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Titlebook: Vesiculation and Crystallization of Magma; Fundamentals of the Atsushi Toramaru Book 2022 The Editor(s) (if applicable) and The Author(s),

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发表于 2025-3-21 20:08:02 | 显示全部楼层 |阅读模式
书目名称Vesiculation and Crystallization of Magma
副标题Fundamentals of the
编辑Atsushi Toramaru
视频video
概述Is the first book that deals comprehensively with vesiculation and crystallization processes in volcanic eruptions.Provides detailed descriptions of the physics and concepts behind the basic formulas
丛书名称Advances in Volcanology
图书封面Titlebook: Vesiculation and Crystallization of Magma; Fundamentals of the  Atsushi Toramaru Book 2022 The Editor(s) (if applicable) and The Author(s),
描述This book comprehensively illustrates the elemental processes of vesiculation and crystallization recorded in volcanic products on the basis of the equilibrium and non-equilibrium theories. The book describes the derivation of equations and the basic physics behind them in detail. This textbook is fundamental in preparing for future volcanic hazards. The target readers are graduate students and researchers, but Parts I and IV are written to be understandable by undergraduate students as well, to inspire them to enter this field.
出版日期Book 2022
关键词Vesiculation of magma; Crystallization of magma; Volcanic eruption; Texture of rock; Pumice; Mechanisms o
版次1
doihttps://doi.org/10.1007/978-981-16-4209-8
isbn_softcover978-981-16-4211-1
isbn_ebook978-981-16-4209-8Series ISSN 2364-3277 Series E-ISSN 2364-3285
issn_series 2364-3277
copyrightThe Editor(s) (if applicable) and The Author(s), under exclusive license to Springer Nature Singapor
The information of publication is updating

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Cooling Crystallization of Magmailibrium as well as supersaturation in terms of thermodynamics. Next, we will conduct the formulation of crystal nucleation and crystal growth, evaluate experiments using these results, and examine the classical theory. As the crystal growth-related problems, the compositional zoning that is often o
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Crystallization Induced by Vesiculationthe influence of bubble nucleation and growth processes, we will examine the case in which water content can change in disequilibrium with pressure. In the latter case, the rate of change in water content is greatly different between the disequilibrium and quasi-equilibrium regimes. Because there is
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