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The oldest crustal rocks are missing primarily due to geological processes such as subduction and erosion. Subduction zones lead to the recycling of oceanic crust into the mantle, while continental crust can be eroded over billions of years, removing evidence of its oldest formations. Additionally, tectonic activity, such as continental drift and mountain building, can also obscure or destroy ancient rocks. Consequently, the oldest rocks we have are typically found in stable continental shields, where they have survived these dynamic processes.

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