Conditions and mechanisms of origination of gravitational instability in layered bulk-elastic geomasses
- 作者: Ryzhak E.I.1, Mukhamediev S.A.1, Sinyukhina S.V.1
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隶属关系:
- Schmidt Institute of Physics of the Earth
- 期: 卷 52, 编号 6 (2016)
- 页面: 787-802
- 栏目: Article
- URL: https://journals.rcsi.science/1069-3513/article/view/223834
- DOI: https://doi.org/10.1134/S1069351316060094
- ID: 223834
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详细
Various geophysical processes which can lead to the origination of gravitational instability of the Rayleigh-Taylor type in layered bulk-elastic geomasses are analyzed. The analysis is based on obtained by the authors general results of theoretical study of two-layer systems of heavy bulk-elastic materials which are arbitrarily stratified over depth and occupy domains of arbitrary shape. Additionally some presented in a number of recent publications erroneous assertions related to considered issues of stability, are criticized.
作者简介
E. Ryzhak
Schmidt Institute of Physics of the Earth
编辑信件的主要联系方式.
Email: E_I_Ryzhak@mail.ru
俄罗斯联邦, ul. B. Gruzinskaya 10, Moscow, 123995
Sh. Mukhamediev
Schmidt Institute of Physics of the Earth
Email: E_I_Ryzhak@mail.ru
俄罗斯联邦, ul. B. Gruzinskaya 10, Moscow, 123995
S. Sinyukhina
Schmidt Institute of Physics of the Earth
Email: E_I_Ryzhak@mail.ru
俄罗斯联邦, ul. B. Gruzinskaya 10, Moscow, 123995
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