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- Chondrite - Wikipedia
A chondrite ˈkɒndraɪt is a stony (non- metallic) meteorite that has not been modified by either melting or differentiation of the parent body [a][1] They are formed when various types of dust and small grains in the early Solar System accreted to form primitive asteroids
- Chondrite | H-Group, Stony-Iron Achondrite | Britannica
Chondrite, in general, any stony meteorite characterized by the presence of chondrules The only meteorites classified as chondrites that do not contain chondrules are the CI group
- Chondrites – Buseck Center for Meteorite Studies
The chondrites take their name from chondrules, the nearly spherical, silicate-rich particles they contain They are the most abundant type of stony meteorite, and contain some of the first objects to have formed in the Solar System, including calcium-aluminum-rich inclusions (CAIs) and chondrules Chondrites have never undergone melting
- Meteorite - Chondrites, Achondrites, Iron-Nickel | Britannica
Chondrites are the most abundant meteorites (about 87 percent of stony meteorites) in collections They also are arguably the most important In terms of terrestrial rocks, these meteorites seem akin to sedimentary conglomerate s—i e , fragments of preexisting rock cemented together
- Carbonaceous chondrite | Definition, Composition, Facts - Britannica
carbonaceous chondrite, a diverse class of chondrite s (one of the two divisions of stony meteorite s), important because of the insights they provide into the early history of the solar system They comprise about 3 percent of all meteorite s collected after being seen to fall to Earth
- Meteorite Identification Pictures
Abee, Canada, EH4 chondrite Fell 1952
- chondrites - Meteorite Gallery
Chondrites are the most primitive group of meteorites They have formation ages dating to at least 4 56 billion years before the present, and have been little changed since then
- H chondrite - Wikipedia
H chondrite The H type ordinary chondrites are the most common type of meteorite, accounting for approximately 40% of all those catalogued, 46% of the ordinary chondrites, and 44% of all chondrites [1]
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