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The article explores the deep crustal structure of the Greenland–Iceland–Faroe Ridge in the North Atlantic, focusing on the characteristics of the Iceland region. Geophysical techniques were used to study the Bouguer gravity anomaly and Moho depth values, revealing significant differences in density and crustal thickness in the study area. The research highlights the development of deep faults and structural zones in the region, providing valuable insights into the tectonic evolution of the Greenland–Norwegian Sea. [Extracted from the article]