What types of sedimentary rocks were rare in the Archean Eon? What does this suggest about the nature of cratons during Archean time?

The Archean Eon is a geological time period that spans from around 4 billion years ago to 2.5 billion years ago. During this time, the Earth's crust had just begun to stabilize, and the first continents were forming. The atmosphere was very different from today, containing high levels of carbon dioxide and very little oxygen.

During the Archean Eon, sedimentary rocks rich in silica, such as sandstones and shales, were rare. This is because the processes required to form these types of rocks, including weathering and erosion of continental crust, were not well established during this time period.

The reason for the scarcity of sandstones and shales during the Archean Eon is that weathering and erosion processes were not as prevalent. The lack of oxygen and high levels of carbon dioxide in the atmosphere, as well as the limited continental landmass, contributed to the rarity of these types of sedimentary rocks.

The rarity of silica-rich sedimentary rocks in the Archean Eon suggests that the nature of cratons during this time was quite different from what it is now. Cratons, which are the ancient, stable cores of continents, were likely smaller and composed primarily of mafic and ultramafic rocks, such as basalts and komatiites, rather than the granitic rocks that dominate modern continental crust. In conclusion, the scarcity of silica-rich sedimentary rocks like sandstones and shales during the Archean Eon reflects the unique nature of the Earth's crust and atmosphere during this time period. This scarcity also provides insight into the nature of cratons during the Archean, implying that they were predominantly composed of mafic and ultramafic rocks, as opposed to the granitic rocks that are characteristic of today's continents.