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Saqiye Group

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Image
 Isopach map of Late Eocene to present sediments (Saqiye and Kurkar groups) in the Jaffa Basin based on the Israeli oilwell database (Fleischer & Varshavsky 2002). Red dots are wells that penetrate the base Saqiye Group. Black dots are wells that did not reach the base. The faults west of the Jaffa Basin are based on seismic mapping as demonstrated in Figures 11 and 12.
Published: 01 March 2008
Fig. 4.  Isopach map of Late Eocene to present sediments (Saqiye and Kurkar groups) in the Jaffa Basin based on the Israeli oilwell database ( Fleischer & Varshavsky 2002 ). Red dots are wells that penetrate the base Saqiye Group. Black dots are wells that did not reach the base. The faults
Image
 The top Judea Group structural map (Fleischer & Gafsou 2003). Bold lines represent major faults; fine lines represent minor faults. Red, faults defined as active or potentially active (Bartov et al. 2002). Blue, reverse faults associated with Syrian Arc folds. Black, normal faults. The grey area at the eastern rim of the Jaffa Basin represents a truncation band where the top of the Judea Group is truncated by the base Saqiye Group. West of that band the Saqiye Group unconformably covers the Talme Yafe Formation. 1, Pardes Hanna water well; 2, Netanya 1 oilwell; 3, Hadera 1 oilwell; 4, Caesarea 1 oilwell; 5, Ashdod 3 oilwell; 6, Netanya 2 oilwell; 7, Hof Asdod 1 oilwell. BR is the Bet Rosh outcrop referred to in Figure 10.
Published: 01 March 2008
faults. The grey area at the eastern rim of the Jaffa Basin represents a truncation band where the top of the Judea Group is truncated by the base Saqiye Group. West of that band the Saqiye Group unconformably covers the Talme Yafe Formation. 1, Pardes Hanna water well; 2, Netanya 1 oilwell; 3, Hadera 1
Image
 Interpreted, time-migrated, regional, composite, seismic section 1 near the marine part of cross-section CC′ (for location see Fig. 13). The seismic section shows the compressive continental margin fault zone (previously named the Pelusium Line). The low-angle, reverse, possibly wrench faults displace the base Saqiye Group (Late Eocene) whereas the Messinian evaporites are faulted by a different, thin-skinned normal fault system.
Published: 01 March 2008
wrench faults displace the base Saqiye Group (Late Eocene) whereas the Messinian evaporites are faulted by a different, thin-skinned normal fault system.
Image
 Interpreted, time-migrated, regional, composite, seismic section 2 along the marine part of cross-section DD′ (for location see Fig. 13). The seismic section shows the compressive continental margin fault zone (previously named the Pelusium Line). The low-angle, reverse, possibly wrench faults displace the base Saqiye Group (Late Eocene) but not the Messinian evaporites, which are faulted by a different, thin-skinned normal fault system.
Published: 01 March 2008
wrench faults displace the base Saqiye Group (Late Eocene) but not the Messinian evaporites, which are faulted by a different, thin-skinned normal fault system.
Image
 Map summarizing all the features coinciding in time and space in and around the Jaffa Basin. The purple contour schematically represents the rhombic structure of the base Saqiye Group surface, which fits the shape of the Judea Group truncation zone (green zone). Together they indicate a fault-bounded basin. The less rhombic and larger structure of the base Yafo and base Kurkar surfaces indicates gradual development of the basin toward an elliptic bowl-shaped structure. The curvature around the basin is preserved in the current topography but not in the current bathymetry, which is governed by high-volume Nile-derived sediments.
Published: 01 March 2008
Fig. 13.  Map summarizing all the features coinciding in time and space in and around the Jaffa Basin. The purple contour schematically represents the rhombic structure of the base Saqiye Group surface, which fits the shape of the Judea Group truncation zone (green zone). Together they indicate
Image
 Stratigraphic table of the study area based on previous publications (Bein & Gvirtzman 1977; Ginzburg & Gvirtzman 1979; G. Gvirtzman 1990; Buchbinder et al. 1993; Buchbinder & Zilberman 1997; Fleischer & Varshavsky 2002; Z. Gvirtzman 2003). Absolute ages for the Jurassic and Cretaceous after Gradstein et al. (1995) and for the Cenozoic after Berggren et al. (1995). Highlighted surfaces are base Kurkar Group, base Yafo Formation, and base Saqiye Group, which refer to the structural maps of Figure 5; and also the base Mount Scopus Group, which refers to the structural map of Figure 6 and the highlighted horizon of Figure 8. The significant modification introduced in this chronostratigraphic scheme relative to previous ones is that the absence of Late Cretaceous and early Tertiary sediments in the coastal plain is interpreted as the result of late Tertiary erosion at the eastern rim of the Jaffa Basin rather than a lack of deposition.
Published: 01 March 2008
for the Jurassic and Cretaceous after Gradstein et al . (1995) and for the Cenozoic after Berggren et al . (1995) . Highlighted surfaces are base Kurkar Group, base Yafo Formation, and base Saqiye Group, which refer to the structural maps of Figure 5 ; and also the base Mount Scopus Group, which refers
Journal Article
Journal: AAPG Bulletin
Published: 01 August 1970
AAPG Bulletin (1970) 54 (8): 1548–1550.
... the Zohar gas field, and 1 in the northern Jordan rift. Two of the coastal plain wells aimed at the Neogene Saqiye Group. The Emeq Hula 1 well tested the Pleistocene fill of the rift valley in a section which is rich in carbonaceous lake and swamp deposits. Gas shows were reported from the Emeq Hula 1 well...
FIGURES
Journal Article
Published: 01 March 2008
Journal of the Geological Society (2008) 165 (2): 563–578.
...Fig. 4.  Isopach map of Late Eocene to present sediments (Saqiye and Kurkar groups) in the Jaffa Basin based on the Israeli oilwell database ( Fleischer & Varshavsky 2002 ). Red dots are wells that penetrate the base Saqiye Group. Black dots are wells that did not reach the base. The faults...
FIGURES | View All (14)
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1972
AAPG Bulletin (1972) 56 (9): 1820–1822.
..., they nevertheless constitute reservoir beds which could be potential producers in the coastal and offshore hinge-line belt ( Bein, 1971 ). A stratigraphic and environmental study of Triassic strata is nearing completion. A comprehensive study of late Eocene to early Pleistocene sediments, the Saqiye Group...
Journal Article
Journal: AAPG Bulletin
Published: 01 June 1985
AAPG Bulletin (1985) 69 (6): 946–949.
... of approximately 2,500 m, is made up of an upper Tertiary to Holocene sedimentary sequence ( Gvirtzman, 1970 ; Mart and Ben Gai, 1982). The upper Tertiary rocks belong to the Saqiye group ( Gvirtzman, 1970 ) and include, in the studied area, four formations (Derin et al, 1979b). The lowermost formations...
FIGURES
Journal Article
Journal: Geology
Published: 01 April 2011
Geology (2011) 39 (4): 355–358.
.... in the Late Eocene–Oligocene (thickness and duration in Figure 2 ). In addition, the nature of deposition throughout the region changed, from pelagic chalks that had characterized the 60 m.y. of the Senonian–Middle Eocene, to hemipelagic marls (Saqiye Group; Gvirtzman and Buchbinder, 1978 ), which have...
FIGURES | View All (4)
Journal Article
Journal: AAPG Bulletin
Published: 01 September 1971
AAPG Bulletin (1971) 55 (9): 1631–1633.
... drilled in the coastal plain, 2 of which aimed at the Jurassic and Lower Cretaceous and 2 at the Neogene Saqiye Group. The Sherif 1 well was an old well drilled deeper in the Negev and aimed at the Paleozoic, and the Gurim 3 was drilled near the Zohar gas field. Oil shows were reported from the Barne’a 1...
FIGURES
Journal Article
Published: 01 January 2010
Journal of the Geological Society (2010) 167 (1): 203–216.
... et al . 1995 ). Our study focuses on the stratigraphic column of the Late Tertiary section, locally recognized as the Saqiye Group ( Gvirtzman 1970 ). The complete Cenozoic section is summarized in a stratigraphic chart (Fig. 2 ) and illustrated in Figures 4 , 5 , 6 . Calibration of seismic...
FIGURES | View All (12)
Image
 Section AA′ from Gvirtzman et al. (2005) showing the north Sharon graben, which preserves a complete section of the Mount Scopus and Avedat groups and a 600–100 m thick Bet Guvrin (lower Saqiye) section. The faults bounding that graben are detected seismically and mapped in the top Judea Group structural map (Fleischer & Gafsou 2003). They are buried by the undisturbed Quaternary Kurkar Group and possibly also by the Pliocene Yafo Formation that wedges out west of the Pardes Hanna well. Stratigraphic correlation with a nearby outcrop (section BB′) indicates that faulting probably occurred during the Miocene (upper part of the Bet Guvrin Formation).
Published: 01 March 2008
Fig. 9.  Section AA′ from Gvirtzman et al . (2005) showing the north Sharon graben, which preserves a complete section of the Mount Scopus and Avedat groups and a 600–100 m thick Bet Guvrin (lower Saqiye) section. The faults bounding that graben are detected seismically and mapped in the top
Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 01 April 2011
Lithosphere (2011) 3 (2): 95–109.
..., 1968 ; Garfunkel, 1988 ). The overlying Avedat Group was deposited in the early to middle Eocene when the sea had reached as far as Egypt and part of Arabia ( Garfunkel, 1988 ). The late Eocene–Pliocene Saqiye Group, which is the focus of this study, is mainly composed of greenish to gray shales...
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Journal Article
Journal: AAPG Bulletin
Published: 01 April 1982
AAPG Bulletin (1982) 66 (4): 460–470.
.... 37 , p. 147 – 175 . Gvirzman , G. , 1970 , The Saqiye Group (late Eocene to early Pleistocene) in the coastal plain and Hashefela regions, Israel : Geol. Survey Israel Rept. OD/5/67 , 180 p. (in Hebrew, English summary). Gvirzman , G. , and B. Buchbinder , 1978...
FIGURES | View All (6)
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1979
AAPG Bulletin (1979) 63 (3): 324–340.
... , Submarine slumping and initiation of turbidity currents, in A. F. Richards, ed., Marine geotechnique : Urbana, Illinois , Univ. Illinois Press , p. 139 – 220 . Nachmias , J. , 1969 , Source rocks of the Saqiye Group sediments in the coastal plain of Israel—a heavy mineral study : Israel Jour...
FIGURES | View All (13)
Book Chapter

Series: AAPG Memoir
Published: 01 January 2014
DOI: 10.1306/13431857M106298
EISBN: 9781629812663
... and uplifted structures, and (4) the source rocks are organic-rich beds within the lower part of the Saqiye Group. The source rocks of the Yafo PS are sapropels and organic-rich marl beds that accumulated in the southeastern Mediterranean in the Upper Miocene and Pliocene (Figure 13D). Reservoir rocks were...
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Journal Article
Journal: AAPG Bulletin
Published: 01 February 1976
AAPG Bulletin (1976) 60 (2): 258–272.
.... Pub. 14 , p. 120 - 138 . Gvirtzman , G. , 1970 , The Saqiye Group (late Eocene to early Pleistocene) in the Coastal Plain and Hashephela regions, Israel : PhD thesis, Hebrew Univ. , 170 p. Gvirtzman , G. , and A. Klang , 1972 , A structural and depositional hinge line...
FIGURES | View All (15)
Journal Article
Published: 09 May 2017
Bulletin of the Seismological Society of America (2017) 107 (3): 1324–1335.
... ). Under the Kurkar Group, the Miocene Saqiye Group (mostly shale and marl) fills a series of canyons that had cut across the continental margin during several deep incision events, the last during the Messinian (late Miocene) Salinity Crisis ( Druckman et al. , 1995 ; Bar, 2010 ). These deep canyons...
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