Triple oxygen isotopes of lunar water unveil indigenous and cometary heritage. [PDF]
Thiemens MM, Martinez MHN, Thiemens MH.
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The role of Bells in the continuous accretion between the CM and CR chondrite reservoirs. [PDF]
van Kooten E +4 more
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A 4,565-My-old record of the solar nebula field. [PDF]
Maurel C, Gattacceca J.
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The late formation of chondrites as a consequence of Jupiter-induced gaps and rings. [PDF]
Srivastava B, Izidoro A.
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Meteoritic Evidence for a Ceres-sized Water-rich Carbonaceous Chondrite Parent Asteroid. [PDF]
Hamilton VE +5 more
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Interstellar ices as carriers of supernova material to the early solar system. [PDF]
Bizzarro M +12 more
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The nucleosynthetic fingerprint of the outermost protoplanetary disk and early Solar System dynamics. [PDF]
van Kooten E +8 more
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Early silica crust formation in planetesimals by metastable silica-rich liquid immiscibility or cristobalite crystallisation: the possible origin of silica-rich chondrules. [PDF]
Faure F.
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History of chondrule forming heating events inferred from chondrule age distribution
Chondrules are major components in primitive meteorites and consist of 70 percent by volume in ordinary chondrites. They are considered to be formed by a flash heating of dusts in the protoplanetary disk, though the nature of the heating mechanism is not yet well understood.
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