academy of Science and Technology
Volume/ Edition
Volume 67 / Issue number 3
Pages
337-375
Abstract
The Sn (-Cu) Tam Dao ore district is located at the southern margin of the South China Block within the Lo Gam structure at northeastern Vietnam. Genetically ore mineralization of the Tam Dao ore district is associated with the homonymous massif of biotite granites of the Pia Bioc complex Middle Triassic age and includes a number of different size tin deposits . The Ngoi Lem deposit (4700 tons of Sn and 300 tons of Cu) is the largest and most studied ones. Despite the widespread distribution of Early-Middle Triassic granitoid magmatism within the Lo Gam structure, tin mineralization was revealed only near the Tam Dao massif and practically does not appear around other massifs of the Phia Bioc complex. Zircon geochemical features from biotite granites of various massifs indicate the similarity of the oxygen fugacity and fractionation degree of the parental melts. The obtained zircon characteristics are fully consistent with realistic genetic models for tin deposits related with reduced intrusions. The partial melting temperature of the metasedimentary substrate is the reasons for the various metal fertility potential of coeval and geochemically similar granitoids. The relatively high zircon crystallization temperatures (~>780-800°C) of tin-bearing biotite granites of the Tam Dao imply that they were produced at a higher temperature by biotite-dehydration melting, which requires additional heat from the mantle. The interaction between ma c and granitic magmas led to the enrichment of acidic melts in copper. The low oxygen fugacity led the dominance of the sul de form of sulfur in melts, which in turn determined its low concentration. The low S/Cu ratio in the granite melt prevented crystallization and fractionation of sul des therefore the residual melts experienced some Cu enrichment. The proposed scenario of granite melt Cu saturation and the absence of its signi cant sul de fractionation explains the contradictory Sn-Cu metallogeny of the Tam Dao ore district. The new obtained features of the Early-Middle Triassic Pia Bioc granites propose key zircon geochemical indicators of tin fertility reduced granitic magma: (1) T~>780-800°C, (2) ΔFMQ
Keywords
гранит оловорудное месторождение U-Pb-датирование циркон геохимия индикаторы фертильности Там Дао Северо-Восточный Вьетнам
Date of publication
21.12.2025
Year of publication
2025
Number of purchasers
0
Views
63

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