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Open AccessJournal ArticleDOI

Origin of the cataclysmic Late Heavy Bombardment period of the terrestrial planets

TLDR
This model not only naturally explains the Late Heavy Bombardment, but also reproduces the observational constraints of the outer Solar System.
Abstract
The petrology record on the Moon suggests that a cataclysmic spike in the cratering rate occurred approximately 700 million years after the planets formed; this event is known as the Late Heavy Bombardment (LHB). Planetary formation theories cannot naturally account for an intense period of planetesimal bombardment so late in Solar System history. Several models have been proposed to explain a late impact spike, but none of them has been set within a self-consistent framework of Solar System evolution. Here we propose that the LHB was triggered by the rapid migration of the giant planets, which occurred after a long quiescent period. During this burst of migration, the planetesimal disk outside the orbits of the planets was destabilized, causing a sudden massive delivery of planetesimals to the inner Solar System. The asteroid belt was also strongly perturbed, with these objects supplying a significant fraction of the LHB impactors in accordance with recent geochemical evidence. Our model not only naturally explains the LHB, but also reproduces the observational constraints of the outer Solar System.

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Journal ArticleDOI

Origin of the orbital architecture of the giant planets of the Solar System.

TL;DR: This model reproduces all the important characteristics of the giant planets' orbits, namely their final semimajor axes, eccentricities and mutual inclinations, provided that Jupiter and Saturn crossed their 1:2 orbital resonance.
Journal ArticleDOI

A low mass for Mars from Jupiter's early gas―driven migration

TL;DR: Simulation of the early Solar System shows how the inward migration of Jupiter to 1.5 au, and its subsequent outward migration, lead to a planetesimal disk truncated at 1’au; the terrestrial planets then form from this disk over the next 30–50 million years, with an Earth/Mars mass ratio consistent with observations.
Journal ArticleDOI

Evolution of Debris Disks

TL;DR: In this article, a review describes the theoretical framework within which debris disk evolution takes place and shows how that framework has been constrained by observations, including infrared photometry of large numbers of debris disks, providing snapshots of the dust present at different evolutionary phases.
Journal ArticleDOI

Lunar impact crater identification and age estimation with Chang’E data by deep and transfer learning

TL;DR: In this paper, the authors identify more than 109,000 previously unrecognized lunar craters and date almost 19,000 craters based on transfer learning with deep neural networks, which results in the identification of 109,956 new craters, which is more than a dozen times greater than the initial number of recognized craters.
Journal ArticleDOI

Chaotic capture of Jupiter's Trojan asteroids in the early Solar System.

TL;DR: 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.
References
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Journal ArticleDOI

Disk Frequencies and Lifetimes in Young Clusters

TL;DR: In this paper, the authors report the results of the first sensitive L-band survey of the intermediate-age (2.5-30 Myr) clusters NGC 2264, NGC 2362, and NGC 1960.
Journal ArticleDOI

Origin of the orbital architecture of the giant planets of the Solar System.

TL;DR: This model reproduces all the important characteristics of the giant planets' orbits, namely their final semimajor axes, eccentricities and mutual inclinations, provided that Jupiter and Saturn crossed their 1:2 orbital resonance.
BookDOI

Origin of the Earth and Moon

A.E. Ringwood
TL;DR: In this paper, a theory of the origin of the Earth is presented, based on the Mantle-Crust system and the formation of the inner core of the Moon, which is a major component of the outer core.
Journal ArticleDOI

Chaotic capture of Jupiter's Trojan asteroids in the early Solar System.

TL;DR: 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.
Journal ArticleDOI

Source regions and timescales for the delivery of water to the Earth

TL;DR: In this paper, the authors investigated the origin of Earth's water of dynamical models of primordial evolution of solar system bodies and check them with respect to chemical constraints, finding that it is plausible that the Earth accreted water all along its formation, from early phases when the solar nebula was still present to the late stages of gas-free sweepup of scattered planetesimals.
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