New insights on the geochemical affinity and age of mineralized rocks in Timok magmatic complex, East Serbia

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New insights on the geochemical affinity and age of mineralized rocks in Timok magmatic complex, East Serbia. / Velojić, Miloš; Klimentyeva, Dina; Von Quadt, Albrecht et al.
In: Geoloski Anali Balkanskoga Poluostrva, Vol. 84.2023, No. 1, 07.2023, p. 47-63.

Research output: Contribution to journal › Article › Research › peer-review

Harvard

Velojić, M, Klimentyeva, D, Von Quadt, A, Guillong, M, Melcher, F, Meisel, T & Prelević, D 2023, 'New insights on the geochemical affinity and age of mineralized rocks in Timok magmatic complex, East Serbia', Geoloski Anali Balkanskoga Poluostrva, vol. 84.2023, no. 1, pp. 47-63. https://doi.org/10.2298/GABP230330004V

APA

Velojić, M., Klimentyeva, D., Von Quadt, A., Guillong, M., Melcher, F., Meisel, T., & Prelević, D. (2023). New insights on the geochemical affinity and age of mineralized rocks in Timok magmatic complex, East Serbia. Geoloski Anali Balkanskoga Poluostrva, 84.2023(1), 47-63. https://doi.org/10.2298/GABP230330004V

Vancouver

Velojić M, Klimentyeva D, Von Quadt A, Guillong M, Melcher F, Meisel T et al. New insights on the geochemical affinity and age of mineralized rocks in Timok magmatic complex, East Serbia. Geoloski Anali Balkanskoga Poluostrva. 2023 Jul;84.2023(1):47-63. doi: 10.2298/GABP230330004V

Author

Velojić, Miloš ; Klimentyeva, Dina ; Von Quadt, Albrecht et al. / New insights on the geochemical affinity and age of mineralized rocks in Timok magmatic complex, East Serbia. In: Geoloski Anali Balkanskoga Poluostrva. 2023 ; Vol. 84.2023, No. 1. pp. 47-63.

Bibtex - Download

@article{51cc97224170422e8ff97b7f88b6c9db,
title = "New insights on the geochemical affinity and age of mineralized rocks in Timok magmatic complex, East Serbia",
abstract = "Bor and {\v C}ukaru Peki are world-class porphyry deposits spatiallyand genetically associated with the Cretaceous Timok magmatic complex. Thisresearch was conducted to determine the age and geochemical affinity of themagmatic rocks that formed these ore deposits. Our new geochemical analysesof magmatic rocks from Bor and {\v C}ukaru Peki deposits imply they compriseadakite-like compositions that have undergone the amphibole fractionationand sulphide saturation processes. The zircon ages indicate that the Bor systemwas formed in the age span between 84.5–82 Ma, while the {\v C}ukaru Pekisystem was created in the age span between 86.5–85 Ma.",
keywords = "adakites, Bor, Bor metallogenic zone, porphyry, zircons, {\v C}ukaru Peki",
author = "Milo{\v s} Veloji{\'c} and Dina Klimentyeva and {Von Quadt}, Albrecht and Marcel Guillong and Frank Melcher and Thomas Meisel and Dejan Prelevi{\'c}",
note = "Publisher Copyright: {\textcopyright} 2023, Geoloski Anali Balkanskoga Poluostrva. All Rights Reserved.",
year = "2023",
month = jul,
doi = "10.2298/GABP230330004V",
language = "English",
volume = "84.2023",
pages = "47--63",
journal = "Geoloski Anali Balkanskoga Poluostrva",
issn = "0350-0608",
number = "1",

}

RIS (suitable for import to EndNote) - Download

TY - JOUR

T1 - New insights on the geochemical affinity and age of mineralized rocks in Timok magmatic complex, East Serbia

AU - Velojić, Miloš

AU - Klimentyeva, Dina

AU - Von Quadt, Albrecht

AU - Guillong, Marcel

AU - Melcher, Frank

AU - Meisel, Thomas

AU - Prelević, Dejan

N1 - Publisher Copyright: © 2023, Geoloski Anali Balkanskoga Poluostrva. All Rights Reserved.

PY - 2023/7

Y1 - 2023/7

N2 - Bor and Čukaru Peki are world-class porphyry deposits spatiallyand genetically associated with the Cretaceous Timok magmatic complex. Thisresearch was conducted to determine the age and geochemical affinity of themagmatic rocks that formed these ore deposits. Our new geochemical analysesof magmatic rocks from Bor and Čukaru Peki deposits imply they compriseadakite-like compositions that have undergone the amphibole fractionationand sulphide saturation processes. The zircon ages indicate that the Bor systemwas formed in the age span between 84.5–82 Ma, while the Čukaru Pekisystem was created in the age span between 86.5–85 Ma.

AB - Bor and Čukaru Peki are world-class porphyry deposits spatiallyand genetically associated with the Cretaceous Timok magmatic complex. Thisresearch was conducted to determine the age and geochemical affinity of themagmatic rocks that formed these ore deposits. Our new geochemical analysesof magmatic rocks from Bor and Čukaru Peki deposits imply they compriseadakite-like compositions that have undergone the amphibole fractionationand sulphide saturation processes. The zircon ages indicate that the Bor systemwas formed in the age span between 84.5–82 Ma, while the Čukaru Pekisystem was created in the age span between 86.5–85 Ma.

KW - adakites

KW - Bor

KW - Bor metallogenic zone

KW - porphyry

KW - zircons

KW - Čukaru Peki

UR - http://www.scopus.com/inward/record.url?scp=85168588427&partnerID=8YFLogxK

U2 - 10.2298/GABP230330004V

DO - 10.2298/GABP230330004V

M3 - Article

AN - SCOPUS:85168588427

VL - 84.2023

SP - 47

EP - 63

JO - Geoloski Anali Balkanskoga Poluostrva

JF - Geoloski Anali Balkanskoga Poluostrva

SN - 0350-0608

IS - 1

ER -

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