Isotopic dates of anorthosites from the Moon and meteorites indicate that the age of the Solar System is about 4.6 b.y. Modal lead ages of volcanic rocks and ores suggest that the age of the Earth is 4.55 to 4.6 b.y.; thus the major melting and crustal-forming events...
CITATION STYLE
Emery, K. O., & Uchupi, E. (1984). The SYN-RIFT Supersequence and Crustal Boundary. In The Geology of the Atlantic Ocean (pp. 263–367). Springer New York. https://doi.org/10.1007/978-1-4612-5278-8_4
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