New Insights of the Early Cretaceous Syn-Rift Sedimentation in the Mecella Structure (Northeastern Atlas of Tunisia): Geodynamic Evolution

被引:7
作者
Aich, Nejla Sekatni [1 ]
Gharbi, Mohamed [2 ]
机构
[1] Univ Sousse, Dept Geog, Fac Lettres & Sci Humaines Sousse, Sousse Ryadh 4029, Sousse, Tunisia
[2] Ctr Rech & Technol Eaux Borj Cedria, Georesources Lab, BP 273, Soliman 8020, Tunisia
来源
PALEOBIODIVERSITY AND TECTONO-SEDIMENTARY RECORDS IN THE MEDITERRANEAN TETHYS AND RELATED EASTERN AREAS | 2019年
关键词
Early cretaceous; Intraplatform basin; Syn-rift tectonic; Halokinetic activity; Mecella structure;
D O I
10.1007/978-3-030-01452-0_61
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Detailed stratigraphy and facies analysis of the Early Cretaceous successions outcropping in the Mecella structure (Northeastern Tunisian Atlas), integrated with a structural analysis, allowed us to characterize the evolution of an intraplatform basin. A syn-rift tectonic is associated with the development of the major synsedimentary normal fault systems producing the tilted blocks basin geometry in Northeastern Tunisian Atlas. Incised sandy turbidite canyon, soft-sediment deformational structures mainly represented by slumps, down-slope sliding of ancient deposits and halokinetic activity are the main features of a syn-rift intraplatform basin. The close up of this intraplatform basin history occurred in the Hauterivian and Barremian stages by the installation of a condensed shallow water carbonate platform on the higher structures. The biostratigraphic results and the facies analysis of the resedimented Triassic series allow us to ascribe the halokinetic activity to the Upper Valanginian.
引用
收藏
页码:255 / 257
页数:3
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