Magma transport and storage
Magma transport and storage
复制标题
岩浆运输和储存
DOI：
10.1038/330216a0
复制
发表时间：
1990
期刊：
影响因子：
64.8
通讯作者：
Storage from Source to Eruption Site
中科院分区：
文献类型：
--
作者：
M. P. Ryan;Storage from Source to Eruption Site
第一部分岩浆系统的热质输运：地球软流圈熔体输运的压实模型--基本模型，应用，A.C.傅勒热点、膨胀和地幔柱，P.奥尔森岩浆波和底辟动力学，J. A. Whitehead：橄榄石熔体系统中熔体迁移的实验研究.小赖尔斯和D.L.之间。Kohlstedt关于玄武岩岩浆层流沿沿着岩脉凝固和熔融的研究，P.M.布鲁斯和H.E. Huppert关于层流和湍流在浮力驱动的岩浆断裂中的作用，D.L. Turcotte火山爆发的计算机模拟，K.H. Wohletz和G.A. Valentine研究了圣海伦斯火山喷发单元的原位热输运特性和热结构。M. P. Ryan等，第2部分：岩浆系统的运输结构、力学和动力学：地幔橄榄岩的熔体提取：水力压裂和多孔流，以及洋脊活动的后果，A.尼古拉斯关于冰岛岩浆运输系统的物理性质，M. P. Ryan北冰岛德拉夫拉火山口动力学- 1975-1985，J.A. Ewart等根据高压高温下橄榄岩的地震测量推断上地幔岩浆的生成，H。佐藤和IS地震层析成像揭示的不同火山环境中岩浆储存的差异-硅质火山中心和与俯冲有关的火山，H.M. E.T.圣海伦斯火山英安质岩浆上升速率的Iyer地球物理和观测约束Endo等在日本樱岛火山的安山质火山爆发中的压力源和诱发的地面变形。JB根据地面变形测量推断，石原在埃特纳火山的高位岩浆输送默里改变了埃特纳火山喷发的风格。Hughes等人
Part 1 Heat and mass transport in magmatic systems: a compaction model for melt transport in the earth's asthenosphere - The basic model, applications, A.C. Fowler hot spots, swells and mantle plumes, P. Olson magma waves and diapiric dynamics, J.A. Whitehead an experimental study of melt migration in an olivine-melt system, G.N. Riles, Jr. and D.L. Kohlstedt solidification and melting along dykes by the laminar flow of basaltic magma, P.M. Bruce and H.E. Huppert on the role of laminar and turbulent flow in buoyancy driven magma fractgures, D.L. Turcotte computer simulations of explosive volcanic eruptions, K.H. Wohletz and G.A. Valentine the in-situ thermal transport properties and the thermal structure of Mount Saint Helens eruptive units. M.P. Ryan et al. Part 2 Transport structure, mechanics and dynamics of magmatic systems: melt extraction from mantle peridotites: hydrofracturing and porous flow, with consequences for oceanic ridge activity, A. Nicolas on the physical nature of the Icelandic magma transport system, M.P. Ryan dynamics of Drafla Caldera North Iceland - 1975-1985, J.A. Ewart et al magma generation in the upper mantle inferred from seismic measurements in peridotite at high pressure and temperature, H. Sato and I.S. Sacks differences in magma storage in different volcanic environments as revealed by seismic tomography - Silicic volcanic centers and subduction-related volcanoes, H.M. Iyer geophysical and observational constraints for ascent rates of dacitic magma at Mount Saint Helens, E.T. Endo et al pressure sources and induced ground deformation associated with explosive eruptions at an andesitic volcano - Sakurajima Volcano, Japan, K. Ishihara high-level magma transport at Mount Etna volcano, as deduced from ground deformation measurements, J.B. Murray changing styles of effusive eruption of Mount Etna since 1600 A D, J.W. Hughes et al.