Modeling figure and orientation of the Earth's lithosphere based on paleoDEM
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The purpose of the research is to determine the displacement of points of the Earth's surface in geological time based on the results of geopaleoreconstructions using the digital elevation model (paleoDEM). By approximating paleoDEM to the form of simple geometric shapes (biaxial and triaxial ellipsoids). their parameters are obtained, and the orientation relative to the ellipsoid that describes the geoid.
[1] Blakey R. (2016). Global Paleogeography. Retrieved from https://www2.nau.edu/rcb7/
[2] Scotese, C.R., and Wright, N., 2018. PALEOMAP Paleodigital Elevation Models (PaleoDEMS) for the Phanerozoic PALEOMAP Project, https://www.earthbyte.org/paleodem-resourcescotese-and-wright-2018/
[3] Scotese, C.R. (2017). PALEOMAP Project. Retrieved from http://www.scotese.com/
[4] Tserklevych, A. L., Zayats, O. S., & Shylo, Y. O. (2016). Approximation of the physical surface of the earth by biaxial and triaxial ellipsoid. Geodynamics, (1), 40-49.
[5] Tserklevych, A. L., Zayats, O. S., Shylo, Y. O., & Shylo, O. M. (2018). Generation of the Stressed State of the Lithosphere of the Earth and Mars Caused by the Reorientation of Their Figures. Kinematics and Physics of Celestial Bodies, 34(1), 19-36.
[6] Tserklevych, A. L., Zayats, O. S., & Shylo, Y. O. (2017). Dynamics of the Earth shape transformation. Kinematics and Physics of Celestial Bodies, 33(3), 130-141.
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