Примери за използване на Carbonaceous chondrites на Английски и техните преводи на Български
{-}
-
Colloquial
-
Official
-
Medicine
-
Ecclesiastic
-
Ecclesiastic
-
Computer
The carbonaceous chondrites are very rare and extremely interesting to scientists.
His studies focus on a rare type of meteorite called carbonaceous chondrites.
The most primitive carbonaceous chondrites have never been heated above 50°C!
It is believed that the volatiles of the earth were carried away by meteorites called carbonaceous chondrites.
Carbonaceous chondrites contain the most primitive materials known in this planetary system.
The structure and composition of these carbonaceous chondrites is more close to that of ordinary chondrites. .
It's long been thought that Earth's volatiles were perhaps carried in on meteorites,called carbonaceous chondrites.
This is especially true for the carbonaceous chondrites that have been relatively unaltered by heating during their history.
Prettyman also noted that Ceres' composition has been compared with a family of meteorites called carbonaceous chondrites.
One theory holds that special kinds of meteorites,called carbonaceous chondrites, slammed into Earth and gave the bulk silicate Earth these volatile elements.
Another very interesting isotopic link exists between the Eagle Station trio and the carbonaceous chondrites of the CO/CV clan.
However, there are different clans and groups of carbonaceous chondrites that formed on different parent bodies in different regions of the early solar nebula.
However, scientists have not yet identified a spectral match for a possible parent body for these rare carbonaceous chondrites yet.
Some carbonaceous chondrites don't fit into established groups, although they can be easily classified as members of the carbonaceous chondrite clan.
Traces of this supernova have been trapped within the CAIs andpreserved in the CV group and other carbonaceous chondrites up to this day.
One theory is that special types of meteorites,so-called carbonaceous chondrites, collided with the earth, giving the voluminous silicate earth these volatile elements.
However, more recently,they have been given their own group since they differ in some respect from all the other carbonaceous chondrites.
This group of carbonaceous chondrites is somewhat of an exception since its name is not derived from a type specimen but from one of the typical properties of those meteorites.
The chondrites of this group are named for their primary mineral, enstatite, andthey differ in many respects from ordinary and carbonaceous chondrites.
Some carbonaceous chondrites don't fit easily into the established groups, although they can be clearly identified as members of the class of carbonaceous chondrites. .
And while the isotopic signatures of Earth's volatiles match these primordial objects,known as carbonaceous chondrites, the elemental ratio of carbon to nitrogen is off.
All members of this group of carbonaceous chondrites belong to the petrologic type 3, and they show a certain relation to the CV group when it comes to chemistry and composition.
Therefore, many researchers suppose that the CV andthe CO group represent a distinct clan of carbonaceous chondrites that formed in the same region of the early solar system.
Carbonaceous chondrites or C chondrites represent some of the most pristine matter known, and their chemical compositions match the chemistry of the Sun more closely than any other class of chondrites. .
They are usually designated as CC ungrouped or CC UNGR andthey probably represent other parent bodies of carbonaceous chondrites or source regions of the primordial solar nebula.
Carbonaceous chondrites are primitive and undifferentiated meteorites that formed in oxygen-rich regions of the early solar system so that most of the metal is not found in its free form but as silicates, oxides, or sulfides.
Some of them show a certain relationshipto each other and to other groups of carbonaceous chondrites, but the Meteoritical Society has decided that it needs at least five members to constitute a new group.
All carbonaceous chondrites are primitive and undifferentiated meteorites that formed in oxygen-rich regions of the primordial solar nebula so that most of the metal is not found in its free form but in the form of silicates, oxides, or sulfides.
A similar oxygen isotopic composition is also displayed by the carbonaceous chondrites of the CO/CV clan, suggesting a formation of the IIF/ESP parent body in the outer regions of the asteroid belt.
Carbonaceous chondrites are primitive and undifferentiated meteorites that formed in oxygen-rich regions of the early solar system so that most of the metal is not found in its free form but as silicates, oxides, or sulfides.