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This page is a summary of: Different zircon recrystallization types in carbonatites caused by magma mixing: Evidence from U–Pb dating, trace element and isotope composition (Hf and O) of zircons from two Precambrian carbonatites from Fennoscandia, Chemical Geology, August 2013, Elsevier,
DOI: 10.1016/j.chemgeo.2012.11.004.
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