Accounting for the influence of the Earth’s sphericity in three-dimensional density modelling


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Abstract

A method for transformation of the three-dimensional regional “flat” density models of the Earth’s crust and upper mantle to the “spherical” models and vice versa is proposed. A computation algorithm and a method of meaningful comparison of the vertical component of the gravity field of both models are presented.

About the authors

P. S. Martyshko

Institute of Geophysics, Ural Branch

Author for correspondence.
Email: pmart3@mail.ru
Russian Federation, Yekaterinburg, 620016

D. D. Byzov

Institute of Geophysics, Ural Branch

Email: pmart3@mail.ru
Russian Federation, Yekaterinburg, 620016

A. I. Chernoskutov

Institute of Geophysics, Ural Branch; Ural Federal University

Email: pmart3@mail.ru
Russian Federation, Yekaterinburg, 620016; Yekaterinburg

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