## 4 Results
\begin{table}
\begin{tabular}{c c c c c c c} \hline
**Code** & **Date** & \begin{tabular}{c} **Latitude** \\ **(Degrees)** \\ \end{tabular} & \
\begin{tabular}{c} **Longitude** \\ **(Degrees)** \\ \end{tabular} & **Depth (km)** &
\begin{tabular}{c} **Magnitude** \\ **(Mw)** \\ \end{tabular} & **Distance (km)** \\ \hline S1 & 5 February 2015 & 8.356 & \(-\)72.102 & 3 & 4.0 & 186.3 \\ S2 & 5 February 2015 & 8.355 & \(-\)72.131 & 4 & 5.4 & 180.1 \\ S3 & 11 April 2015 & 6.395 & \(-\)73.273 & 3 & 4.3 & 69.7 \\ S4 & 19 September 2015 & 6.064 & \(-\)74.294 & 4 & 4.5 & 175 \\ S5 & 30 January 2017 & 6.533 & \(-\)73.364 & 32 & 4.0 & 63.4 \\ S6 & 7 March 2017 & 7.277 & \(-\)72.152 & 2 & 4.1 & 99.3 \\ S7 & 8 August 2017 & 6.593 & \(-\)72.203 & 4 & 4.9 & 96.7 \\ S8 & 25 May 2018 & 6.941 & \(-\)72.335 & 21 & 4.1 & 73 \\ S9 & 22 August 2018 & 6.22 & \(-\)74.157 & 20 & 4.0 & 152.4 \\ S10 & 5 November 2019 & 6.994 & \(-\)73.066 & 5 & 4.2 & 5.6 \\ S11 & 21 December 2019 & 6.994 & \(-\)73.066 & 5 & 4.1 & 5.6 \\ S12 & 30 January 2020 & 6.994 & \(-\)73.066 & 5 & 4.2 & 5.6 \\ S13 & 14 February 2020 & 6.093 & \(-\)73.943 & 11 & 4.0 & 142.3 \\ S14 & 6 March 2020 & 6.994 & \(-\)73.066 & 5 & 4.1 & 5.6 \\ S15 & 4 September 2020 & 6.994 & \(-\)73.066 & 5 & 4.5 & 5.6 \\ S16 & 29 January 2021 & 7.053 & \(-\)72.145 & 15 & 4.3 & 93.7 \\ S17 & 23 March 2021 & 7.394 & \(-\)71.806 & 30 & 4.6 & 139.4 \\ \hline \end{tabular}
\end{table} 
Table 1: Inventory of seismic events present for the study region obtained from the SGC [62], with depth selection parameters from 0 to 50 km, magnitude \(\geq\)4 Mw and radius of 200 km. As mentioned above, there is a significant discrepancy between the deformation rates observed by the ascending and descending view of LOS and their correlation with seismic events. This behavior is largely due to the acquisition geometry and the sensitivity of the signal due to the effect of the displacement of the satellite, which is limited only to measuring the movement of the ground in a one-dimensional (1D) way in the field of view of LOS, thus acquiring the displacements due to the co-seismic effects in an anamorphic way and with biased source parameters [66; 67]. The other factor that influences the behavior of Figure 5a,b, especially where it correlates with the events of Table 1, is the effect of the focal mechanism, since it describes in a two-dimensional way the geometry of the fault plane and its motion. An important aspect to mention within the general behavior of Figure 5a,b, is that these are the sectors that do not have a point of convergence with the seismic record, since it is not possible to establish the reason for the present deformation. Among these sectors is the behavior, especially in 2016 and 2019, in an ascending and descending direction, which, in turn, relatively describe the highest rates of deformation without a seismic event that presents the aforementioned characteristics. Taking this into account and adding other sectors that present the same conditions, the surface seismic events, as described, would not generate the present surface deformation. Based on this, for the present research and taking into account the results obtained from the superficial analysis, which are based on the descriptions made by [PERSON] and [PERSON] [7], temporal spaces are observed within the sequence of differential interferometry images that do not present a convergence with this surface tectonic analysis. In this sense, in order to establish a broader assessment where a scenario that generates these disturbances is proposed, an assessment from a more regional point of view will be addressed. With this approach, it is observed that the study region is located at the interaction of three tectonic plates (Nazca, Caribbean and South American Plate) that generate at the level of the Colombian territory zones that are described in the study by [PERSON] et al. [68] as subduction, stable continental region (non-Craton) and active continental shallow region, the latter being the area where the study region is located.