How Old Is Planet Earth?
- 6 June 2003
- journal article
- perspective
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 300 (5625) , 1513-1514
- https://doi.org/10.1126/science.1080682
Abstract
Using a precise hafnium-tungsten "clock," three groups have recently revised the time table of the early events that led to Earth's formation. In his Perspective, Jacobsen explains how this isotopic clock works and what it has revealed about early Earth. Just 10 million years after the first grains formed in the solar system, Earth had already accreted about 64% of its mass. About 20 million years later, a Mars-sized impactor smashed into Earth, leading to the formation of the Moon. The data also shed light on the origin of the materials from which the solar system was made.Keywords
This publication has 7 references indexed in Scilit:
- Lead Isotopic Ages of Chondrules and Calcium-Aluminum-Rich InclusionsScience, 2002
- New W-isotope evidence for rapid terrestrial accretion and very early core formationGeochimica et Cosmochimica Acta, 2002
- A short timescale for terrestrial planet formation from Hf–W chronometry of meteoritesNature, 2002
- Rapid accretion and early core formation on asteroids and the terrestrial planets from Hf–W chronometryNature, 2002
- Hf-W Isotopic Evidence for Rapid Accretion and Differentiation in the Early Solar SystemScience, 1996
- Abundances of Actinides and Short-lived Nonactinides in the Interstellar Medium: Diverse Supernova Sources for the [ITAL]r[/ITAL]-ProcessesThe Astrophysical Journal, 1996
- Evidence for 182Hf in the early Solar System and constraints on the timescale of terrestrial accretion and core formationGeochimica et Cosmochimica Acta, 1996