Rayed bubbles in tektites

Details Rayed bubbles in tektites Rayed bubbles in tektites

Sep 1964

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1964gecoa..28.1373b&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 28, Issue 9, pp.1373-1374

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Scientific paper

The discovery of thin rays extending outward from bubbles in indochinites and a moldavite adds another link to the evidence that tektites formed very quickly at high temperatures from terrestrial rocks, and cooled rapidly. The rays have a refractive index between 1.49 and 1.51, which is in the range of refractive index of albitic glass. The rays may be the result of explosive volatilization of a hydrous sodium aluminum silicate.

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