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


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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.

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P. Martyshko

Institute of Geophysics, Ural Branch

编辑信件的主要联系方式.
Email: pmart3@mail.ru
俄罗斯联邦, Yekaterinburg, 620016

D. Byzov

Institute of Geophysics, Ural Branch

Email: pmart3@mail.ru
俄罗斯联邦, Yekaterinburg, 620016

A. Chernoskutov

Institute of Geophysics, Ural Branch; Ural Federal University

Email: pmart3@mail.ru
俄罗斯联邦, Yekaterinburg, 620016; Yekaterinburg

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