RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 21, ES1002, doi:10.2205/2020ES000722, 2021
Figure 1. 2D vertical prism model (O is the origin, $P$ is the calculation point, $h_1$ and $h_2$ are the top and bottom depths, respectively) and its parameters.
Citation: Tan Aylin, Mahir Isik, Hakki Senel (2021), Gravity interpretation of the Erzincan-Cayirli Basin its connection with the North Anatolian Fault Zone using quadratic density function, Russ. J. Earth Sci., 21, ES1002, doi:10.2205/2020ES000722.
Copyright 2021 by the Geophysical Center RAS.
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