A revised timeline of lunar bombardment, featuring greater granularity and matching new assumptions. (Figure 3, Morbidelli, Marchi, Bottke & Kring, 2012) [ arXiv:1208.4624v1 ]. |
Morbidelli, Marchi, Bottke & Kring
OCA, Nice
Center for Lunar Origin & Evolution, SwRI, Boulder
Center for Lunar Science & Exploration, USRA -
Lunar and Planetary Institute, Houston
TX, USA
We revisit the early evolution of the Moon's bombardment.
Our work combines modeling (based on plausible projectile sources and their dynamical decay rates) with constraints from the lunar crater record, radiometric ages of the youngest lunar basins and the abundance of highly siderophile elements in the lunar crust and mantle.
OCA, Nice
Center for Lunar Origin & Evolution, SwRI, Boulder
Center for Lunar Science & Exploration, USRA -
Lunar and Planetary Institute, Houston
TX, USA
We revisit the early evolution of the Moon's bombardment.
Our work combines modeling (based on plausible projectile sources and their dynamical decay rates) with constraints from the lunar crater record, radiometric ages of the youngest lunar basins and the abundance of highly siderophile elements in the lunar crust and mantle.
The new profile for lunar bombardment matches a population of 150 basins since lunar formation [Frey (2009)]. |
The Nectaris basin should have been one of the first basins formed at the sawtooth. We predict the bombardment rate since 4.1 billion years ago declined slowly and adhered relatively close to classic crater chronology models (Neukum and Ivanov (1994)). Overall we expect the sawtooth event accounted for about 1/4 the total bombardment suffered by the Moon since its formation. Consequently, considering that 12-14 basins formed during the sawtooth event, we expect the net number of basins formed on the Moon was 45-50.
From our expected bombardment timeline, we derived a new and improved lunar chronology suitable for use on Pre-Nectarian surface units. According to this chronology, a significant portion of the oldest lunar cratered terrains have an age of 4.38 - 4.42 billion years. Moreover, the largest lunar basin, South Pole-Aitken, is older than 4.3 billion years and was therefore not produced during the lunar cataclysm.
- A Sawtooth-like Timeline for the First Billion Year of Lunar Bombardment
Alessandro Morbidelli, Simone Marchi, William F. Bottke, David A. Kring
arXiv.org (Submitted on 22 Aug 2012) arXiv:1208.4624v1 [astro-ph.EP]
Alessandro Morbidelli, Simone Marchi, William F. Bottke, David A. Kring
arXiv.org (Submitted on 22 Aug 2012) arXiv:1208.4624v1 [astro-ph.EP]
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