This supports the idea that CAIs crystallization and chondrule formation occurred around the same time during the formation of the solar system.
22.
The main characteristic of CI chondrites is the lack of recognizable chondrules ( an exception being the sample from Tagish Lake ).
23.
Saponite is also found in the " dark rims " of chondrules in carbonaceous chondrites and seen as a sign of aqueous alteration.
24.
Yet small chondrule fragments and calcium-aluminium-rich inclusions ( CAI's ) do occur, but are quite rare.
25.
The geological history of Benton has four stages : chondrule formation and accumulation, brecciation, thermal metamorphism and finally shock vein formation.
26.
Most chondrules are composed primarily of the silicate minerals olivine and pyroxene, surrounded by feldspathic material that may either be glassy or crystalline.
27.
The main arguments for this hypothesis are the relics of chondrules, the euhedral enstatites surrounded by meteoric iron and the occurrence of keilite.
28.
The variation of accretion efficiency with pebble size during this process results in the size sorting of the chondrules observed in the primitive meteorites.
29.
The growth of silicate particles is limited by the bouncing barrier to ~ 1 mm, roughly the size of the chondrules found in meteorites.
30.
Each chondrite group has a distinctive mixture of chondrules, refractory inclusions, matrix ( dust ), and other components and a characteristic grain size.
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