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• W2892593114 endingPage "253" @default.
• W2892593114 startingPage "239" @default.
• W2892593114 abstract "The oldest preserved terrestrial rocks occur as small blocks tectonically incorporated within younger orogens, most commonly Neoarchean in age. As more age data have become available, it is clear that almost every Archean Craton contains blocks with formation ages ≥3.4 Ga. These blocks are generally <500 km across and are separated from surrounding, mostly Archean, crust by shear zones. Even though the blocks are relatively small, their widespread distribution is consistent with, but does not demand, an original widespread distribution of pre-3 Ga continental crust, most of which was subsequently recycled back into the mantle." @default.
• W2892593114 created "2018-10-05" @default.
• W2892593114 creator A5013541003 @default.
• W2892593114 date "2019-01-01" @default.
• W2892593114 modified "2023-10-17" @default.
• W2892593114 title "Earth's Oldest Rocks and Minerals" @default.
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