Trace element composition and Lu-Hf isotope systematics of zircon from plagiogneisses of the Kola superdeep well: Contribution of a Paleoarchean crust in Mesoarchean metavolcanic rocks

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• 作者：V. R. Vetrin ; E. A. Belousova ; V. P. Chupin
• 关键词：Kola superdeep well ; Mesoarchean volcanic rocks ; zircon ; trace elements ; Lu ; Hf systematics ; Paleoarchean crust
• 刊名：Geochemistry International
• 出版年：2016
• 出版时间：January 2016
• 年：2016
• 卷：54
• 期：1
• 页码：92-111
• 全文大小：2,769 KB
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• 作者单位：V. R. Vetrin (1)
  E. A. Belousova (2)
  V. P. Chupin (3) (4)
  
  1. Geological Institute, Kola Science Center, Russian Academy of Sciences, ul. Fersmana 14, Apatity, 184209, Russia
  2. NSW 2109, Macquarie University, Department of Earth and Planetary Sciences, Faculty of Science, Sydney, Australia
  3. Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, pr. Akad. Koptyuga 3, Novosibirsk, 630090, Russia
  4. Novosibirsk State University, ul. Pirogova 2, Novosibirsk, 630090, Russia
  
• 刊物主题：Geochemistry;
• 出版者：Springer US
• ISSN：1556-1968

文摘

Zircons have been studied in three samples of Archean plagiogneisses from the Kola superdeep well (SG-3). The crystals consist of cores, magmatic shells, and metamorphic rims. The cores and shells are characterized by similar lowered concentrations of most trace elements, which is typical of zircons from plagiogranitoids, rocks of elevated basicity, and basites. At a wide range of Hf isotope characteristics, the cores and shells have similar average 176Hf/177Hf_i, which determines the close composition of their sources. The metamorphic rims have close 176Hf/177Hf_i ratio. The minimum age of the crustal contaminant of parental melts is estimated at 3.4 and 3.3 Ga for cores and 3.3–3.2 Ga for shells at almost equal proportions of mantle and crustal components in them. The contribution of Paleoarchean crust established in zircons from plagiogneisses of SG-3 using Lu-Hf isotope systematics is confirmed by the presence of 3.3and 3.4-Ga old zircons in surrounding TTG. Keywords Kola superdeep well Mesoarchean volcanic rocks zircon trace elements Lu-Hf systematics Paleoarchean crust