Geological and macrostratigraphic evidence demonstrates that the relative proportions and compositions of igneous, sedimentary, and metamorphic rocks have continuously evolved throughout Earth's history due to shifting tectonic and magmatic processes.
The retrieved papers consistently support the idea that the relative abundance, distribution, and composition of major rock types (igneous, sedimentary, metamorphic) have varied over geological time as part of Earth's secular evolution and crustal recycling. Therefore, the claim is supported.