Can planetesimals left over from terrestrial planet formation produce the lunar Late Heavy Bombardment
@article{Bottke2007CanPL, title={Can planetesimals left over from terrestrial planet formation produce the lunar Late Heavy Bombardment}, author={William F. Bottke and Harold F. Levison and David Nesvorn{\'y} and Luke Dones}, journal={Icarus}, year={2007}, volume={190}, pages={203-223} }
Figures from this paper
103 Citations
The onset of the lunar cataclysm as recorded in its ancient crater populations
- Physics, Geology
- 2012
Onset of Giant Planet Migration before 4480 Million Years Ago
- Geology, PhysicsThe Astrophysical Journal
- 2019
Soon after their formation, the terrestrial planets experienced intense impact bombardment by comets, leftover planetesimals from primary accretion, and asteroids. This temporal interval in solar…
Comets as collisional fragments of a primordial planetesimal disk
- Physics, Geology
- 2015
The Rosetta mission and its exquisite measurements have revived the debate on whether comets are pristine planetesimals or collisionally evolved objects. We investigate the collisional evolution…
Impact bombardment chronology of the terrestrial planets from 4.5 Ga to 3.5 Ga
- Geology, PhysicsIcarus
- 2020
The terrestrial Planet V hypothesis as the mechanism for the origin of the late heavy bombardment
- Physics, Geology
- 2011
In this study we attempt to model, with numerical simulations, the scenario for the origin of the late heavy bombardment (LHB) proposed in Chambers (2007, Icarus, 189, 386). Chambers suggested that…
Modeling the Historical Flux of Planetary Impactors
- Geology, Physics
- 2016
The impact cratering record of the Moon and the terrestrial planets provides important clues about the formation and evolution of the solar system. Especially intriguing is the epoch ≃3.8–3.9 Gyr ago…
New Perspectives on the Lunar Cataclysm from Pre-4 Ga Impact Melt Breccia and Cratering Density Populations
- Geology
- 2007
Crystallisation ages of impact melt breccias from the near-side equatorial regions of the Moon show a pronounced clustering between 3.75 and 3.95 billion years. This age distribution was unexpected…
What are the real constraints on the existence and magnitude of the late heavy bombardment
- Geology, Physics
- 2007
Common feedstocks of late accretion for the terrestrial planets
- Geology, PhysicsNature Astronomy
- 2021
Abundances of the highly siderophile elements (HSEs) in silicate portions of Earth and the Moon provide constraints on the impact flux to both bodies, but only since ~100 Myr after the beginning of…
References
SHOWING 1-10 OF 152 REFERENCES
Origin of the cataclysmic Late Heavy Bombardment period of the terrestrial planets
- Physics, GeologyNature
- 2005
This model not only naturally explains the Late Heavy Bombardment, but also reproduces the observational constraints of the outer Solar System.
A plausible cause of the late heavy bombardment
- Physics, Geology
- 2001
Abstract— We show that at the end of the main accretional period of the terrestrial planets, a few percent of the initial planetesimal population in the 1–2 AU zone is left on highly‐inclined orbits…
Could the Lunar “Late Heavy Bombardment” Have Been Triggered by the Formation of Uranus and Neptune?
- Physics, Geology
- 2001
We investigate the hypothesis that the so-called Late Heavy Bombardment (LHB) of the Moon was triggered by the formation of Uranus and Neptune. As Uranus and Neptune formed, which we assume occurred…
Iron meteorites as remnants of planetesimals formed in the terrestrial planet region
- Geology, PhysicsNature
- 2006
It is shown that the iron-meteorite parent bodies most probably formed in the terrestrial planet region, and it is predicted that some asteroids are main-belt interlopers and a select few may even be remnants of the long-lost precursor material that formed the Earth.
What are the real constraints on the existence and magnitude of the late heavy bombardment
- Geology, Physics
- 2007
Megaregolith evolution and cratering cataclysm models—Lunar cataclysm as a misconception (28 years later)
- Geology, Physics
- 2003
Abstract— The hypothesis of a lunar cataclysmic cratering episode between 3.8 and 3.9 Gyr ago lacks proof. Its strongest form proposes no cratering before about 4.0 Gyr, followed by catastrophic…
Chaotic capture of Jupiter's Trojan asteroids in the early Solar System
- Physics, GeologyNature
- 2005
It is shown that the Trojans could have formed in more distant regions and been subsequently captured into co-orbital motion with Jupiter during the time when the giant planets migrated by removing neighbouring planetesimals.
Effects of Type I Migration on Terrestrial Planet Formation
- Geology, Physics
- 2004
Planetary embryos embedded in a gas disk suffer a decay in semimajor axis—type I migration—due to the asymmetric torques produced by the interior and exterior wakes raised by the body. This presents…
The Primordial Excitation and Clearing of the Asteroid Belt
- Physics, Geology
- 2001
Abstract In this paper, we use N -body integrations to study the effect that planetary embryos spread between ∼0.5 and 4 AU would have on primordial asteroids. The most promising model for the…