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Abstract Chondrules are millimeter-scale rocky particles that occur as the dominant component in most chondrite meteorites. Chondrules formed within the first few million years of formation of the first solids in the solar system, 4,562–4,567 million years ago.
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Chondrules: Suggestion Concerning the Origin
Science, 1966The millimeter-sized, sometimes glassy spheroids called chondrules that occur abundantly in stony meteorites may have been produced by lightning in the primitive Laplacian-type nebula while earthy materials were condensing and collecting to form the asteroids and the terrestrial planets.
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Early evolution of the solar accretion disk inferred from Cr-Ti-O isotopes in individual chondrules
Earth and Planetary Science Letters, 2020Yves Marrocchi +2 more
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