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B. Fu, T. P. Mernagh, N. T. Kita, A. I. S. Kemp and J. W. Valley, “Distinguishing Magmatic Zircon from Hydrothermal Zircon: A Case Study From the Gidginbung High-Sulphidation Au-Ag-(Cu) Deposit, SE Australia,” Chemical Geology, Vol. 259, 2009, pp. 131-142. doi:10.1016/j.chemgeo.2008.10.035

has been cited by the following article:

• TITLE: Early Proterozoic U-Pb Zircon Ages from Basement Gneiss at the Solovetsky Archipelago, White Sea, Russia

  AUTHORS: Stephan Schuth, Victor I. Gornyy, Jasper Berndt, Sergei S. Shevchenko, Alexandr F. Karpuzov, Tim Mansfeldt

  KEYWORDS: Solovetsky Archipelago; Granitic Gneiss Outcrop; Age Determination; 2.430 Ga

  JOURNAL NAME: International Journal of Geosciences, Vol.3 No.2, May 23, 2012

  ABSTRACT: The central region of the Neoarchaean Belomorian Mobile Belt (BMB) is, except for the Solovetsky Archipelago, largely covered by the White Sea. A newly discovered granitic gneiss outcrop on Solovetsky Island, Russia, enables a first age determination of the archipelago and evaluation of the hitherto poorly constrained central BMB. Zircons separated from the orthogneiss were analysed with SIMS-SHRIMP and LA-ICP-MS techniques. Both techniques yield a concordant U-Pb age of ca. 2.430 Ga, coinciding with ages of granitic intrusions in the BMB ca. 50 km west of the Solovetsky Islands.