作者: A. R. McBirney , T. Murase
DOI: 10.1007/BF02596762
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摘要: The basic condition governing the formation of pyroclastic rocks is relationship between disruptive force gas pressure in bubbles to strength liquid for short term stresses and surface tension. latter factor controls coalescence bubbles, because it strongly dependent on composition, temperature, water content liquid. Data tension volcanic liquids are presented.