Conditions and mechanisms of origination of gravitational instability in layered bulk-elastic geomasses


如何引用文章

全文:

开放存取 开放存取
受限制的访问 ##reader.subscriptionAccessGranted##
受限制的访问 订阅存取

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

补充文件

附件文件
动作
1. JATS XML

版权所有 © Pleiades Publishing, Ltd., 2016