I can't say this with any definiteness, but I don't believe any "new" (i.e., unweathered) chondrules show signs of concentric layering, only ones that have been exposed to Earth's atmosphere and have suffered degradation from moisture. I can't point to any example I have seen that shows anything like growth rings that have definitely formed outside Earth conditions; they all imply forming at once, rather than in successive buildups. This completely ignores the question of armored chondrules, however.

Tracy Latimer

ON THE ORIGIN OF CHONDRULES
Norm and List,
Please excuse my ignorance for putting forth this question but as a relative "newbe" to meteorite collecting, I hope you will entitle me to this query.
I came across the term "accretionary lapilli" also called "volcanic pisolites" in Dorothy Ferris Lapidus 1987 edition of "The Facts on File Dictionary of Geology and Geophysics.
If you bear with me I'll quote " these are shperoidal concentrically layered pellets composed mainly of vitric dust and ash, usually between 2 and 10 mm in diameter. They are formed primarily through the accretion of ash and dust by condensed moisture in eruption clouds. Formless nuclei of coarse particles fall through the fine debris and acquire shells of progressively finer ash. These concentric shells indicate the increasiing temperature and decreasing humidity of the cloud at lower levels.
My question is, does the process described above provide any anology("something similar but different") to the origin of chondrules.


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