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

Acta Geochimica 2022年第6期41卷 1019-1029页

作者： David Shengelia Leonid Shumlyanskyy Giorgi Chichinadze Tamara Tsutsunava Giorgi Beridze Irakli Javakhishvili Al.Janelidze Institute of Geology of Iv.Javakhishvili Tbilisi State University TbilisiGeorgia School of Earth and Planetary Sciences Curtin UniversityPerthAustralia M.P.Semenenko Institute of Geochemistry Mineralogy and Ore FormationKyivUkraine

The Beshta-Kamenistaya intrusions are located in the Main Range structural zone of the greater *** are composed of tonalitic gneisses that genetically resemble granites of the tholeiitic series of the ophiolitic *** Beshta-Kamenistaya orthogneisses and associated rocks of the nappes differ markedly from those of the Main Range *** of them were overthrust to the Main Range zone during the Bretonian *** age of their protolith and the metamorphism are still not *** the zircon U-Pb LA-ICP-MS dating two age populations of zircons have been distinguished in the rocks of the Beshta-Kamenistaya *** age of the main population of zircons from orthogneisses is 426-300 *** age groups can be distinguished in this *** main group yielded a Concordia age of386.9±1.4 *** are also smaller peaks at 409-405,375-373,and 351 *** oldest ages(426-395 Ma)were detected in the core parts of the complex *** assume that the crystallization of the parental for orthogneisses rocks(tonalities)took place at 410-395 Ma,whereas the Concordia age of 386.9±1.4 Ma and a peak at 375-373 Ma correspond to the metamorphic *** whole metamorphic cycle,including progressive and regressive stages,occurred between 395 and 370 ***,dated in the Beshta-Kamenistaya intrusion at350 Ma and younger,correspond to the Late Variscan *** dated 3102-2769 Ma represent xenocrysts captured by the melts during their formation from the ancient rocks in the crystalline basement.

关键词： the greater caucasus Magmatism Metamorphism Orthogneisses U–Pb zircon dating

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