Viscosity of kimberlite and basaltic magmas at the origin, ascent and eruption
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Viscosity of kimberlite and basaltic magmas at the origin, ascent and eruption
The 6th ENGII Conference——Diamonds carrier kimberlite magmas will ascend from mantle to the crust with the essential acceleration. Viscosity of kimberlite magmas will decrease by about 1.5 orders of magnitude during their evolution and the ascent from mantle to the crust in spite of considerable decreasing of the magmas temperature (about 300℃), magmas partly degassing and crystallization during such processes.
嘉 賓 ：
Prof. Eduard Persikov
關鍵字 ：
金伯利岩 玄武岩 岩漿粘度 火山爆發視頻年代：2014
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