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Titlebook: Some Aspects of the Formation of the Solar System; Vsevolod N. Anfilogov,Yurij V. Khachay Book 2015 The Author(s) 2015 Meteorites and Form

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发表于 2025-3-21 18:14:39 | 显示全部楼层 |阅读模式
书目名称Some Aspects of the Formation of the Solar System
编辑Vsevolod N. Anfilogov,Yurij V. Khachay
视频videohttp://file.papertrans.cn/872/871893/871893.mp4
概述Includes supplementary material:
丛书名称SpringerBriefs in Earth Sciences
图书封面Titlebook: Some Aspects of the Formation of the Solar System;  Vsevolod N. Anfilogov,Yurij V. Khachay Book 2015 The Author(s) 2015 Meteorites and Form
描述.This book is devoted to the problems that occur when attempting to understand and construct a concise representation of the original conditions, composition and dynamics of the evolution of the Earth-Moon system in the form in which it is seen today. This volume will perhaps contribute to a better understanding of what is necessary to research the dynamics of the Solar system..
出版日期Book 2015
关键词Meteorites and Formation of the earth and the moon; Molecular clouds and solar system formation; Solar
版次1
doihttps://doi.org/10.1007/978-3-319-17831-8
isbn_softcover978-3-319-17830-1
isbn_ebook978-3-319-17831-8Series ISSN 2191-5369 Series E-ISSN 2191-5377
issn_series 2191-5369
copyrightThe Author(s) 2015
The information of publication is updating

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,The Model of the Earth’s Heterogeneous Accumulation,distribution in the pre-planetary body allow us to determine that the heat released due to the decay of short-living radioactive elements can provide the melted state in the inner parts of bodies with sizes greater than 50 km.
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,The Model of the Earth’s Heterogeneous Accumulation,e suggest a new model of the Earth’s heterogeneous accumulation. The results of the numerical modeling, presented in this chapter, of the temperature distribution in the pre-planetary body allow us to determine that the heat released due to the decay of short-living radioactive elements can provide
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,Formation of the Earth’s Silicate Mantle,e accumulation is provided are defined. Attention is drawn to the role of chondrites of different composition in the frame of the Earth’s heterogeneous accumulation model. The conditions are formulated by which a melted layer at the bottom of the mantle is formed. At the bottom boundary of the layer
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About the Origin of the Moon Matter,s the decay of short-living isotopes stipulates a principally new mechanism of matter differentiation into the proto-planetary cloud and allows the construction of a dynamic model of the Moon’s formation as a development of the results of Schmidt, Safronov, Maeva, Ruskol, and Kaula without the model
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