Tectonic and Hydrothermal Activities in Debagh, Guelma Basin (Algeria) - INSU - Institut national des sciences de l'Univers Access content directly
Journal Articles Journal of Geological Research Year : 2013

Tectonic and Hydrothermal Activities in Debagh, Guelma Basin (Algeria)


Quaternary and Pliocene travertines, deposited from hot springs, can reveal much about neotectonic and hydrothermal activity. Theaimof this work is the understanding of the actual tectonic activity in the Guelma Basin and in one of its spa structures. Gravity data were collected during a field study in the Hammam Debagh (HD) area and then analyzed to better highlight the architecture of its subsurface underlying structures.This analysis was performed by means of a Bouguer anomaly, upward continuations, and residual and derivative maps. Comparison of gravity maps, field geology, geomorphic observations, and structural maps allowed us to identify the major structural features in the Hammam Debagh. As a result, we confirm the position of the Hammam Debagh active fault which is superimposed to the hydrothermal active source in the NW-SE direction characterized by a negative gravity anomaly.
Fichier principal
Vignette du fichier
409475.pdf (13.12 Mo) Télécharger le fichier
Origin Publisher files allowed on an open archive

Dates and versions

insu-00796415 , version 1 (04-03-2021)




Said Maouche, Abdesslam Abtout, Nacer-Eddine Merabet, Tahar Aifa, Et Al.. Tectonic and Hydrothermal Activities in Debagh, Guelma Basin (Algeria). Journal of Geological Research, 2013, pp.Article ID 409475. ⟨10.1155/2013/409475⟩. ⟨insu-00796415⟩
198 View
38 Download



Gmail Mastodon Facebook X LinkedIn More