U-Pb dating, oxygen and hafnium isotopic ratios of zircon from rocks of oceanic core complexes at Mid-Atlantic Ridge: evidence for an interaction of young and ancient crusts at spreading of the ocean floor
- Authors: Bortnikov N.S.1, Silantiev S.А.2, Bea F.3, Montero P.3, Zinger T.F.4, Skolotnev S.G.5, Sharkov E.V.1
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Affiliations:
- Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry of the Russian Academy of Sciences
- Vernadsky Institute of Geochemistry and Analytical Chemistry of the Russian Academy of Sciences
- University of Granada
- Institute of Precambrian Geology and Geochronology of the Russian Academy of Sciences
- Geological Institute of the Russian Academy of Sciences
- Issue: Vol 489, No 5 (2019)
- Pages: 483-489
- Section: Geology
- URL: https://journals.eco-vector.com/0869-5652/article/view/18843
- DOI: https://doi.org/10.31857/S0869-56524895483-489
- ID: 18843
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Abstract
U-Pb age, oxygen and hafnium isotopic ratios in zircon from rocks of ocean core complexes at Mid-Atlantic Ridge have been studied using SHRIMP and MC-LA-ICP-MS techniques. U-Pb dating revealed four group of zircons: 1) 0,6-1,7 Ma, 2) 6,7-11,2 Ma, 3) 12,9-17,6 Ma, 4) ≥200 to 2044 Ma. The δ18O values range from 4,74 to 7,2‰ and are distinct for zircon grains of different ages. Hafnium isotopic ratio for zircon aged from 0,6 to 17,6 Ma corresponds or is close to that of MORB from Central Atlantic. The oxygen and hafnium isotopic compositions of zircon elder than 280 Ma correspond to those of the sialic continental crust. A hypothesis of involvement of the ancient “pre-Atlantic” sialic (≥280 млн лет) and “old Atlantic” (7-17 Ma) crusts in a generation of the contemporary (“young”) oceanic crust during formation of the slow-spreading Mid-Atlantic Ridge has been proposed.
About the authors
N. S. Bortnikov
Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry of the Russian Academy of Sciences
Email: silantyev@geokhi.ru
Academician of the Russian Academy of Sciences
Russian Federation, 35, Staromonetny, Moscow, 119017S. А. Silantiev
Vernadsky Institute of Geochemistry and Analytical Chemistry of the Russian Academy of Sciences
Author for correspondence.
Email: silantyev@geokhi.ru
Russian Federation, 19, Kosygin street, Moscow, 119991
F. Bea
University of Granada
Email: silantyev@geokhi.ru
Foreign Member of the Russian Academy of Sciences
Spain, Avda. del Hospicio, Granada, 18010P. Montero
University of Granada
Email: silantyev@geokhi.ru
Spain, Avda. del Hospicio, Granada, 18010
T. F. Zinger
Institute of Precambrian Geology and Geochronology of the Russian Academy of Sciences
Email: silantyev@geokhi.ru
Russian Federation, 2, Makarova embankment, St.Petersburg, 199034
S. G. Skolotnev
Geological Institute of the Russian Academy of Sciences
Email: silantyev@geokhi.ru
Russian Federation, 7, Pyzhevsky lane, Moscow, 119017
E. V. Sharkov
Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry of the Russian Academy of Sciences
Email: silantyev@geokhi.ru
Russian Federation, 35, Staromonetny, Moscow, 119017
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