Titlebook: Spectral Methods for the Estimation of the Effective Elastic Thickness of the Lithosphere; Jonathan Kirby Book 2022 Springer Nature Switze

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Book 2022 Earth sciences in general—none cover the details of the methods for its estimation. This book brings together the disparate knowledge required to estimate Te in one handy volume: signal processing, harmonic analysis, civil engineering, and foundational mathematics and physics, in addition to the re

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Map Projectionsrojection: angle, area or distance; the other two must be sacrificed. In this chapter we will learn about map projections and the concept of distortion, honing in upon the best projections for planar spectral analysis of data given on a curved surface.

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Isostasy, Flexure and Strengthpport by bending stresses within a thin, elastic plate. The former mechanism is known as isostasy, the latter as flexure. Here, we chart the path taken from the beginnings of isostatic theory up to the current flexural isostatic models, though only in a qualitative, descriptive manner. We will be in

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Map Projectionsspace and wavenumber domains. However, the gravity and topography data from which effective elastic thickness is estimated are collected and coordinated on the surface of a planet—a curved surface which is best modelled as a sphere or ellipsoid. The procedure by which geodetically-coordinated data a

Exposition

Loading and Flexure of an Elastic Plate of flexural models. Hence, one needs to be able to determine a relationship between applied loads on the lithosphere and the amount of bending such loads generate. Studies have shown that, over very long timescales, the lithosphere flexes like a thin, elastic plate with thickness .. Thus, this chap

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