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A chondrite (/ˈkɒn.draɪt/, CON-drite) is a stony (non-metallic) meteorite that has not been modified by either melting or differentiation of the parent body. They are formed when various types of dust and small grains in the early Solar System accreted to form primitive asteroids. Some such bodies that are captured in the planet's gravity well become the…
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chondrites chondrules type refractory matrix meteorite formed inclusions solar elements groups metal alteration asteroids experienced contain group minerals system metamorphism
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Chondrite | Compositional type | Stony | 1.00 | infobox |
| Chondrite | Parent body | Small to medium asteroids that were never part of a body large enough to undergo melting and planetary differentiation. | 1.00 | infobox |
| Chondrite | Petrologic type | 3–6 | 1.00 | infobox |
| Chondrite | Total known specimens | Over 27,000 | 1.00 | infobox |
| olivine | instance of | They are often referred to as unequilibrated chondrites because minerals | 0.80 | text |
| pyroxene show a wide range of compositions | instance of | They are often referred to as unequilibrated chondrites because minerals | 0.80 | text |
| reflecting formation under a wide variety of conditions in the solar nebula | instance of | They are often referred to as unequilibrated chondrites because minerals | 0.80 | text |
| feldspar form.Some workers have extended the Van Schmus | instance of | metamorphic minerals | 0.80 | text |
| Wood metamorphic scheme to include a type 7 | instance of | metamorphic minerals | 0.80 | text |
| although there is not consensus on whether this is necessary | instance of | metamorphic minerals | 0.80 | text |
| glycine | instance of | It is a CM2 and it contains common amino acids | 0.80 | text |
| alanine | instance of | It is a CM2 and it contains common amino acids | 0.80 | text |
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