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- W2004703510 abstract "La corrélation des faunes d'ammonites, d'ostracodes et de calpionelles, dans trois coupes de la chaîne du Nara (Tunisie centrale) précise la biostratigraphie de la formation marno-calcaire de Sidi Kralif. Le Tithonique supérieur (zone à Jacobi pars) et le Berriasien inférieur (zone à Grandis) correspondent à environ 40 m de sédiments pélagiques, lesquels reposent sur les dolomies du Nara. Le Berriasien moyen (zone à Occitanica), de même faciès, montre des variations d'épaisseurs sensibles (60 à 100 m). Seule la base du Berriasien supérieur (sous-zone à Paramimounum) est représentée au sommet, avec des faciès néritiques divers (calcaires bioclastiques, grès, dolomies, brèches de ravinement) et des épaísseurs très variables (10 à 100 m). La puissante formation détritique du Meloussi débute donc dans le Bérriasien terminal. The biostratigraphy of Sidi Kralif formation is precised by means of correlation of calpionellid, ostracod and ammonite faunas in three sections of Nara Mountain (Central Tunisia). The Upper Tithonian (Jacobi zone pars) and the Lower Berriasian (Grandis zone) show 40 m of pelagic sediments above the Nara dolomitic formation. The Middle Berriasian (Occitanica zone) under the same facies points out variations of thickness (60 to 100 m). Only the lower part of the Upper Berriasian (Paramimounum subzone) is present at the upper part with neritic facies (bioclastic limestones, sandstones, dolomites, breccia) and some changes of thickness (10 to 100 m). With the Upper Berriasian begins the thick detritic Meloussi formation." @default.
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- W2004703510 date "1976-01-01" @default.
- W2004703510 modified "2023-10-18" @default.
- W2004703510 title "Précisions biostratigraphiques nouvelles sur le Berriasien des Djebel Nara et Sidi Kralif (Tunisie centrale)" @default.
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- W2004703510 doi "https://doi.org/10.1016/s0016-6995(76)80033-2" @default.
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