Archean Crustal Evolution in the Ukrainian Shield

[1]  A. Antonov,et al.  The long (3.7–2.1 Ga) and multistage evolution of the Bug Granulite–Gneiss Complex, Ukrainian Shield, based on the SIMS U–Pb ages and geochemistry of zircons from a single sample , 2016, Special Publications.

[2]  M. Whitehouse,et al.  Can oxygen isotopes in magmatic zircon be modified by metamorphism? A case study from the Eoarchean Dniester-Bug Series, Ukrainian Shield , 2016 .

[3]  S. Claesson,et al.  Early crust of the Podolia Domain of the Ukrainian Shield: Isotopic age of terrigenous zircons from quartzites of the Bug Group , 2015, Stratigraphy and Geological Correlation.

[4]  M. V. Kranendonk,et al.  Oxygen isotopes in Pilbara Craton zircons support a global increase in crustal recycling at 3.2Ga , 2015 .

[5]  C. Hawkesworth,et al.  207Pb/206Pb ages and Hf isotope composition of zircons from sedimentary rocks of the Ukrainian shield: Crustal growth of the south-western part of East European craton from Archaean to Neoproterozoic , 2015 .

[6]  G. Artemenko,et al.  ПIЗHЬОПАЛЕОАРХЕЙСЬКI ТОНАЛIТОВI ГНЕЙСИ ЗАХIДНО-ПРИАЗОВСЬКОГО БЛОКА (ПРИАЗОВСЬКИЙ МЕГАБЛОК УКРАЇНСЬКОГО ЩИТА) , 2014 .

[7]  S. Sergeev,et al.  The Orekhov–Pavlograd Zone, Ukrainian Shield: Milestones of its evolutionary history and constraints for tectonic models , 2014 .

[8]  V. Balagansky,et al.  Metasedimentary rocks of the paleoarchean Dniester-Bug Group, Ukrainian Shield: Composition, age, and sources , 2014, Lithology and Mineral Resources.

[9]  G. Artemenko,et al.  ВІК ЗАЛІЗИСТО-КРЕМЕНИСТО-ВУЛКАНОГЕННОЇ ФОРМАЦІЇ ЧОРТОМЛИЦЬКОГО ЗАЛІЗОРУДНОГО РОДОВИЩА (СЕРЕДНЬОПРИДНІПРОВСЬКИЙ МЕГАБЛОК УКРАЇНСЬКОГО ЩИТА) , 2014 .

[10]  B. Dhuime,et al.  The oldest crust in the Ukrainian Shield – Eoarchaean U–Pb ages and Hf–Nd constraints from enderbites and metasediments , 2014 .

[11]  V. Starostenko,et al.  Late Palaeoproterozoic mafic dyking in the Ukrainian Shield of Volgo-Sarmatia caused by rotation during the assembly of supercontinent Columbia (Nuna) , 2013 .

[12]  M. V. Kranendonk,et al.  Long-lived, autochthonous development of the Archean Murchison Domain, and implications for Yilgarn Craton tectonics , 2013 .

[13]  S. Claesson,et al.  Isotope-geochronological (U-Th-Pb, Lu-Hf) study of the zircons from the archean magmatic and metasedimentary rocks of the Podolia domain, Ukrainian shield , 2013, Geochemistry International.

[14]  J. Moyen,et al.  Forty years of TTG research , 2012 .

[15]  M. Anosova,et al.  The early crust beneath the Azov Domain of the Ukrainian Shield: Isotopic-geochronological and geochemical investigations of detrital zircons from metasedimentary rocks of the Fedorovka structure , 2012, Stratigraphy and Geological Correlation.

[16]  V. V. Balaganskii,et al.  Composition and age of metaorthopyroxenite xenoliths and host enderbite gneisses in the Pobuzhie granulite complex, Ukrainian Shield , 2012, Doklady Earth Sciences.

[17]  E. B. Sal’nikova,et al.  The age of metamorphism of granulite complexes of the Voronezh crystalline massif: The monazite U-Pb geochronology , 2010 .

[18]  L. Ilyinsky,et al.  Early Archean crust of the Middle Dnepr and Azov domains, Ukrainian Shield—evidence from ages of detrital zircons in Mesoarchean greenstone belts , 2010, American Journal of Science.

[19]  I. Krylov,et al.  Late Archean magmatic complexes of the Azov terrane, Ukrainian Shield: Geological setting, isotopic age, and sources of material , 2008 .

[20]  A. Samsonov,et al.  Geodynamics of the eastern margin of Sarmatia in the Paleoproterozoic , 2007 .

[21]  C. D. Ignacio,et al.  Isotope geochemistry and FOZO mantle component of the alkaline-carbonatitic association of Fuerteventura, Canary Islands, Spain , 2006 .

[22]  S. Bogdanova,et al.  Archaean terranes, Palaeoproterozoic reworking and accretion in the Ukrainian Shield, East European Craton , 2006, Geological Society, London, Memoirs.

[23]  M. Basei,et al.  4.4 billion years of crustal maturation: oxygen isotope ratios of magmatic zircon , 2005 .

[24]  R. Garetsky,et al.  EUROPE | East European Craton , 2005 .

[25]  V. Chavagnac.  A geochemical and Nd isotopic study of Barberton komatiites (South Africa): implication for the Archean mantle , 2004 .

[26]  Stanislav S. Gornostayev,et al.  Evidence for the emplacement of ca. 3.0 Ga mantle-derived mafic-ultramafic bodies in the Ukrainian Shield , 2004 .

[27]  W. Griffin,et al.  Archean crustal evolution in the northern Yilgarn Craton: U–Pb and Hf-isotope evidence from detrital zircons , 2004 .

[28]  M. Murphy,et al.  International Stratigraphic Guide — An abridged version , 1999 .

[29]  S. Bogdanova,et al.  The Sarmatian crustal segment: Precambrian correlation between the Voronezh Massif and the Ukrainian Shield across the Dniepr-Donets Aulacogen , 1996 .

[30]  A. Nutman,et al.  Evolution of the Archaean Aulian Gneiss Complex, Middle Dnieper gneiss-greenstone terrain, Ukrainian Shield: SHRIMP UPb zircon evidence , 1996 .

[31]  D. Zhuravlev,et al.  Geochronology and Petrogenesis of the Archean Silicic Volcanoplutonic Series of the Verkhovtsevo Greenstone Structure, Ukraine , 1993 .

[32]  I. Williams,et al.  Ion microprobe U-Th-Pb isotopic studies of zircons from three early Precambrian areas in the U.S.S.R. , 1990 .

[33]  E. Bibikova.  The Most Ancient Rocks in the USSR Territory by U-Pb Data on Accessory Zircons , 1984 .