Earth's early crust evolved from a mafic to a more felsic composition.
Is it true that Earth's early crust evolved from a mafic to a more felsic composition?
Yes. Geological evidence indicates that Earth's upper continental crust transitioned from a predominantly mafic composition to a more felsic composition following the Archean era.
Verdict: SUPPORTED · 3 sources for, 0 against · Last checked
Multiple high-impact studies using geochemical proxies, element ratios, and vanadium isotopes confirm the secular transition of Earth's crust from early mafic-dominated compositions to more felsic compositions over geological time.
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Tang, M., Chen, K., & Rudnick, R. L. (2016). Archean upper crust transition from mafic to felsic marks the onset of plate tectonics. doi.org. https://doi.org/10.1126/science.aad5513
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Xia, B., Artemieva, I., & Thybo, H. (2024). Phanerozoic emergence of global continental collision and onset of massive crustal eclogitization. doi.org. https://doi.org/10.1130/g52647.1
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Tian, S., Ding, X., Qi, Y., Wu, F., Cai, Y., Gaschnig, R. M., Xiao, Z., Lv, W., Rudnick, R. L., & Huang, F. (2023). Dominance of felsic continental crust on Earth after 3 billion years ago is recorded by vanadium isotopes.. doi.org. https://doi.org/10.1073/pnas.2220563120
What does the evidence say?
Multiple high-impact studies using geochemical proxies, element ratios, and vanadium isotopes confirm the secular transition of Earth's crust from early mafic-dominated compositions to more felsic compositions over geological time.
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