U–Pb LA-ICP-MS geochronology of polygenetic zircons from Beshta and Kamenistaya intrusions (the Greater Caucasus)

Author:

Shengelia DavidORCID,Shumlyanskyy LeonidORCID,Chichinadze GiorgiORCID,Tsutsunava TamaraORCID,Beridze GiorgiORCID,Javakhishvili IrakliORCID

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology

Reference39 articles.

1. Adamia Sh (1984) Pre-Alpine basement of the Caucasus—composition, structure, formation. In: Otkhmezuri Z (ed) Tectonics and metallogeny of the Caucasus. Metsniereba, Tbilisi, pp 1–104 (in Russian)

2. Baranov G, Grekov I (1982) Geodynamic model of the Greater Caucasus. In: Muratov M (ed) Problems of the geodynamics of the Caucasus. Nauka, Moscow, pp 51–59 (in Russian)

3. Baranov G, Kropachov S (1976) Stratigraphy, magmatism and tectonics of the Greater Caucasus Precambrian and Paleozoic stages. Nedra, Moscow

4. Belousova E, Griffin WL, O’Reilly SY, Fisher NL (2002) Igneous zircon: trace element composition as an indicator of source rock type. Contrib Mineral Petrol 143:602–622. https://doi.org/10.1007/s00410-002-0364-7

5. Bouvier A, Vervoort JD, Patchett PJ (2008) The Lu-Hf and Sm-Nd isotopic composition of CHUR: constraints from unequilibrated chondrites and implication for the bulk composition of terrestrial planets. Earth Planet Sci Lett 273:48–57. https://doi.org/10.1016/j.epsl.2008.06.010

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