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Titlebook: Volcanic Processes; Mechanisms in Materi Flavio Dobran Book 2001 Springer Science+Business Media New York 2001 gas.magma.plate tectonics.py

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發(fā)表于 2025-3-21 18:09:56 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書目名稱Volcanic Processes
副標(biāo)題Mechanisms in Materi
編輯Flavio Dobran
視頻videohttp://file.papertrans.cn/985/984084/984084.mp4
圖書封面Titlebook: Volcanic Processes; Mechanisms in Materi Flavio Dobran Book 2001 Springer Science+Business Media New York 2001 gas.magma.plate tectonics.py
描述Volcanic eruptions are fascinating manifestations of the Earth‘s dynamic inte- rior which has been cooling for the past several billion years. The planets of the solar system originated some 4.5 billion years ago from the same gas and dust cloud created by the big bang. Some of the gas collapsed by the gravitational force to form the Sun at the center, while the whirling disk of gas and dust around the Sun subsequently cooled and lumped together to form larger and larger lumps of materials or planetesimals. These planetesimals collided fre- quently and violently and in the process liberated heat that melted the material in them. With time this material gradually cooled and formed the planets of the solar system. During the second half of the twentieth century the theory of plate tectonics of the Earth became established and demonstrated that our planet is covered with six large and many small plates of the lithosphere. These plates move over a highly viscous lower part of the Earth‘s upper mantle and contain the continental and oceanic crusts. The lower mantle extends below the upper mantle until it meets the core that is more than half the diameter of the entire globe (12,740 km).
出版日期Book 2001
關(guān)鍵詞gas; magma; plate tectonics; pyroclastics; volcanic eruption
版次1
doihttps://doi.org/10.1007/978-1-4615-0647-8
isbn_softcover978-1-4613-5175-7
isbn_ebook978-1-4615-0647-8
copyrightSpringer Science+Business Media New York 2001
The information of publication is updating

書目名稱Volcanic Processes影響因子(影響力)




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發(fā)表于 2025-3-21 22:48:40 | 只看該作者
Overview of Volcanic Processes,arth’s land masses had once been joined together into a supercontinent (Hallam, 1975). In . (1620) even Francis Bacon called attention to the similarities of the continental outlines between Africa and South America without suggesting that they may once had formed a unified land. And in 1856 Antonio
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Properties of Igneous Materials,rature transformation and melting that transforms them into molten rock or magma. This sum of changes of the rock is called .. Typical metamorphic reactions occur above 150°C and at the highest temperatures give rise to magmatic processes. Under water-saturated conditions the crust starts melting at
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Magma Chambers,time intervals involving hundreds or thousands of years can be considered as a fluid. At shallower depths where the adiabat intersects the solidus (Figure 4.3), partial melting occurs. The melt fraction and the depth at which melting occurs are, however, poorly constrained because of the uncertainty
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Pyroclastic Dispersions,ver hundreds of kilometers because of the ejection of millions of tons of volcanic debris into the atmosphere in 20-50 hours of activity. In the stratosphere these clouds disperse horizontally and form shapes like the branches of a large Mediterranean pine tree. The ash and pumice in volcanic clouds
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