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Titlebook: Chaotic Processes in the Geological Sciences; David A. Yuen Conference proceedings 1992 Springer-Verlag New York, Inc. 1992 applied mathem

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樓主: 選民
31#
發(fā)表于 2025-3-26 21:49:31 | 只看該作者
Bayesian Networks in Decision Support,ity in the lower mantle of the Earth is emphasized. The latter may be responsible for the separation between standing and drifting fields found in the analysis of secular variation. It is even possible in principle to find dynamo action based on lateral variations of conductivity.
32#
發(fā)表于 2025-3-27 03:22:38 | 只看該作者
33#
發(fā)表于 2025-3-27 09:08:34 | 只看該作者
34#
發(fā)表于 2025-3-27 09:59:10 | 只看該作者
The IMA Volumes in Mathematics and its Applicationshttp://image.papertrans.cn/c/image/223931.jpg
35#
發(fā)表于 2025-3-27 13:36:00 | 只看該作者
Conference proceedings 1992ces have many nonlinearities from the nature of the complicated physical laws which give rise to strongly chaotic behavior. Foremost and most visible are earthquakes and volcanic eruptions, more subtle are the time- dependent variations of the Earth‘s magnetic fields and motions of the surface plate
36#
發(fā)表于 2025-3-27 18:49:18 | 只看該作者
37#
發(fā)表于 2025-3-27 23:25:30 | 只看該作者
Convection and Chaos,corresponding Poincaré map should lead to a chaotic distribution of plumes in space and time..For cellular convection, we give a synopsis of the recent scaling theory of the Chicago group. There is a mean flow in the cell, fuelled by thermal plumes which erupt from the boundary layer as they are adv
38#
發(fā)表于 2025-3-28 03:47:48 | 只看該作者
39#
發(fā)表于 2025-3-28 07:27:12 | 只看該作者
Vigorous Motions in Magma Chambers and Lava Lakes,m laboratory experiments using aqueous solutions. The agreement between the two sets of results is shown to be very good. Calculations using the simple, geologically oriented, two- component anorthite-diopside system are presented and their geological interpretation discussed briefly.
40#
發(fā)表于 2025-3-28 11:55:09 | 只看該作者
The Eruption and Spreading of Lava,ints on the evolution of the magma reservoir which feeds them. During flow away from a volcanic vent at the Earth’s surface, compressibility affects the dynamics of spreading, leading to smaller variations of flow thickness and hence to slower rates of advance..Lava eruptions present a puzzle becaus
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