2010
DOI: 10.1130/g31219.1
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Mesoarchean subduction processes: 2.87 Ga eclogites from the Kola Peninsula, Russia

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Cited by 144 publications
(81 citation statements)
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“…, Sajeev et al, 2007;Santosh et al, 2009aSantosh et al, , 2012Shimizu et al, 2013a, b;Iwamura et al, 2013 CO 2 , Tsunogae et al, 2002Tsunogae et al, , 2008aOhyama et al, 2008-Satish-Kumar et al, 2002Nakano et al, 2011 TiO 2 Kawasaki and Motoyoshi, 2016TIMS Asami et al, 1998Grew et al, 2001;Osanai et al, 2001a;Suzuki et al, 2001Suzuki et al, , 2006, Santosh et al, 2006aMiyamoto et al, 2006;Hokada and Motoyoshi, 2006 2000 SHRIMP LA-ICP-MS EPMA 2010 Baba et al, 2010Baba et al, , 2012Sajeev et al, 2010;Sato et al, 2010;Bose et Liu et al, 2012;Santosh et al, 2012;Koizumi et al, 2014;Santosh et al, 2014;Yang et al, 2014a, b;Takamura et al, 2015;Hokada et al, 2016;Osanai et al, 2016a, b;Owada et al, 2016 --25 -2.5 Ga ; , Osanai et al, 1999a;Hokada et al, 2004, 1.9 Ga ;, Baba, 1998, Baba et al, 2012Santosh et al, 2012 25 40 km , Mints et al, 2010;…”
Section: °C 1 Gpamentioning
confidence: 99%
“…, Sajeev et al, 2007;Santosh et al, 2009aSantosh et al, , 2012Shimizu et al, 2013a, b;Iwamura et al, 2013 CO 2 , Tsunogae et al, 2002Tsunogae et al, , 2008aOhyama et al, 2008-Satish-Kumar et al, 2002Nakano et al, 2011 TiO 2 Kawasaki and Motoyoshi, 2016TIMS Asami et al, 1998Grew et al, 2001;Osanai et al, 2001a;Suzuki et al, 2001Suzuki et al, , 2006, Santosh et al, 2006aMiyamoto et al, 2006;Hokada and Motoyoshi, 2006 2000 SHRIMP LA-ICP-MS EPMA 2010 Baba et al, 2010Baba et al, , 2012Sajeev et al, 2010;Sato et al, 2010;Bose et Liu et al, 2012;Santosh et al, 2012;Koizumi et al, 2014;Santosh et al, 2014;Yang et al, 2014a, b;Takamura et al, 2015;Hokada et al, 2016;Osanai et al, 2016a, b;Owada et al, 2016 --25 -2.5 Ga ; , Osanai et al, 1999a;Hokada et al, 2004, 1.9 Ga ;, Baba, 1998, Baba et al, 2012Santosh et al, 2012 25 40 km , Mints et al, 2010;…”
Section: °C 1 Gpamentioning
confidence: 99%
“…Belomorian tectonic province; Mints et al, 2010) to Cenozoic (e.g. Himalayas; Liu and Zhong, 1997), are important indicators of plate convergence and collision following the subduction of oceanic or continental crust (O'Brien and Rötzler, 2003;Ernst and Liou, 2008).…”
Section: Introductionmentioning
confidence: 99%
“…Archaean rocks predominate in the northeast, and include tonalitetrondhjemite-granodiorite (TTG) suites, subordinate greenstone belts and paragneisses, yielding ages mainly between 2.9 and 2.7 Ga (Hölta et al, 2008 and references therein). High-grade metamorphic events recorded in these rocks include 2.9-2.7 Ga, eclogite-or granulitefacies metamorphism, as well as younger, c. 1.9 Ga, highgrade metamorphic overprinting Mints et al, 2010;Skublov et al, 2011), related to Fennoscandian reamalgamation.…”
Section: Figure 1 Fennoscandia and Its Location Within The East Euromentioning
confidence: 97%