Zobrazeno 1 - 10
of 26
pro vyhledávání: '"Hédi Zouari"'
Publikováno v:
Revue Française de Photogrammétrie et de Télédétection, Iss 215 (2017)
L'article présente les résultats de l'étude de l'évolution spatiale et temporelle de l'occupation du sol dans le bassin de l'Oued Chiba (200 km2) situé au Nord-Est de la Tunisie. Cette analyse est fondée sur une classification de données de t
Externí odkaz:
https://doaj.org/article/70b3c18e362342f99736663163bb9ce6
Publikováno v:
Journal of African Earth Sciences. 149:291-306
The lower Maastrichtian chalks of the Ghezala-Mateur area, northern Tunisian domain, were investigated with regard to their palaeogeographic implications. Two lateral facies have been identified (i) the white chalk facies occurs to the NW, NE and SE
Publikováno v:
Revue Française de Photogrammétrie et de Télédétection, Iss 215 (2017)
Revue Française de Photogrammétrie et de Télédétection, Iss 215 (2020)
Revue Française de Photogrammétrie et de Télédétection, Iss 215 (2020)
L'article présente les résultats de l'étude de l'évolution spatiale et temporelle de l'occupation du sol dans le bassin de l'Oued Chiba (200 km2) situé au Nord-Est de la Tunisie. Cette analyse est fondée sur une classification de données de t
Publikováno v:
Modeling Earth Systems and Environment. 3:1323-1341
The Utique basin is situated in the northeastern Tunisia, It is borded by Jebel Hakima and Jebel en Nadour to the north, the Gulf of Tunis to the east, Jebel Amar and Jebel Nahli to the south and Jebel Kechabta to the west. The sedimentary series in
Publikováno v:
Arabian Journal of Geosciences. 12
The northwestern Tunisian Mateur–Beja domain comprises a thick succession of carbonate units belonging to the Late Cretaceous (Abiod Formation) and the Early Eocene times (Bou Dabbous Formation and its lateral equivalent). Sedimentological analyses
Publikováno v:
International Journal of Remote Sensing
International Journal of Remote Sensing, Taylor & Francis, 2019, 40 (4), pp.1506-1533. ⟨10.1080/01431161.2018.1528018⟩
International Journal of Remote Sensing, Taylor & Francis, 2019, 40 (4), pp.1506-1533. ⟨10.1080/01431161.2018.1528018⟩
International audience; The potential of Visible Near-Infrared and Short-Wave Infrared (VNIR-SWIR, 400 nm-2500 nm) hyperspectral imagery for use in multivariate approaches and geostatistical techniques for mapping topsoil properties has been previous
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b36294dbdd53d89477c2315fcb0e551c
http://www.documentation.ird.fr/hor/fdi:010075212
http://www.documentation.ird.fr/hor/fdi:010075212
Autor:
Cécile Gomez, Ahmed Laamrani, Anis Gasmi, Philippe Lagacherie, Abdelghani Chehbouni, Hédi Zouari
Publikováno v:
Geoderma
Geoderma, Elsevier, 2021, 388, pp.114864. ⟨10.1016/j.geoderma.2020.114864⟩
Geoderma, Elsevier, 2021, 388, pp.114864. ⟨10.1016/j.geoderma.2020.114864⟩
Visible, near-infrared and short wave infrared (VNIR/SWIR, 400–2500 nm) remote sensing imagery is a useful tool for topsoil property mapping, but limited to bare soils pixels. With the increasing amount of freely available VNIR/SWIR satellite image
Autor:
Meriem Tarki, Abdelkrim Charef, Hédi Zouari, Bilel Challouf, Mouna Andolssi, Jalila Makni, Sofien Alyahyaoui
Publikováno v:
Arabian Journal of Geosciences. 8:8879-8897
The Utique region is located in the extreme north part of Tunisia. It is represented by the main and over exploited shallow Plio-Quaternary aquifers of Ghornata-Aousdja-Ghar el Meleh. These aquifers are captured by a good number of wells which are ch
Tunisia is enriched by many natural resources (natural water and geothermal water) that are located along the South to the North. This paper aims mainly to evaluate the resources water potential. The available remote sensing images for two typical ex
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c72aecf52924bbf5905de9fe758719f3
Autor:
Fehmy Belghouthi, Hédi Zouari
Publikováno v:
Journal of African Earth Sciences. 160:103608
The lower Eocene carbonate deposits of the northwestern Tunisian basin is represented by shallow-marine carbonate series composed of abundant coarse-grained deposits including conglomerate, coquina-bearing limestone, coarse-grained calcarenite and gl