Static Mantle Density Distribution 3 Dimpling and Bucking of Spherical Crust

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SFRL6NDV

Static Mantle Density Distribution 3 Dimpling and Bucking of Spherical Crust

Tian-Quan Yun
Tian-Quan Yun
DOI

Abstract

This paper is the third step of project “Static mantle distribution, Equation, Solution and Application”. It consists of , , and this paper. Our result on shape of core is a “X type”, which differs from the traditional view that core is a sphere. Which one is correct? or, both are not correct? The aim of this paper is to study dimpling and bucking of the spherical crust under mantle loading. Dimpling analysis depends on the outer solution of non-homogeneous non-linear D. E., while bucking analysis depends on nonlinear Eigen value of the homogeneous D. E The results based on two models and governing equations show that crust dimpled at poles is proved theoretically and numerical result well consists with pole radius, while the non-linear bucking Eigen value boundary problem is solved by decomposition method. The results show that bucking can occur, and the un-continuity of internal force per unit length causes un-continuity of masses by mantle material emitting to crust at turning point of “X”. The growing of Tibet high-land might be viewed as an evidence of the mass 𝐦𝐦𝐬𝐬(𝛉𝛉𝟎𝟎) increasing due to mantle emission. Both poles radius and equatorial radius have been used to support our analysis. Question: how the nature makes cold at poles?

Static Mantle Density Distribution 3 Dimpling and Bucking of Spherical Crust

This paper is the third step of project “Static mantle distribution, Equation, Solution and Application”. It consists of , , and this paper. Our result on shape of core is a “X type”, which differs from the traditional view that core is a sphere. Which one is correct? or, both are not correct? The aim of this paper is to study dimpling and bucking of the spherical crust under mantle loading. Dimpling analysis depends on the outer solution of non-homogeneous non-linear D. E., while bucking analysis depends on nonlinear Eigen value of the homogeneous D. E The results based on two models and governing equations show that crust dimpled at poles is proved theoretically and numerical result well consists with pole radius, while the non-linear bucking Eigen value boundary problem is solved by decomposition method. The results show that bucking can occur, and the un-continuity of internal force per unit length causes un-continuity of masses by mantle material emitting to crust at turning point of “X”. The growing of Tibet high-land might be viewed as an evidence of the mass 𝐦𝐦𝐬𝐬(𝛉𝛉𝟎𝟎) increasing due to mantle emission. Both poles radius and equatorial radius have been used to support our analysis. Question: how the nature makes cold at poles?

Tian-Quan Yun
Tian-Quan Yun

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Tian-Quan Yun. 2020. “. Global Journal of Science Frontier Research – A: Physics & Space Science GJSFR-A Volume 20 (GJSFR Volume 20 Issue A8): .

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Crossref Journal DOI 10.17406/GJSFR

Print ISSN 0975-5896

e-ISSN 2249-4626

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GJSFR Volume 20 Issue A8
Pg. 21- 38
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GJSFR-A Classification: FOR Code: 010599
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Static Mantle Density Distribution 3 Dimpling and Bucking of Spherical Crust

Tian-Quan Yun
Tian-Quan Yun

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