Summary: Evidence is presented for the existence of silicon-oxygen chains up to 1000 Å. in length in melts of CaMgSi2O6 and of LiAISi2O6 at temperatures a little above the melting point.
Mineralogical Magazine; December 1960 v. 32; no. 251; p. 640-643; DOI: 10.1180/minmag.1960.032.251.04
© 1960, The Mineralogical Society
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