Age of meteorites and the Earth
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The Earth formed at c. 4.54 Ga.
“since the Earth's formation at c. 4.54 Ga (Patterson, 1956)”
From Secular change and the onset of plate tectonics on Earth (2020) · cites this paper as Patterson, 1956
Cites
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“In this contribution, we review the current state of understanding of the veracity of various lines of evidence proposed to support or refute the operation of plate tectonics since the Earth's formation at c. 4.54 Ga (Patterson, 1956).”
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- Authors
- Patterson, C.
- Affiliations
- California Institute of Technology (US)
- Corresponding author
- Patterson, Claire
- Venue
- Geochimica et Cosmochimica Acta
- Publisher
- Elsevier BV
- Published
- 1956-10
- Volume
- 10
- Issue
- 4
- Pages
- 230-237
- ISSN
- 0016-7037 (ISSN-L)
- OpenAlex
- W2047040143
- Cited by
- 559
- References
- 10
- Citations by year
- 2026: 11 · 2025: 12 · 2024: 16 · 2023: 12 · 2022: 15 · 2021: 13 · 2020: 17 · 2019: 17 · 2018: 37 · 2017: 20 · 2016: 18 · 2015: 30 · 2014: 18 · 2013: 17 · 2012: 12
- FWCI
- 26.63
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Geochimica et Cosmochimica Acta (publishedVersion)
- Topics
- Physical Sciences › Physics and Astronomy › Astronomy and Astrophysics › Astro and Planetary Science
- Physical Sciences › Earth and Planetary Sciences › Geophysics › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Keywords
- meteorite ages, age of the Earth, radiometric dating, Earth formation
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Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
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