Stéphanie Larmagnatespace.inrs.ca/5241/1/S3585.pdfThe Silurian Sayabec Formation reservoir...
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The Silurian Sayabec Formation reservoir potential in the Lower St. Lawrence River area, Québec, Canada 1 2 1 1 Stéphanie Larmagnat , Alexandre Aubiès-Trouilh , Michel Malo , Jasmin Raymond 1 INRS - Centre Eau Terre Environnement, 490, rue de la Couronne, Québec (Québec), Canada, G1K 9A9, 2 Ressources & Énergie SQUATEX Inc., 7055, boul. Taschereau, bureau 500, Brossard (Québec), Canada, J4Z 1A7 Fine-scale stratigraphy of the Sayabec Formation (Massé No. 2 well) In the Massé structure area, the average thickness of the Sayabec Fm is 300 meters. The succession is mainly carbonate interbedded with silty and/or argillaceous layers or variable thickness. The interval revealed four levels of reservoir quality (Figure 2). Reservoir analogs The Sayabec Fm facies can be considered as analogous of hydrothermal dolomite reservoir facies of the Albion-Scipio and Stony Point fields in the Trenton–Black River Fms (Ordovician, Michigan basin, USA; Figures 5 and 6) or the Ladyfern gas field (Devonian, Slave Point Reservoir, British Columbia; Boreen and Colquhoun, 2001; Smith, 2006). Methods Ÿ Mapping the Sayabec Fm in the Massé structure area (Figure 1); Ÿ Sedimentologic, stratigraphic and structural analysis at the outcrop scale; Ÿ Core logging of Massé No.1, Massé No.2 and Portage wells (approx. 2 000 meters); Ÿ Petrography of 54 thin sections from cores; Ÿ Integration of wireline logs, seismic interpretations and core logging into a 3D database. References Bourque, P.A., Brisebois, D., and Malo, M., 1995. Gaspé belt, In : Geology of the Appalachian-Caledonian Orogen in Canada and Greenland. H. Williams (ed). Geological Society of America, Geology of North America, v.F-1, p. 316-351. Boreen, T., and Colquhoun, K. (2001). Ladyfern, NEBC: major gas discovery in the Devonian Slave Point Formation. Davies, G. R., and Smith Jr, L. B. (2006). Structurally controlled hydrothermal dolomite reservoir facies: An overview. AAPG bulletin, 90(11), 1641- 1690. Lavoie, D., and Chi, G. (2001). The Lower Silurian Sayabec Formation in northern Gaspé: carbonate diagenesis and reservoir potential. Bulletin of Canadian Petroleum Geology, 49(2), 282-298. Ackowledgements Financial support of the project was provided by both Mitacs and Ressources and Energie Squatex Inc. through a Mitacs Acceleration postdoctoral fellowship (IT06251). We are gratefull to K. Bedard and F.A. Comeau (INRS-ETE) for their technical support throughout the project. Future works To improve our understanding of the Sayabec Fm reservoir potential, future works will focus on: Ÿ geochemistry analyses of fractures-filling mineral phases; Ÿ wireline log re-interpretations with new refined stratigraphic framework; Ÿ acquisition of new seismic lines in the Massé structure; Ÿ building a 3D geological model of the Sayabec Fm integrating all subsurface data available. The Massé structure The Massé structure belongs to the northern part of the Connecticut Valley-Gaspé synclinorium. In this area, the Taconian unconformity separates the Cambro-Ordovician strata (to the north) and the Siluro-Devonian sucession (to the south; Malo and Bourque, 1993; Bourque et al., 1995). The Massé structure is limited by two normal faults and its sedimentary sequence was preserved with little amount of deformation and only local brecciation and/or fracturing occurrences. Context Squatex has recently demonstrated interest for developing the oil and gas potential of the Lower St. Lawrence River area. The company drilled over 6000 meters of stratigraphic wells over the past 10 years. Several of them revealed oil or gas shows associated with naturally fractured zones, notably within the carbonate Silurian Sayabec Formation (Fm). This research project intended to assess the reservoir quality of sedimentary facies from this later lithostratigraphic unit in a prospective play, the Massé structure. Here we documented primary depositional facies and established a fine-scale stratigraphic framework. Lateral variation - Massé No. 1 Massé no.1 has a distinctive 40 m thick interval of hydrothermal dolomite (HTD; Figure 3) where highly connected porosity is common. Pores are associated with fractures, dissolved bioclasts and vugs. Size of voids ranges from millimetric to pluricentimetric and shape varies from circular/pseudo circular to lenticular. Lateral variation - HTD outcrop At Saint-Cleophas the Sayabec Fm is exposed in a quarry on the southern flank of the Lac Matapedia Syncline (Figure 4). The 20 m thick brecciated dolostone section consists of replacive and pore-filling saddle dolomite of hydrothermal origin (Lavoie and Chi, 2001; Lavoie and Morin, 2004). ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! Price Sayabec Rimouski Mont-Joli Luceville Saint-Noël Val-Brillant La Rédemption Saint-Gabriel Saint-Anaclet Pointe-au-Père Sainte-Blandine Saint-Léon-le-Grand Sainte-Angèle-de-Mérici Saint-Zénon-du-Lac-Humqui Saint-Narcisse-de-Rimouski 67°30'W 67°30'W 68°W 68°W 68°30'W 68°30'W 48°30'N 48°30'N 48°20'N 48°20'N 48°10'N 48°10'N Ü 0 5 10 15 20 Kilomètres Affleurements visités Traverses Chemin de Portage Figure 1 : Location map of the study area illustrating the 252 outcrop locations and cross-sections visited. Figure 2 : Detailed stratigraphic log of the Sayabec Fm within Massé No.2 well. Reservoir quality intervals (red arrows) are associated with variable porosity types (intergranular, intragranular, moldic and vuggy). Permeability is potentially high due to the presence of naturally fractured intervals (green arrows). Figure 3 : Fractured and vug-bearing intervals within Massé No.1 well. Width of the picture is approx. 30 mm. Figure 4 : Highly porous dolostone from the Sayabec Fm at the Saint-Cleophas quarry. Lavoie, D., and Morin, C. (2004). Hydrothermal dolomitization in the Lower Silurian Sayabec Formation in northern Gaspé-Matapédia (Québec): Constraint on timing of porosity and regional significance for hydrocarbon reservoirs. Bulletin of Canadian Petroleum Geology, 52(3), 256-269. Malo, M., and Bourque, P. A. (1993). Timing of the deformation events from Late Ordovician to Mid-Devonian in the Gaspé Peninsula. Geological Society of America Special Papers, 275, 101-122. Thornton, J. E., and Grammer, G. M. (2011). Prediction of Petrophysical Properties of Trenton-Black River (Ordovician) Reservoirs by Comparing Pore Architecture and Permeability to Sonic Velocity. ESAAPG abstract, AAPG Search and Discovery, 90142. Figure 5 : Left - Albion-Scipio HTD reservoir facies (from Thornton and Grammer, 2011). Right - Fractured and vugs showing interconnected porosity within the Sayabec Fm carbonate facies. Figure 6 : Left - Albion-Scipio burrowed reservoir facies with variable size porosity at the cm-scale (from Thornton and Grammer, 2011). Right - Similar fine-grained burrowed facies with matrix locally replaced by microdolomite in the Sayabec Fm. 100 µm Bioclastic wackestone with bioturbation Bioclastic grainstone Bioclastic packstone with large bioclast Coarse grained packstone with crinoids Bryozoan boundstones Peloidal packstone Breccia Laminated/bioturbated mudrock/siltstone Bioclastic wackestone to packstone Bioturbated siltstone/mudrock Naturally fractured interval 1582,9 1574,1 1565,2 1556,6 1547,7 1539,0 1530,2 1517,0 1587,3 1596,1 1605,0 1613,8 1622,6 1631,5 1640,2 1648,7 1697,0 1705,8 1714,7 1688,4 1679,5 1670,8 1661,9 1653,0 1719,0 1728,0 1736,0 1745,3 1753,8 1762,8 1780,3 1771,5 1784,8 1793,4 1801,2 Bioclastic packstone with large bioclasts Boundstone (bryozoan thickets) Bioclastic grainstone Coarse grained bioclastic packstone with Pentamerus rich layers Sample 1000 µm 1000 µm
Transcript of Stéphanie Larmagnatespace.inrs.ca/5241/1/S3585.pdfThe Silurian Sayabec Formation reservoir...
The Silurian Sayabec Formation reservoir potential in the Lower St. Lawrence River area, Québec, Canada
1 2 1 1Stéphanie Larmagnat , Alexandre Aubiès-Trouilh , Michel Malo , Jasmin Raymond
1INRS - Centre Eau Terre Environnement, 490, rue de la Couronne, Québec (Québec), Canada, G1K 9A9, 2 Ressources & Énergie SQUATEX Inc., 7055, boul. Taschereau, bureau 500, Brossard (Québec), Canada, J4Z 1A7
Fine-scale stratigraphy of the Sayabec Formation (Massé No. 2 well)In the Massé structure area, the average thickness of the Sayabec Fm is 300 meters. The succession is mainly carbonate interbedded with silty and/or argillaceous layers or variable thickness. The interval revealed four levels of reservoir quality (Figure 2).
Reservoir analogsThe Sayabec Fm facies can be considered as analogous of hydrothermal dolomite reservoir facies of the Albion-Scipio and Stony Point fields in the Trenton–Black River Fms (Ordovician, Michigan basin, USA; Figures 5 and 6) or the Ladyfern gas field (Devonian, Slave Point Reservoir, British Columbia; Boreen and Colquhoun, 2001; Smith, 2006).
MethodsŸ Mapping the Sayabec Fm in the Massé structure area
(Figure 1);Ÿ Sedimentologic, stratigraphic and structural analysis at
the outcrop scale;Ÿ Core logging of Massé No.1, Massé No.2 and Portage
wells (approx. 2 000 meters);Ÿ Petrography of 54 thin sections from cores; Ÿ Integration of wireline logs, seismic interpretations and
core logging into a 3D database.
ReferencesBourque, P.A., Brisebois, D., and Malo, M., 1995. Gaspé belt, In : Geology of the Appalachian-Caledonian Orogen in Canada and Greenland. H. Williams (ed). Geological Society of America, Geology of North America, v.F-1, p. 316-351. Boreen, T., and Colquhoun, K. (2001). Ladyfern, NEBC: major gas discovery in the Devonian Slave Point Formation.Davies, G. R., and Smith Jr, L. B. (2006). Structurally controlled hydrothermal dolomite reservoir facies: An overview. AAPG bulletin, 90(11), 1641-1690.Lavoie, D., and Chi, G. (2001). The Lower Silurian Sayabec Formation in northern Gaspé: carbonate diagenesis and reservoir potential. Bulletin of Canadian Petroleum Geology, 49(2), 282-298.
AckowledgementsFinancial support of the project was provided by both Mitacs and Ressources and Energie Squatex Inc. through a Mitacs Acceleration postdoctoral fellowship (IT06251). We are gratefull to K. Bedard and F.A. Comeau (INRS-ETE) for their technical support throughout the project.
Future worksTo improve our understanding of the Sayabec Fm reservoir potential, future works will focus on:Ÿ geochemistry analyses of fractures-filling mineral phases;Ÿ wireline log re-interpretations with new refined
stratigraphic framework; Ÿ acquisition of new seismic lines in the Massé structure;Ÿ building a 3D geological model of the Sayabec Fm
integrating all subsurface data available.
The Massé structureThe Massé structure belongs to the northern part of the Connecticut Valley-Gaspé synclinorium. In this area, the Taconian unconformity separates the Cambro-Ordovician strata (to the north) and the Siluro-Devonian sucession (to the south; Malo and Bourque, 1993; Bourque et al., 1995). The Massé structure is limited by two normal faults and its sedimentary sequence was preserved with little amount of deformation and only local brecciation and/or fracturing occurrences.
ContextSquatex has recently demonstrated interest for developing the oil and gas potential of the Lower St. Lawrence River area. The company drilled over 6000 meters of stratigraphic wells over the past 10 years. Several of them revealed oil or gas shows associated with naturally fractured zones, notably within the carbonate Silurian Sayabec Formation (Fm). This research project intended to assess the reservoir quality of sedimentary facies from this later lithostratigraphic unit in a prospective play, the Massé structure. Here we documented primary depositional facies and established a fine-scale stratigraphic framework.
Lateral variation - Massé No. 1 Massé no.1 has a distinctive 40 m thick interval of hydrothermal dolomite (HTD; Figure 3) where highly connected porosity is common. Pores are associated with fractures, dissolved bioclasts and vugs. Size of voids ranges from millimetric to pluricentimetric and shape varies from circular/pseudo circular to lenticular.
Lateral variation - HTD outcrop At Saint-Cleophas the Sayabec Fm is exposed in a quarry on the southern flank of the Lac Matapedia Syncline (Figure 4). The 20 m thick brecciated dolostone section consists of replacive and pore-filling saddle dolomite of hydrothermal origin (Lavoie and Chi, 2001; Lavoie and Morin, 2004).
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Price
Sayabec
Rimouski
Mont-Joli
Luceville
Saint-Noël
Val-Brillant
La RédemptionSaint-Gabriel
Saint-Anaclet
Pointe-au-Père
Sainte-Blandine
Saint-Léon-le-Grand
Sainte-Angèle-de-Mérici
Saint-Zénon-du-Lac-Humqui
Saint-Narcisse-de-Rimouski
67°30'W
67°30'W
68°W
68°W
68°30'W
68°30'W
48°3
0'N
48°3
0'N
48°2
0'N
48°2
0'N
48°1
0'N
48°1
0'N
Ü
0 5 10 15 20
Kilomètres
Affleurements visités
Traverses
Chemin de Portage
Figure 1 : Location map of the study area illustrating the 252 outcrop locations and cross-sections visited.
Figure 2 : Detailed stratigraphic log of the Sayabec Fm within Massé No.2 well. Reservoir quality intervals (red arrows) are associated with variable porosity types (intergranular, intragranular, moldic and vuggy). Permeability is potentially high due to the presence of naturally fractured intervals (green arrows).
Figure 3 : Fractured and vug-bearing intervals within Massé No.1 well. Width of the picture is approx. 30 mm.
Figure 4 : Highly porous dolostone from the Sayabec Fm at the Saint-Cleophas quarry.
Lavoie, D., and Morin, C. (2004). Hydrothermal dolomitization in the Lower Silurian Sayabec Formation in northern Gaspé-Matapédia (Québec): Constraint on timing of porosity and regional significance for hydrocarbon reservoirs. Bulletin of Canadian Petroleum Geology, 52(3), 256-269.Malo, M., and Bourque, P. A. (1993). Timing of the deformation events from Late Ordovician to Mid-Devonian in the Gaspé Peninsula. Geological Society of America Special Papers, 275, 101-122.Thornton, J. E., and Grammer, G. M. (2011). Prediction of Petrophysical Properties of Trenton-Black River (Ordovician) Reservoirs by Comparing Pore Architecture and Permeability to Sonic Velocity. ESAAPG abstract, AAPG Search and Discovery, 90142.
Figure 5 : Left - Albion-Scipio HTD reservoir facies (from Thornton and Grammer, 2011). Right - Fractured and vugs showing interconnected porosity within the Sayabec Fm carbonate facies.
Figure 6 : Left - Albion-Scipio burrowed reservoir facies with variable size porosity at the cm-scale (from Thornton and Grammer, 2011). Right - Similar fine-grained burrowed facies with matrix locally replaced by microdolomite in the Sayabec Fm.
100 µm
Bioclastic wackestone with bioturbation
Bioclastic grainstone
Bioclastic packstone with large bioclast
Coarse grained packstone with crinoids
Bryozoan boundstones
Peloidal packstone
Breccia
Laminated/bioturbated mudrock/siltstone
Bioclastic wackestone to packstone
Bioturbated siltstone/mudrock
Naturally fractured interval
1582,9
1574,1
1565,2
1556,6
1547,7
1539,0
1530,2
1517,0 1587,3
1596,1
1605,0
1613,8
1622,6
1631,5
1640,2
1648,7
1697,0
1705,8
1714,7
1688,4
1679,5
1670,8
1661,9
1653,0 1719,0
1728,0
1736,0
1745,3
1753,8
1762,8
1780,3
1771,5
1784,8
1793,4
1801,2
Bioclastic packstone with large bioclasts
Boundstone (bryozoan thickets)
Bioclastic grainstone
Coarse grained bioclastic packstone with Pentamerus rich layers
Sample
1000 µm
1000 µm
