2D and 3D structural boundaries of the tectonic composition of the Anatolia and
surrounding seas using by the gravity (Satellite Data): Eastern Mediterranean
Gravity data is processed and the problems of the earth are examined. The density of the data can be
arranged to solve detail, semi-detail and regional problems. Here, the gravitational data obtained by
processing the linearity of the 2D and 3D visuals in terms of plate size large wavelength structures
are examined. 2D linearities determine important stress areas but they are affected at different rates
with respect to the spatial distribution of source effect. Due to grid formation, these boundaries
are affected at different rates from less dense and very dense structures. Different wavelengths
in structure boundary analysis; derivative and phase elements and filters. Vertical change in 3D
analysis can be made at the approach level with the analytical examination of 2D change. At this
stage, the distribution of source effect and depth model structure parameters are calculated. When
examining large wavelength structures, some of the buried structures appear due to cover removal.
In search of solutions for tectonic structures that we may miss; The tectonic components that need to
be confirmed in the Eastern Mediterranean have been tried to be elucidated in this study. 3D building
solutions are important in this respect.
