A recent analysis of
chondrites by Carnegie's Myriam Telus was concerned with iron - 60, a short - lived radioactive isotope that decays into nickel - 60.
Not exact matches
The cores of the worlds studied
by Bouquet and his co-authors are thought to have
chondrite - like compositions.
The stone's noble gas content supports an extraterrestrial origin, while the presence of tiny diamonds — larger than nanodiamonds found in a common kind of meteorite called
chondrites, but similar in size to diamond aggregates known to be formed
by impacts — supports a cometary origin.
Or, the proto - moon and proto - Earth were showered
by the same family of carbonaceous
chondrites soon after they separated, said James Van Orman, professor of earth, environmental and planetary sciences at Case Western Reserve, and a co-author.
They moreover show that the light signature emitted
by Phobos and Deimos is incompatible with that of the primordial matter that formed Mars (meteorites such as ordinary
chondrite, enstatite
chondrite and / or angrite).
Based on data obtained with the Gamma Ray and Neutron Detector aboard the Dawn spacecraft, Prettyman et al. (p. 242, published online 20 September) show that Vesta's reputed volatile - poor regolith contains substantial amounts of hydrogen delivered
by carbonaceous
chondrite impactors.
Two possible ways that the inner solar system received water are: water molecules sticking to dust grains inside the «snow line» (as shown in the inset) and carbonaceous
chondrite material flung into the inner solar system
by the effect of gravity from protoJupiter.
In the samples of mantle gas taken
by Holland and his colleagues, the krypton measurements were heavy, producing «something that looks rather like gases that are trapped in primitive
chondrites today,» Pepin says.
«The results confirm one of the basic ideas of planetary formation theory, that most of the Earth formed
by collisions of smaller objects like carbonaceous
chondrites,» says Scott Kenyon at the Harvard - Smithsonian Center for Astrophysics in Cambridge, Massachusetts.
The composition of the matter from which the solar system formed is deduced from that of stony meteorites called
chondrites and from the composition of the Sun's atmosphere, supplemented
by data acquired from spectral observations of hot stars and gaseous nebulas.
«The water content (
by weight) of the meteorites is about 11 percent for type 1
chondrites, about 9 percent for type 2, and 2 percent or less for type 3.»