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The gravity map of Ouaddai in the eastern region of Chad exhibits important anomalies that are often delimitated by the high gravity gradients, resulting from the density contrasts between various anomaly sources. This presumes an important tectonic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8fe2c8e440a1062577d5c978371d0a72
