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El Haria Formation

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Interpreted seismic lines showing an unconformity at the <b>El</b> <b>Haria</b> <b>Formation</b>...
Published: 01 September 2021
Figure 18. Interpreted seismic lines showing an unconformity at the El Haria Formation base published by Abidi et al. (2018) . Picked horizons are the (1) top Cenomanian Fahdene Formation, (2) top Coniacian-Santonian Aleg Formation, (3) top Campanian Abiod Formation, (4) top Maastrichtian
Image
—Isopach map of <b>El</b> <b>Haria</b> <b>Formation</b>. CI 100 m, 200 m.
Published: 01 March 1975
Fig. 21 —Isopach map of El Haria Formation. CI 100 m, 200 m.
Journal Article
Published: 01 January 1963
Bulletin de la Société Géologique de France (1963) S7-V (3): 345–350.
...Sassi B. M. Sassi Abstract Eocene and Mio-Pliocene formations of the Gafsa region are differentiated by their clay minerals. The clays of the El-Haria formation are composed of equal amounts of montmorillonite and kaolinite. The overlying Eocene marine clays of Djebel M'Dilla are composed...
Image
Interpreted seismic line with partial erosion of the Upper Cretaceous serie...
Published: 01 September 2021
Figure 8. Interpreted seismic line with partial erosion of the Upper Cretaceous series. U 1 : Campanian unconformity; Horizons relate to the (1) top Aleg Formation, (2) top Abiod Formation, (3) top El Haria Formation, (4) top BouDabbous Formation, (5) top Souar Formation, (6) top Ketatna
Image
Interpreted seismic line showing systems of normal faulting. The red fault ...
Published: 01 September 2021
Figure 10. Interpreted seismic line showing systems of normal faulting. The red fault system relates to the intra-Lutetian phase; the black fault system is posterior to the Ain Grab Formation. The picked horizons are the (1) top Abiod Formation, (2) top El Haria Formation, (3) top BouDabbous
Image
(a) Interpreted seismic line showing the depocenter of the Souar <b>Formation</b>....
Published: 01 September 2021
Figure 9. (a) Interpreted seismic line showing the depocenter of the Souar Formation. (b) Flattening at the top of Souar Formation. (c) Flattening at the top of Ain Grab Formation showing the Fortuna Formation depocenter. (1) Top Abiod Formation, (2) top El Haria Formation, (3) top BouDabbous
Image
Postdeposited series on the inherited floor geometry related to the reefal ...
Published: 01 September 2021
Figure 7. Postdeposited series on the inherited floor geometry related to the reefal construction distribution. GR log (the green color) and DT log (the red color); (0) reef construction facies, (1) top reef construction, (2) top Aleg Formation, (3) top Abiod Formation, (4) top El Haria Formation
Image
Model-based inversion using W1 well on a seismic profile passing through th...
Published: 01 September 2021
) top El Haria Formation, (3) top BouDabbous Formation, (4) top Souar Formation, (5) top Fortuna Formation, (6) top Ain grab Formation, and (7) top Oum Douil Formation.
Image
Structural evolution highlighting the intra-Lutetian compressive phase and ...
Published: 01 September 2021
. Picked horizons are (0) reef construction facies, (1) top reef construction, (2) top Aleg Formation, (3) top Abiod Formation, (4) top El Haria Formation, (5) top BouDabbous Formation, (6) top Souar Formation, (7) top Fortuna Formation, (8) top Ain grab Formation, and (9) top Mahmoud Formation.
Journal Article
Journal: Interpretation
Published: 01 September 2021
Interpretation (2021) SH39–SH56.
...Figure 18. Interpreted seismic lines showing an unconformity at the El Haria Formation base published by Abidi et al. (2018) . Picked horizons are the (1) top Cenomanian Fahdene Formation, (2) top Coniacian-Santonian Aleg Formation, (3) top Campanian Abiod Formation, (4) top Maastrichtian...
FIGURES | View All (21)
Journal Article
Published: 01 September 2005
Journal of Paleontology (2005) 79 (5): 1031–1035.
... Kalaat Senan, Tajerouine, and Kalaa Khasba (see Robaszynski et al., 1990 , 1993a , 1993b , 1993c , 2000 ; Hardenbol et al., 1993 ; Dupuis et al., 2000 ; and Steurbaut et al., 2000 for detailed litho- and biostratigraphy) ( Fig. 1 ). An almost 600 m thick marly sequence of the El Haria Formation...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1975
AAPG Bulletin (1975) 59 (3): 413–450.
...Fig. 21 —Isopach map of El Haria Formation. CI 100 m, 200 m. ...
FIGURES | View All (27)
Journal Article
Published: 01 April 2003
Petroleum Geoscience (2003) 9 (2): 145–161.
... the unconformable contact with the underlaying El Haria Formation of Paleocene age ( Bishop 1988 ; Saint-Marc 1992 ). This bed is exposed in five sections: in the Kef El Guitoune 1 and Bou Dabous sections of Transect 1, in the Sidi-El-Rahbi section of Transect 2, and in the El Sfeia and Kef El Garia sections...
FIGURES | View All (12)
Journal Article
Journal: Clay Minerals
Published: 01 April 2000
Clay Minerals (2000) 35 (2): 375–381.
... as accurately as possible the mineralogical characteristics of the clay fraction. Three clay samples from central Tunisia (JZ1 and 22/2) and southern Tunisia (A402) were selected for this study. The JZ1 and 22/2 samples are from the Souar formation (Upper Eocene) and A402 from the El Haria formation...
FIGURES
Journal Article
Published: 01 April 2010
Journal of Foraminiferal Research (2010) 40 (2): 148–164.
... Formation at El Kef, central-northeastern Tunisia, were chosen for this study (Fig. 1 ). The El Haria Formation consists of marls and micritic limestones of late Maastrichtian–Paleocene age, lying between the Campanian–Maastrichtian Abiod Formation and the lower Eocene Jebel Madhkour Formation ( Bourollet...
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Journal Article
Published: 22 April 2013
Journal of the Geological Society (2013) 170 (3): 435–449.
... Campanian to Maastrichtian in age, is composed of two limestone beds interbedded with marl ( Fig. 3 ). The Tertiary is represented by Palaeocene clay (El Haria Formation), Early Eocene limestone (Bou Dabbous Formation), Late Eocene clay (Souar Formation) and Oligocene alternations of sand and clay (Fortuna...
FIGURES | View All (15)
Journal Article
Published: 01 January 2003
Micropaleontology (2003) 49 (2): 189–195.
...) for the Cretaceous-Paleogene boundary and plays a key role in stratigraphic correlation worldwide ( Cowie et al. 1989 ). The K-P boundary is situated in the middle part of a hemipelagic marl succession of El Haria Formation and is defined by a 2 mm thick reddish ferruginous layer containing, among others, the well...
FIGURES
Journal Article
Published: 01 October 2007
Journal of Micropalaeontology (2007) 26 (2): 97–101.
..., Eastern Desert, Egypt ( Morsi & Speijer, 2003 ) and has been reported here from the Ain Settara Marls, El Haria Formation, Sidi Nasseur sections (Danian/Selandian transition) ( Van Itterbeeck et al ., 2007 ). It has also been observed from the Paleocene/Eocene transition higher up in the same...
FIGURES
Journal Article
Journal: Palynology
Published: 01 January 2001
Palynology (2001) 25 (1): 29–55.
... to the El Haria Formation. Sample GSAS 2, latest Eocene–?basal Oligocene in age ( Hemiplacophora semilunifera, Rottnestia borussica, Samlandia chlamydophora, Magnastriatites howardii ), is likely ascribable to the Souar Formation. This attribution is supported by the absence of bisaccate pollen which...
FIGURES | View All (13)
Journal Article
Published: 01 July 2000
Journal of Foraminiferal Research (2000) 30 (3): 202–218.
... in Central Tunisia, in the region between Kalaat Senan, Tajerouine and Kalaa Khasba, 50 km south of the El Kef K/P boundary stratotype (Fig. 1 ). The K/P boundary lies within the lower part of the marly El Haria Formation, at about 180 m above the top of the Abiot Formation and 400 m below the base...
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