Sentence examples for planetary accretion from inspiring English sources

Boujibar, A. et al. Metal silicate partitioning of sulphur, new experimental and thermodynamic constraints on planetary accretion.

Walker, R. J. Highly siderophile elements in the Earth, Moon and Mars: update and implications for planetary accretion and differentiation.

During Stage 1 of the "Era of Planetary Accretion," which occurred earlier than 4.55 billion years ago, supernova explosions distributed elements that condensed into about 60 minerals.

During the first billion years of Solar System evolution, following planetary accretion, the rate of impact cratering was substantially higher than over the past 3.5 Gyr.

Prior to the Archean Eon, the Earth was in the astronomical (Hadean) stage of planetary accretion that began about 4.6 billion years ago; no rocks are preserved from this stage.

Here I show that Pluto could have acquired its current orbit during the late stages of planetary accretion, when the jovian planets underwent significant orbital migration as a result of encounters with residual planetesimals7.

In these earliest stages of terrestrial accretion heat was generated by three possible phenomena: (1) the decay of short-lived radioactive isotopes, (2) the gravitational energy released from the sinking of metals, or (3) the impact of small planetary bodies (or planetesimals).

The idea cited most often is that, when Venus was forming from the accretion of planetary building blocks (planetesimals), one of the largest of these bodies collided with the proto-Venus in such a way as to tip it over and possibly slow its spin as well.

Chondritic material could have been a common component of the inner Solar system shortly after its formation and the biologically useful products of clay mineral organic matter interactions could have also widespread, and delivered to planetary surfaces through the accretion of carbonaceous asteroids.

The Earth formed through the accretion of numerous planetary embryos that were already differentiated into a metallic core and silicate mantle.

This high metallicity is thought to have been crucial to the Sun's development of a planetary system because the planets form from the accretion of "metals".