Примери за използване на Differentiated asteroid на Английски и техните преводи на Български
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They are thought to be pieces of the metallic core of differentiated asteroids that were fragmented by impacts.
They are nickel-rich and contain high amounts of gallium, germanium, copper, and cobalt,indicating that formation occurred in the core of a differentiated asteroid.
Both groups probably formed on the same parent body, a differentiated asteroid that was disrupted by a single impact event.
These data suggest the formation of the IIIF irons occurred in the core of a small, differentiated asteroid.
Perhaps both groups share a common origin on a partially differentiated asteroid, one also thought to be the source of a class of rare primitive achondrites- the winonaites.
This is considered to be evidence that this group originated in the core of a small, differentiated asteroid.
Recent research suggests that the IVA irons formed in the core of a small, differentiated asteroid disrupted by a major impact shortly after its formation.
With regards to elemental abundances, the IIC irons are known for their high thallium content, andit is thought that they formed in the core of a small, differentiated asteroid.
One theory has them formed by the collision of two differentiated asteroids, allowing the still liquid core of one asteroid to mix with the solidified crust of the other.
The IVB irons display low values for the trace elements gallium and germanium,consistent with the supposed formation of the IVB irons in the core of a small, differentiated asteroid.
More recent research suggests that the IVA iron meteorites formed in the core of a small, differentiated asteroid that was disrupted by a major impact shortly after its formation.
This suggests that the formation of the IIG irons occurred in the outer regions of the core of a differentiated asteroid, probably distinct from the IIAB parent body.
The metal in mesosiderites is similar to that of IIIAB irons, andcame from the core of a differentiated asteroid, genetically unrelated to the precursor of the eucritic and diogenitic portion.
However, the metal in mesosiderites is similar to group IIIAB irons,obviously representing the core of a distinct, differentiated asteroid, genetically unrelated to the precursor of the eucritic and diogenitic portion.
Recent research suggests that both, winonaites andIAB irons, originated on a common parent body- a partially differentiated asteroid that was disrupted just as it began to form an iron core and a silicate-rich crust.
Recent research suggests that both the winonaites andthe IAB iron meteorites originated on the same parent body- a partially differentiated asteroid that was violently disrupted just as it began to form a nickel-iron core and silicate-rich crust.
Formation history: Recent research suggests that both, winonaites and IAB irons,originated on a common parent body- a partially differentiated asteroid that was disrupted just as it began to form an iron core and a silicate-rich crust.
Formation history& Origin: Recent research suggests that both the winonaites andthe IAB iron meteorites originated on the same parent body- a partially differentiated asteroid that was violently disrupted just as it began to form a nickel-iron core and silicate-rich crust.
Probably a moderately differentiated C-type asteroid that was disrupted by an impact event and then rapidly cooled.
Trace element abundances also suggest that the IIAB irons formed in the core of a differentiated C-type asteroid that was disrupted by several impact events.
During the early history of the Solar System, the asteroids also melted to some degree, allowing elements within them to be partially or completely differentiated by mass.
The asteroids melted to some level during the Solar System's early history, and thus the elements within them were either wholly or partially differentiated by mass.
The asteroid belt also goes by other names such as the main belt or main asteroid belt, to differentiate it from other asteroids in the solar system including the Trojan asteroids. .
Some asteroids are similarly differentiated… where you have a metallic iron-nickel core… surrounded by a layer of silicates… and various combinations of other materials in the shell.