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Cited by 214

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Lunar Impact History from 40 Ar/ 39 Ar Dating of Glass Spherules

Culler, Timothy S., Becker, Timothy A., Muller, Richard A., Renne, Paul R.·2000·Science

Abstract

Lunar spherules are small glass beads that are formed mainly as a result of small impacts on the lunar surface; the ages of these impacts can be determined by the 40 Ar/ 39 Ar isochron technique. Here, 155 spherules separated from 1 gram of Apollo 14 soil were analyzed using this technique. The data show that over the last ∼3.5 billion years, the cratering rate decreased by a factor of 2 to 3 to a low about 500 to 600 million years ago, then increased by a factor of 3.7 ± 1.2 in the last 400 million years. This latter period coincided with rapid biotic evolutionary radiation on Earth.

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Metadata

Authors
Culler, T. S., Becker, T. A., Muller, R. A., & Renne, P. R.
Venue
Science
Published
2000-03-10
Volume
287
Issue
5459
Pages
1785-1788
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2141244066
Cited by
214
References
1
FWCI
11.36
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Lunar Impact History from 40 Ar/ 39 Ar Dating of Glass Spherules. https://app.cochat.ai/papers/10.1126/science.287.5459.1785
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Culler, T. S., Becker, T. A., Muller, R. A., & Renne, P. R. (2000). Lunar Impact History from 40 Ar/ 39 Ar Dating of Glass Spherules. Science. https://doi.org/10.1126/science.287.5459.1785

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

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