Timescales of Magamtic Processes from U-series Disequilibria
作者单位：Department of Geology and GeophysicsWoods Hole Oceanographic InstitutionWoods HoleMA 025423
会议名称：《International Conference on Continental Volcanism》
会议日期：2006年
学科分类：0709[理学-地质学] 070901[理学-矿物学、岩石学、矿床学] 07[理学]
摘 要：正The formation and transport of basaltic magma in the mantle by adiabatic decompression can be characterized in terms of the velocity of the upwelling （solid） mantle, the rate of melting, the melt velocity, the dispersivity associated with melt migration, and the delay time, or storage time, of magma before eruption. Two of these parameters, the velocity of upwelling mantle and the corresponding melting rate, can be estimated from models coupled with thermodynamic data and