A point source seismological model is used in this study to model the available strong motion accelerograms recorded by 17 events and to calculate three seismological model parameters, the source, path, and quality factor. Due to the paucity of recorded events, this is the first time these model parameters have been obtained for the northeastern and its surrounding region of India. The quality factors of the horizontal and vertical components of recorded events with corresponding standard deviations are QH(f) = 188.55f 0.94 , σ 1 value (25, 0.025) and QV (f) = 169.76f0.93 , σ1 value (20, 0.03), respectively. The source parameter stress drop values (△σ) vary within 124-180 bars for the subduction region and 80-169 bars for the active region. The Kappa factors for the horizontal and vertical components of recorded events on the soft rock site are 0.06 and 0.05, respectively. These seismological model parameters obtained in this study will be useful for future work deriving a ground motion attenuation relation based on a spectral model. Finally, these results are useful for seismic hazard assessment of a region having sparsely recorded events. A point source seismological model is used in this study to model the available strong motion accelerograms recorded by 17 events and to calculate three seismological model parameters, the source, path, and quality factor. Due to the paucity of recorded events, this is the first The quality factors of the horizontal and vertical components of recorded events with corresponding standard deviations are QH (f) = 188.55f 0.94, σ 1 value (25, 0.025 ) and QV (f) = 169.76f0.93, σ1 value (20, 0.03), respectively. The source parameter stress drop values ​​(△ σ) vary within 124-180 bars for the subduction region and 80-169 bars for the active region. The Kappa factors for the horizontal and vertical components of recorded events on the soft rock sites are 0.06 and 0.05, respectively. These seismological model parameters obtained in this study will be useful for future work deriving a ground motion attenuation relation based on a spectral model. Finally, these results are useful for seismic hazard assessment of a region have sparsely recorded events.