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Venture Field

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Journal Article
Published: 18 August 2011
Canadian Journal of Earth Sciences (2011) 48 (9): 1293–1306.
... six wells in the Venture field were analysed by optical petrography, scanning electron microscopy (SEM), and electron microprobe. A total of 122 primary and secondary fluid inclusions were analysed from different cements. Primary aqueous inclusions in quartz overgrowths have homogenization...
FIGURES
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1992
AAPG Bulletin (1992) 76 (3): 318–338.
...P. L. Forbes; P. Ungerer; B. S. Mudford ABSTRACT We used a basin-scale model to reconstruct the development of overpressures in a sedimentary basin. The area of application is the Venture gas field, Nova Scotia, Canada. It is in an overpressured zone in which sedimentation rates have been...
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Series: AAPG Memoir
Published: 01 January 1992
DOI: 10.1306/M54555C5
EISBN: 9781629811086
... ABSTRACT The Venture gas field is a potential giant gas accumulation discovered in 1979 by the Mobil et al. Venture D-23 well drilled by Petro-Canada on a farm-in from Mobil. This well was completed at a total depth of 4945 m (16,224 ft). The field is located on the Scotian Shelf, 5 to 16 km (3...
Journal Article
Journal: AAPG Bulletin
Published: 01 October 1990
AAPG Bulletin (1990) 74 (10): 1640–1658.
... . In the Venture field, the abnormal pressures are confined below a depth of 4500 m and are associated with Upper Jurassic–Lower Cretaceous gas- and condensate-bearing sandstone reservoirs. The overpressures occur within normally compacted shales containing numerous overpressured sandstone reservoir beds...
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Journal Article
Published: 01 June 1990
Bulletin of Canadian Petroleum Geology (1990) 38 (2): 246–258.
...Brett S. Mudford ABSTRACT The Venture gas field, offshore Nova Scotia, contains a number of deep (>4.5 km) overpressured gas reservoirs. Within the overpressured zone, shales make up about 50 per cent of the bulk rock matrix. They have low permeability, low porosity, and nearly normal levels...
Journal Article
Journal: AAPG Bulletin
Published: 01 November 1989
AAPG Bulletin (1989) 73 (11): 1383–1396.
...Brett S. Mudford; Melvyn E. Best ABSTRACT The Venture gas field is a deep, overpressured gas reservoir on the Scotian Shelf off eastern Canada. Overpressuring occurs at depths below 4.5 km and is associated with significant quantities of gaseous hydrocarbons. The overpressured zone is composed...
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Journal Article
Journal: Geophysics
Published: 01 April 1996
Geophysics (1996) 61 (2): 422–436.
... different well logs, and permeability. Data from four wells in the Venture gas field (offshore eastern Canada) are organized into training and supervising data sets for BP-ANN modeling. Data from a fifth well in the same field are retained as an independent data set for testing. When applied to this test...
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—Log expressions of overpressured zone in the Venture field (Venture B-52 well). Normal compaction trend can be inferred from the logs with no change in log characteristics at the top of the overpressured zone. Minor decrease in resistivity in the deeper part of the overpressured zone we relate to the increase in salinity of formation fluids.
Published: 01 October 1990
Figure 6 —Log expressions of overpressured zone in the Venture field (Venture B-52 well). Normal compaction trend can be inferred from the logs with no change in log characteristics at the top of the overpressured zone. Minor decrease in resistivity in the deeper part of the overpressured zone we
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Fig. 2.
Published: 18 August 2011
Fig. 2. Map of Venture field showing location of individual wells in relation to faults (grey tones) and the inferred gas–water contacts (hatching) (modified from Canada – Nova Scotia Offshore Petroleum Board 2000 ). Letters A to H refer to reservoir compartments after Richards et al. (2008
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Stratigraphy of sandstone reservoirs in the Venture Field (modified from Wade and MacLean, 1990 and Sable Offshore Energy, 1996).
Published: 01 September 2005
Fig. 4. Stratigraphy of sandstone reservoirs in the Venture Field (modified from Wade and MacLean, 1990 and Sable Offshore Energy, 1996 ).
Image
—Location map of Venture field, Scotian Shelf, Canada. The extent of overpressuring and the main Venture wells are shown after Grant et aL (1986). A striped bar indicates the location of the modeled section, and dashed lines indicate the location of the nearest interpreted geological (Meneley, 1986) and seismic (Friedenreich, 1987) sections.
Published: 01 March 1992
Figure 1 —Location map of Venture field, Scotian Shelf, Canada. The extent of overpressuring and the main Venture wells are shown after Grant et aL (1986) . A striped bar indicates the location of the modeled section, and dashed lines indicate the location of the nearest interpreted geological
Image
—Geological cross section through the Venture field and Sable subbasin (from Meneley, 1986). Overpressured areas and gas accumulations are shown. Refer to Figure 1 for the location of the section.
Published: 01 March 1992
Figure 3 —Geological cross section through the Venture field and Sable subbasin (from Meneley, 1986 ). Overpressured areas and gas accumulations are shown. Refer to Figure 1 for the location of the section.
Image
—Geological logs and cross sections through Venture field. (A) Interpreted section as reported by Meneley (1986), and logs with tops of principal lithologic units from Mudford and Best (1989). (B) Part of the total modeled section related to the Venture field itself, and associated log for the reservoir units. See Figure 1 for the location of this section.
Published: 01 March 1992
Figure 4 —Geological logs and cross sections through Venture field. (A) Interpreted section as reported by Meneley (1986) , and logs with tops of principal lithologic units from Mudford and Best (1989) . (B) Part of the total modeled section related to the Venture field itself, and associated
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—Upper part of our modeled geological cross section through Venture field. The whole section is in Figure 5; its central part is detailed in Figure 4B. These sections correspond to that of Meneley (1986) in Figure 3. Locations of the sections are in Figure 1. See Figure 2 for lithologic symbols.
Published: 01 March 1992
Figure 6 —Upper part of our modeled geological cross section through Venture field. The whole section is in Figure 5 ; its central part is detailed in Figure 4B . These sections correspond to that of Meneley (1986) in Figure 3 . Locations of the sections are in Figure 1 . See Figure 2
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—Fluid pressure vs. depth in Venture field. Dots are composite data from the four main wells in the field as reported by Ervine and Bell (1987) and Mudford and Best (1989). Solid-line curves show the computed profiles assuming various fault permeability values: 10−24 m2 (curve 1, reference case), 10−23 m2 (curve 2), or 10−21 m2 (curve 3).
Published: 01 March 1992
Figure 9 —Fluid pressure vs. depth in Venture field. Dots are composite data from the four main wells in the field as reported by Ervine and Bell (1987) and Mudford and Best (1989) . Solid-line curves show the computed profiles assuming various fault permeability values: 10 −24 m 2 (curve 1
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—Sandstone porosity vs. depth in Venture field. Data are from sonic and porosity logs and from core measurements (Mudford and Best, 1989). The line and gray dots indicate the sandstone porosity profile computed in our reference case model.
Published: 01 March 1992
Figure 10 —Sandstone porosity vs. depth in Venture field. Data are from sonic and porosity logs and from core measurements ( Mudford and Best, 1989 ). The line and gray dots indicate the sandstone porosity profile computed in our reference case model.
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—Gas accumulation vs. depth in Venture field. The left part of the figure shows the complete modeled stratigraphic section (B43 well location) and corresponding gas saturation computed in our reference case model. The right part is a detailed description of actual reservoir units with the related gas zones as reported by Meneley (1986) plus computed gas saturation. See Figure 2 for lithologic symbols.
Published: 01 March 1992
Figure 12 —Gas accumulation vs. depth in Venture field. The left part of the figure shows the complete modeled stratigraphic section (B43 well location) and corresponding gas saturation computed in our reference case model. The right part is a detailed description of actual reservoir units
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—Lithostratigraphic correlation of five wells in the Venture field. Shown is a suite of mechanical logs from 300 m subsurface to total depth for the wells, formation boundaries, the overpressured zone boundaries, measured pressure gradients, and location of cores and cuttings used in the study. Stratigraphic position of gas-condensate and water-wet sandstones is also shown. The boundary of the very high overpressure zone coincide with the top of limestone bed 9.
Published: 01 October 1990
Figure 4 —Lithostratigraphic correlation of five wells in the Venture field. Shown is a suite of mechanical logs from 300 m subsurface to total depth for the wells, formation boundaries, the overpressured zone boundaries, measured pressure gradients, and location of cores and cuttings used
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—Stratigraphic cross section through Venture field showing fluid pressure vs. depth, resistivity logs, sonic logs, and tops of principal lithologic units. Heavy lines indicate boundaries between pressure regimes. Stratigraphic terminology follows that used by Mobil Oil Canada, Ltd. 1 MPa = 145 psi.
Published: 01 November 1989
Figure 4 —Stratigraphic cross section through Venture field showing fluid pressure vs. depth, resistivity logs, sonic logs, and tops of principal lithologic units. Heavy lines indicate boundaries between pressure regimes. Stratigraphic terminology follows that used by Mobil Oil Canada, Ltd. 1 MPa
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Published: 01 November 1989
Table 1 Permeabilities and Porosities Qf Venture Field Sandstones