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Titlebook: Lava Flows and Domes; Emplacement Mechanis Jonathan H. Fink Book 1990 Springer-Verlag Berlin Heidelberg 1990 Deformation.Mafic.formation.gr

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书目名称Lava Flows and Domes
副标题Emplacement Mechanis
编辑Jonathan H. Fink
视频video
丛书名称IAVCEI Proceedings in Volcanology
图书封面Titlebook: Lava Flows and Domes; Emplacement Mechanis Jonathan H. Fink Book 1990 Springer-Verlag Berlin Heidelberg 1990 Deformation.Mafic.formation.gr
描述This collection of papers is based on a symposium held in 1987 at the Interna­ tional Union of Geology and Geodesy Congress in Vancouver, British Colum­ bia. The Symposium was planned as a follow-up to a session at the 1984 Geo­ logical Society of America Annual Meeting in Reno, Nevada, which dealt with the emplacement of silicic lava domes. In both cases, emphasis was placed on the physical and mechanical rather than chemical aspects of lava flow. The IUGG Symposium consisted of two lecture sessions, a poster session, and two discussion periods, and had 22 participants. The contributions to this volume are all based on papers presented in the various parts of the Sym­ posium. The motivation for studying lava flow mechanics is both practical and scientific. Scientists and government agencies seek to more effectively predict the hazards associated with active lavas. Recovering mineral resources found in lava flows and domes also requires an understanding of their emplacement. From a more theoretical standpoint, petrologists view lava studies as a way to directly observe the rheologic consequences of mixing crystals, bubbles, and solid blocks of country rock with silicate liquids. Th
出版日期Book 1990
关键词Deformation; Mafic; formation; growth; lava; magma; morphology; ore deposit; volcano
版次1
doihttps://doi.org/10.1007/978-3-642-74379-5
isbn_softcover978-3-642-74381-8
isbn_ebook978-3-642-74379-5Series ISSN 0939-9658
issn_series 0939-9658
copyrightSpringer-Verlag Berlin Heidelberg 1990
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The Development and Distribution of Surface Textures at the Mount St. Helens Domef lava samples, have revealed relationships among lava surface texture, underlying slope, volatile content, and repose period. Two principal types of surface texture, smooth and scoriaceous, have formed on the Mount St. Helens dome during two different types of extrusive episodes. Type I extrusions
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Viscoplastic Models of Lava Domeshe spread of viscoplastic material over a horizontal surface provide means of examining geological data on dome growth in terms of dome rheology. Experiments using kaolin slurries show that a growing dome maintains a state of static equilibrium such that its height, H, radius, R, density, ., and yie
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