Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Naoufel Ghannem"'
Publikováno v:
Quaternary International. 604:93-112
Located at the Tunisian Atlas area, the Quaternary basin of Borj Edouane-El Gara could serve as a good example for close relation between the continental infill and the neotectonic morphostructural pattern. This Quaternary basin is superimposed on pr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a44c002baf753b39fecc01d982f5ab6d
https://doi.org/10.1016/j.quaint.2021.07.012
https://doi.org/10.1016/j.quaint.2021.07.012
Publikováno v:
Journal of Earth System Science. 131
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d0384a25167699397aeb7a342f051ab1
https://doi.org/10.1007/s12040-022-01974-2
https://doi.org/10.1007/s12040-022-01974-2
Publikováno v:
International Journal of Earth Sciences. 109:221-238
The carbonate Borj Edouane Unit represents the northernmost documented Middle–Late Pleistocene continental carbonate deposits in Tunisia. The unit consists of two main facies associations, asymmetrically distributed: (1) calcrete–palustrine–lam
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2b8a4d053ea2fa70f7235b438959f5a3
https://doi.org/10.1007/s00531-019-01798-4
https://doi.org/10.1007/s00531-019-01798-4
Autor:
Ildefonso Armenteros, Naoufel Ghannem
Publikováno v:
Facies. 67
The middle-upper Pleistocene Borj Edouane unit records a singular spectrum of terrestrial carbonates in a shallow depression on Cretaceous rocks in north Tunisia. This study aims to decipher the depositional system and reveal the climatic and paleohy
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1cbdb25f0f6e8d91362b7c908bf6ad2e
https://doi.org/10.1007/s10347-020-00612-x
https://doi.org/10.1007/s10347-020-00612-x
Publikováno v:
Advances in Science, Technology & Innovation ISBN: 9783030014513
The Pleistocene Borj Edouane in NW Tunisia unit consists of two principal facies associations: (1) calcrete-palustrine-laminar crust facies and (2) microbialites. The laminar crusts consist of millimeter-thick couples (ranging from 0.7 to 3 mm thick)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::74a4fa71b4441b9c39c98c3b1f2c7fc6
https://doi.org/10.1007/978-3-030-01452-0_37
https://doi.org/10.1007/978-3-030-01452-0_37
Publikováno v:
Advances in Science, Technology & Innovation ISBN: 9783030015749
The Pleistocene carbonates of the Borj Edouane unit are made up of two principal facies associations: (1) calcrete-palustrine-laminar crust and (2) microbialites. The former represents the deposition in shallow lakes, as subjected to periodic exposur
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0c33439ffab7aca8be9a8b1e52a15ffc
https://doi.org/10.1007/978-3-030-01575-6_28
https://doi.org/10.1007/978-3-030-01575-6_28
Publikováno v:
Carnets de géologie (Notebooks on geology). 16:43-59
Les calcaires palustres d'âge quaternaire (Pleistocene moyen et superieur), objet de cette etude, se trouvent au niveau du massif El Gara Tajerouine (Nord-Ouest de la Tunisie). L'etude de ces depots a differentes echelles, macroscopique (description
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::970c5aeff63f43c5c4a5fedd14247007
https://doi.org/10.4267/2042/58976
https://doi.org/10.4267/2042/58976