3d facies modeling
DESCRIPTION
3D Facies Modelling project using Petrel software. Msc Geology and Geophysics Abstract The Montserrat and Sant Llorenç del Munt fan-delta complexes were developed during the Eocene in the Ebro basin. The depositional stratigraphic record of these fan deltas has been described as a made up by a several transgressive and regressive composite sequences each made up by several fundamental sequences. Each sequence set is in turn composed by five main facies belts: proximal alluvial fan, distal alluvial fan, delta front, carbonates platforms and prodelta. Using outcrop data from three composite sequences (Sant Vicenç, Vilomara and Manresa), a 3D facies model was built. The key sequential traces of the studied area georeferenced and digitalized on to photorealistic terrain models, were the hard data used as input to reconstruct the main surfaces, which are separating transgressive and regressive stacking patterns. Regarding the facies modelling has been achieved using a geostatistical algorithm in order to define the stacking trend and the interfingerings of adjacent facies belts, and five paleogeographyc maps to reproduce the paleogeometry of the facies belts within each system tract. The final model has been checked, using a real cross section, and analysed in order to obtain information about the Delta Front facies which are the ones susceptible to be analogous of a reservoir. Attending to the results including eight probability maps of occurrence, the transgressive sequence set of Vilomara is the greatest accumulation of these facies explained by its agradational component.TRANSCRIPT
Student: Marc Diviu Franco
Tutors: P. Cabello, M. López
Reservoir Geology and Geophysics master
Year 2013-14
Index1. Introduction
• Aims
• Geological setting
2. Workflow• Stratigraphic framework
• Fault Modelling
• Pillar Gridding
• Make Horizons
• Layering
• 3D facies Modeling
3. Results
4. Discussion
5. Conclusions
6. References
1.- Introduction
“3D models of subsurface heterogeneity have
proved to be important tools for the efficient
management of hydrocarbon reservoirs and
aquifers” (Matheron et al. 1987; Gundeso & Egeland 1990; Stanley et al.
1990; Weber & van Geuns 1990; Bryant & Flint 1993; Krum & Johnson 1993;
Deutsch & Hewett 1996; Drubrule & Damsleth 2001; Falivene et al. 2007; Jackson
et al. 2009; Sech et al. 2009; Cabello et al. 2011).
1-. Introduction 1.1. Aims
• Develop a realistic facies model
Data source: 8 Geological maps at scale 1:10000 (López-Blanco &
Piña (1992/93) , key sequential traces, Digital Elevation Models &
Orthophotomaps 1:5000 Institut Cartogràfic de Catalunya
• Improve the knowledge about the depositional framework of
deltaic pattern that can be related with the subsurface geology.
Modelling of geological frameworks is quite important to improve the
capacity of recover the sources placed in the underground.
Personal Expectations
Learn more about the modelization workflow acquiring the skills involved
in this process.
• Location
López Blanco M. (2012)
NE Spain, South-Eastern part
of Ebro basin
1.- Introduction1.2. Geological Setting
• Characterization
Average of sediment
thickness about 1000 m
Areal extension
SLM: 350/450 km2
Monts: 100/150 km2
1-. Geological Setting
• Facies belts
López Blanco M., (2006)
Cyclic stacking pattern (Agradational, Progradational or
Retrogradational)
Hyerarchical Sequential subdivision: 3 Orders of magnitude
• Milany composite megasequence
• Composite sequences 10__ >100 m thick
• Fundamental Sequences 1__>10 m thick
Study Area
Gomez Packard et al., (2012)
1-. Geological Setting
2-. MethodologyWorkflow
Stratigraphic Framework Fault Modelling Pillar Gridding
Make horizons Layering Facies modelling
2.1. Stratigraphic framework
2-. Methodology
- Georeferencing
2-. Methodology
2.1. Stratigraphic framework
- Addition and analysis of altitudes. DTM at scale of 1:5000
2-. Methodology
2.1. Stratigraphic framework
- Data Treatment
2-. Methodology
2.1. Stratigraphic framework
- Contour Maps
Elevation Control points
2.1. Stratigraphic framework
2-. Methodology
2-. Methodology
2.2. Fault Modelling
- Vertical Faults
Plan view3D view
2.2. Fault Modelling
Basement thrusts
“Els brucs thrust sheet” SW 18º towards the south
“Les Pedritxes” SE 12º towards the South East
2-. Methodology
Hanging wall Surfaces
Footwall Surfaces
“Els brucs”
“Les pedritxes”
2-. Methodology
2.3. Pilar Gridding
SEGMENT 1
SEGMENT 2
3D view
2D view
2.4. Make Horizons
2-. Methodology
2.5. Layering
2-. Methodology
TSS: 40 layers
RSS: 60 layers
2.7. Facies Modelling
2-. Methodology
• Geostatistical algorithm based on the truncation of the sum of a deterministic
expectation trend and a gaussian random field (TTG): Distribution terrigenous
facies belts. 2 different parts:
The linear expectation trend: Character of sequence sets
The gausian random field: interingering between adjacent facies belts
• Object Based Method (OBM): Carbonate Platforms
2.7. Facies Modelling
2-. Methodology
FM. Terrigenous
FM. Terrigenous Sep.
FM. DDF+PPD
FM. CarbonatePlatforms
Final Model
2.7. Facies Modelling
2-. Methodology
2.7. Facies Modelling
2-. Methodology
FM. Terrigenous
FM. Terrigenous Sep.
FM. DDF+PDD
FM. CarbonatePlatforms
Final Model
2.7. Facies Modelling
2-. Methodology
2.7. Facies Modelling
2-. Methodology
FM. Terrigenous
FM. Terrigenous Sep.
FM. DDF+PPD
FM. CarbonatePlatforms
Final Model
2.7. Facies Modelling
2-. Methodology
• Paleogeographic Maps
• 3D facies Model (10 realizations)
• 4 Stratigraphic Thickness Maps
• Proportions and volume of facies belts (average of realizations)
• Cross Sections
• Model and probability maps (average of realizations)
3-. Results and Discussion
• Paleogeographic Maps
3-. Results and Discussion
Prox_Dist_AF_TOP
Prox_Dist_AF_BASE
CLine_TOP
CLine_BASE
DF_Off_TOP
DF_Off_BASE
3-. Results and Discussion
• 3D facies Model (10 realizations)
3-. Results
3-. Results and Discussion
3-. Results and Discussion
Riera de Santa Maria Cross section
López-Blanco (1996)
3-. Results and Discussion
• Model
• Carbonatic Platforms
• Probability maps
• Compartmentalization
Probability models and maps
3-. Results and Discussion
4-. Conclussion
• Workflow applied is a good approximation to the reality
• The treatment of the final model have provided indications
about the place where the DF concentration is maximum
• Scale of work linked to the exploration one
• HC could be trapped at the dead-ends in the depositional pinch-
outs of the fan-delta front wedges. (Cabello, P., López-Blanco, M., Howell,
J., Arbués, P., Ramos, E. 2009)
• Model suitable to be analogue of similar subsurface geological
bodies
Further Work
5-. References
[1] Cabello, P., Falivene, O., López-Blanco, M., Howell, John A., Arbués, P., Ramons, E. (2011). An
outcrop-based comparison of facies modelling strategies in fan-delta reservoir analogues from the
Eocene Sant Llorenç del Munt fan-delta (NE Spain). Pet. Geocience, Vol. 17, pp. 65-90.
[2] Cabello, P., López-Blanco, M., Howell, J., Arbués, P., Ramos, E. (2009). Modelling facies belt
distribution in fan deltas coupling sequence stratigraphy and geostatics: The Eocene Sant Llorenç del
Munt example (Ebro foreland basin, NE Spain). Elsevier ltd. Marine and petroleum Geology.
[3] Dubrule, O. & Damsleth, E. 2001. Achievements and challenges in petroleum geostatistics.
Petroleum Geocience, 7, S1-7.
Deutsch, C.V. 1999. Reservoir modelling with publicly available software Computers & Geociences, 24,
69-76.
[4] Falivene O., Arbués, P., Howell, J., Muñoz, J.A., Fernandez, O. & Marzo, M. 2006, Hierarchical
geocellular facies modelling of a turbidite reservoir analogue from the Eocene of the Ainsa Basin, NE
Spain. Marine and Petroleum Geology, 23, 679-701.
[5] Gómez-Paccard, M., López-Blanco, M. et al. (2012). Tectonic and climatic controls on the sequential
arrangement of an alluvial fan/fan-delta complex(Montserrat,Eocene,Ebro Basin,NESpain). Basin
Research 24, 437-455. Pg. 3.
[6] Gundeso, R. & Egeland, O. 1990. SESIMIRA: a new geological tool for 3D modelling of
heterogenous reservoirs. In: Buller, A.T., Berg, E., Hjelmeland, O., Kleppe, J., Torsaeter, O. &
Aasen, J.O (eds) North Sea oil and Gas Reservoirs II.The Norwegian Institute of Technology,
Graham & Trotman, London, 363-371.
[7] Jackson, M.D., Hampson, G.J. & Sech, R.P. 2009. Three-dimensional modelling of a
shoreface-shelf parasequence reservoir analog: Part 2. Geologic controls on fluid flow and
hydrocarbon recovery. American Association of Ppetroleum Geologists Bulletin, 93, 1183-1208.
[8] López-Blanco, M. (2006). Stratigraphic and tectonosedimentary development of the Eocene
Sant Llorenç del Munt and Montserrat fan-delta complexes (Southeast Ebro basin margin,
Northeast Spain). CONTRIBUTIONS to SCIENCE, 3(2): 125-148. Pg. 134
[9] López-Blanco, M. (1993). Stratigraphy and sedimentary development of the Sant Llorenç
del Munt fan-delta complex (Eocene, southern Pyrenean foreland basin, norheast Spain). Int.
Ass. Sediment, 20,67-88.
[10] Matheron, G., Beucher, H., de Fouquet, H., Galli, A., Gerillot, D. & Ravenne, C. 1987.
Conditional simulation of the geometry of fluviodeltaic reservoirs. Paper SPE 16753, presented
at the 62nd Annual SPE Conference and Exhibition, Dallas, 27-30 September, 591-599.
Stanley, K.O., Jorde, K., Raestad, N. & Stockbridge, C.P. 1990. Stochastic modelling of
reservoir sandbodies for input to reservoir simulation, Snorre field , northern North Sea,
Norway. In: Buller, A.T., Berg, E., Hjelmeland, O., Kleppe, J, Torsaeter, O. & Aasen, J.O. (eds)
North Sea Oil and Gas Reservoirs II. The Norwegian Institute of Technology, Graham &
Trotman, London, 91-103.
5-. References
[11] Sech, R.P., Jackson, M.D. & Hampson, G.J. 2009. Three-dimensional modelling of a shoreface-
shelf parasequence reservoir analog: Part 1. Surface-based modelling to capture high-resolution
facies architecture. American Association of Petroleum Geologists Bulletin, 93, 1155-1181.
[12] Travé A. (1988). Estratigrafia i Sedimentologia dels dipòsits deltaics de l’eocè mitjà-superior al
sector de Manresa. Universitat de Barcelona Phd thesis, pp. 85.
Valles J.C. (1985). Facies y evolución del complejo de abanico deltaico de Montserrat en la
transversal del rio Llobregat (Eoceno, Provincia de Barcelona). Phd thesis, pp. 66
5-. References