The Oligo-Miocene deepwater system of the Levant Basin

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- 65 -cMiddle to Late MiocenebAfiq canyonFigure 37: Upper Miocene reservoir elements in the western part of the Afiq Canyon (a). The seismic profile (b) show a highamplitudereflection within the canyon. On a time slice (c) from 3D seismic survey C this reflection is part of a linear featurethat is interpreted as a channel fill.a
- 66 -SlopePartly Uplifted ?Hordos sandsShelfContinentalMiddle Miocene shorelineHazeva sandsExposed NubiansandstoneFigure 38: The paleogeography of the Levant margin during the Middle to upperMiocene. Continental drainage systems are marked by black arrows, submarinecanyons are marked by red dashed lines, and occurrences of shelf and deep-water sandsin wells are marked by yellow polygones. Hazeva and Hordos sands where the sourceof siliciclastics. The transport fron the NE may have been restricted by uplifting,associated with Syrian Arc deformation.
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The Oligo-Miocene deepwater system
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ITable of contentPageAbstract …
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IIIFigure 16: Depth map of the base
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- 2 -Oligo-Miocene sands were depos
Page 11 and 12:
- 4 -The discoveries of the early 2
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- 6 -the southeastern part of the b
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- 8 -Legend2D survey A2D survey B2D
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- 10 -2.2 Seismic dataThe seismic i
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- 12 -conditions, and possibly sedi
Page 21 and 22: - 14 -3.3.2 Lower Oligocene sedimen
Page 23 and 24: - 16 -Druckman, 2006; Bertoni and C
Page 25 and 26: - 18 -aSWNETWT (ms)bSWHanaha-1NEMav
Page 27 and 28: - 20 -aNWSETWT (ms)bYam West-1Ziqim
Page 29 and 30: - 22 -WETWT (ms)aYam Yafo-1multiple
Page 31 and 32: - 24 -NW SEaYam West-2Plio-Pleistoc
Page 33 and 34: - 26 -A third incision surface, mar
Page 35 and 36: - 28 -4.2.2 Deep, central part of t
Page 37 and 38: - 30 -10812591167Figure 13: Time st
Page 39 and 40: - 32 -10812591167Figure 15: Time st
Page 41 and 42: - 34 -HaifaQishon302829AtlitCaesare
Page 43 and 44: - 36 -Figure 19: Depth map on the t
Page 45 and 46: - 38 -SW NEAfiq Canyon Ashdod Canyo
Page 47 and 48: - 40 -The Beer Sheva-Afiq Canyon lo
Page 49 and 50: - 42 -SWNE SW NE SW NEPlio-Pleistoc
Page 51 and 52: - 44 -SWHanaha-1NE SW NE SW Hof Ash
Page 53 and 54: - 46 -BMSL1400m.1500200025003000Han
Page 55 and 56: - 48 -WE W E NW SEPlio-PleistoceneC
Page 57 and 58: - 50 -W EPlio-PleistoceneMessinian
Page 59 and 60: - 52 -S NPlio-PleistoceneM.-U. Mioc
Page 61 and 62: Figure 31: Stratigraphic section al
Page 63 and 64: - 56 -W ELower-slope and basin floo
Page 65 and 66: - 58 -SlopeSusita + En-GevsandsShel
Page 67 and 68: - 60 -In the Hadera Canyon the seis
Page 69 and 70: - 62 -Additional mechanisms for tra
Page 71: - 64 -The existence of channel fill
Page 75 and 76: - 68 -Oligo-Miocene sands were depo
Page 77 and 78: - 70 -Druckman, Y., Conway, B.H., E
Page 79 and 80: - 72 -Neev, D., 1960, A pre-Neogene
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The Oligo-Miocene deepwater system of the Levant Basin

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