In situ U-Pb dating of zircon formed from retrograde garnet breakdown during decompression in Rogaland, SW Norway
Regionally metamorphosed metapelites from Rogaland, SW Norway, contain zircon formed during the decompression reaction garnet + sillimanite + quartz → cordierite. The zircon, which occurs as inclusions in cordierite coronas around garnet, is texturally,
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|Source:||Journal of Metamorphic Geology|
|01_Tomkins_In_situ_U-Pb_dating_of_zircon_2005.pdf||665.31 kB||Adobe PDF||Request a copy|
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