Analysis of samples with the electron backscatter diffraction (EBSD) technique revealed zircon crystal structures that form only when reidite melts at very high temperatures and is then converted to zircon.[11] Reidite has been found only at meteorite impact sites, where it was formed at the very high pressures of impact. Airbursts never yield this type of mineral transformation.[12]
^Kramers, J.D et al (2013): Unique chemistry of a diamond-bearing pebble from the Libyan Desert Glass strewnfield, SW Egypt: Evidence for a shocked comet fragment. Earth and Planetary Science Letters 382, 21-31 doi:10.1016/j.epsl.2013.09.003
^B. Kleinmann (1968): The breakdown of zircon observed in the Libyan desert glass as evidence of its impact origin. Earth and Planetary Science Letters 5, 497-501. doi:10.1016/S0012-821X(68)80085-8
^Weeks, R. (1984): Libyan Desert glass: A review. Journal of Non-Crystalline Solids, 67, 593-619. doi:10.1016/0022-3093(84)90177-7
^Seebaugh, W. R. & Strauss, A. M. (1984): Libyan Desert Glass: Remnants of an Impact Melt Sheet. LUNAR AND PLANETARY SCIENCE XV, 744-745. [Abstract.] Bibcode:1984LPI....15..744S
^Barbara Kleinmann, Peter Horn and Falko Langenhorst (2001): Evidence for shock metamorphism in sandstones from the Libyan Desert Glass strewn field. Meteoritics & Planetary Science 36, 1277-1282 doi:10.1111/j.1945-5100.2001.tb01960.x
^Giovanni Pratesi, Cecilia Viti, Curzio Cipriani and Marcello Mellini (2002): Silicate-silicate liquid immiscibility and graphite ribbons in Libyan desert glass. Geochimica et Cosmochimica Acta 66, 903-911.doi:10.1016/S0016-7037(01)00820-1
^Greshake, Ansgar; Koeberl, Christian; Fritz, Jörg; Reimold, W. Uwe (2010). "Brownish inclusions and dark streaks in Libyan Desert Glass: Evidence for high-temperature melting of the target rock". Meteoritics & Planetary Science. 45 (6): 973–989. doi:10.1111/j.1945-5100.2010.01283.x. S2CID128920720.
^ abCavosie, Aaron J.; Koeberl, Christian (1 July 2019). "Overestimation of threat from 100 Mt–class airbursts? High-pressure evidence from zircon in Libyan Desert Glass". Geology. 47 (7): 609–612. Bibcode:2019Geo....47..609C. doi:10.1130/G45974.1. S2CID155125330.