In geology, platform sediments can be classified into the following groups: a "protoplatform" of metamorphosed sediments at the bottom, a "quasiplatform" of slightly deformed sediments, a "cataplatform", and an "orthoplatform" at the top.
The Mesoproterozoic Jotnian sediments of the Baltic area are examples of a "quasiplatform".
[1] The post-Ordovician rocks of the South American Platform are examples of an orthoplatform.
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Oceanic crust
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0–20
Ma
20–65
Ma
>65
Ma
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