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Understanding the Moon's formation mechanism is necessary for studying not only the Moon itself, but also the evolution, formation, habitability, and structure of other planets and the moons in the Solar system and in extrasolar planetary…

地球与行星天体物理 · 物理学 2014-02-04 Mukesh Gupta

We examine the dynamics and stability of circumbinary particles orbiting around the Earth-Moon binary system. The moon formed close to the Earth (semi-major axis $a_{EM}\approx 3\, R_\oplus$) and expanded through tides to its current day…

地球与行星天体物理 · 物理学 2024-07-16 Stephen Lepp , Rebecca G. Martin , Stanley A. Baronett

The mean angular momentum associated with the collision of two celestial objects moving in almost circular heliocentric orbits was studied. The results of these studies were used to develop models of the formation of binaries at the stage…

地球与行星天体物理 · 物理学 2010-11-29 Sergei I. Ipatov

The solar system's terrestrial planets are thought to have accreted over millions of years out of a sea of smaller embryos and planetesimals. Because it is impossible to know the surface density profile for solids and size frequency…

地球与行星天体物理 · 物理学 2020-05-11 Matthew S. Clement , Nathan A. Kaib , John E. Chambers

In the leading theory of lunar formation, known as the giant impact hypothesis, a collision between two planet-size objects resulted in a young Earth surrounded by a circumplanetary debris disk from which the Moon later accreted. The range…

地球与行星天体物理 · 物理学 2023-07-13 Miles Timpe , Christian Reinhardt , Thomas Meier , Joachim Stadel , Ben Moore

Massive cores of the giant planets are thought to have formed in a gas disk by accretion of pebble-size particles whose accretional cross-section is enhanced by aerodynamic gas drag [1][2]. A commonly held view is that the terrestrial…

地球与行星天体物理 · 物理学 2021-09-24 M. Brož , O. Chrenko , D. Nesvorný , N. Dauphas

The problem of the formation of the Moon is still not explained satisfactorily. While it is a generally accepted scenario that the last giant impact on Earth between some 50 to 100 million years after the starting of the formation of the…

地球与行星天体物理 · 物理学 2015-07-01 Rudolf Dvorak , Birgit Loibnegger , Thomas I. Maindl

The classical scenario of terrestrial planet formation is characterized by a phase of giant impacts among Moon-to-Mars mass planetary embryos. While the classic model and its adaptations have produced adequate analogs of the outer three…

地球与行星天体物理 · 物理学 2022-08-17 P. Franco , A. Izidoro , O. C. Winter , K. S. Torres , A. Amarante

Reproducing Uranus and Neptune remains a challenge for simulations of solar system formation. The ice giants' peculiar obliquities suggest that they both suffered giant collisions during their formation. Thus, there must have been an epoch…

地球与行星天体物理 · 物理学 2015-10-28 Andre Izidoro , Alessandro Morbidelli , Sean N. Raymond , Franck Hersant , Arnaud Pierens

Mars is likely to be a planetary embryo formed through collisions with planetesimals, which can explain its small mass and rapid formation timescale obtained from 182Hf-182$W chronometry. In the classical theory of planet formation, the…

地球与行星天体物理 · 物理学 2015-06-15 Hiroshi Kobayashi , Nicolas Dauphas

The giant impact hypothesis is the dominant theory explaining the formation of our Moon. However, its inability to produce an isotopically similar Earth-Moon system with correct angular momentum has cast a shadow on its validity.…

It has been proposed recently that the first step in the formation of both rocky and gas giant planets is dust sedimentation into a solid core inside a gas clump (giant planet embryo). The clumps are then assumed to migrate closer to the…

地球与行星天体物理 · 物理学 2015-05-20 Sergei Nayakshin

The dominant accretion process leading to the formation of the terrestrial planets of the Solar System is a subject of intense scientific debate. Two radically different scenarios have been proposed. The classic scenario starts from a disk…

地球与行星天体物理 · 物理学 2024-11-15 Alessandro Morbidelli , Thorsten Kleine , Francis Nimmo

Almost all the planets of our solar system have moons. Each planetary system has however unique characteristics. The Martian system has not one single big moon like the Earth, not tens of moons of various sizes like for the giant planets,…

The leading theory for the origin of the Moon is the giant impact hypothesis, in which the Moon was formed out of the debris left over from the collision of a Mars-sized body with the Earth. Soon after its formation, the orbit of the Moon…

科普物理 · 物理学 2015-03-11 Emil Noordeh , Patrick Hall , Matija Cuk

Modeling the formation of the ice giants Uranus and Neptune is a long-lasting problem in planetary science. Due to gas-drag, collisional damping, and resonant shepherding, the planetary embryos repel the planetesimals away from their reach…

地球与行星天体物理 · 物理学 2015-05-28 M. Jakubik , A. Morbidelli , L. Neslusan , R. Brasser

The current standard theory of the origin of the Moon is that the Earth was hit by a giant impactor the size of Mars causing ejection of iron poor impactor mantle debris that coalesced to form the Moon. But where did this Mars-sized…

天体物理学 · 物理学 2014-10-13 Edward Belbruno , J. Richard Gott

The terrestrial planets are believed to have formed by violent collisions of tens of lunar- to Mars-size protoplanets at time t<200 Myr after the protoplanetary gas disk dispersal (t_0). The solar system giant planets rapidly formed during…

地球与行星天体物理 · 物理学 2021-01-13 David Nesvorny , Fernando V. Roig , Rogerio Deienno

Terrestrial planets grew in a series of similar-sized collisions that swept up most of the next-largest bodies. Theia was accreted by the Earth to form the Moon according to the theory. Planetesimals likewise may have finished their…

地球与行星天体物理 · 物理学 2018-10-16 Erik Asphaug

The evolution of Earth-Moon system is described by the dark matter field fluid model proposed in the Meeting of Division of Particle and Field 2004, American Physical Society. The current behavior of the Earth-Moon system agrees with this…

综合物理 · 物理学 2008-01-13 Hongjun Pan