Image log & dipmeter analysis courseCharacterisation of carbonate reservoir heterogeneity using borehole image logs... • Core calibration can be used to confirm – Image logs can only p
Trang 1Image log & dipmeter analysis course
Characterisation of carbonate reservoir
heterogeneity using borehole image logs
Trang 3• Borehole imaging tools
• Heterogeneities
– Structural – fractures/faults
– Depositional and diagenetic
– Pore system evaluation
• Reservoir rock typing
• Conclusions
Outline
Trang 4dish structures/dewatering
bioclasts soft sediment deformation scours/erosion surfaces grain size/bed thickness trends bedforms
channel lags
slumpsScales of investigation
Trang 5• Fractures
– Closed or open
– Natural or drilling induced
– Orientation, spacing and frequency
• Faults
– Determine strike and dip of the fault
– Determine rock displacement along the
fault
– Reservoir compartmentalisation
• In-situ stresses
– Borehole breakout
– Drilling induced fractures
– Potential & artificial fracturing
• Input to fracture modeling
3 6 7 2
N
Structural heterogeneities
Trang 8CBIL sm ACOUSTIC EARTH Imagersm
GR HEXDIP sm
5m
Fracture identification in oil based mud systems
Trang 9• For resistivity images:
– Conductive (dark image) =/= Open?
– Resistive (light) =/= Closed?
• For Acoustic Images
– low amplitude (dark) =/= Open?
– high amplitude (light) =/= Closed?
• Core calibration can be used to confirm
– Image logs can only provide an interpretive insight only
• Only dynamic data provide true insight into
Open versus closed fractures
Trang 10Flowmeter data
Conductive (open) fractures Acoustic
Calibration of image log data with core
Trang 11Fault identification
Trang 12BIU 1
BIU 3A BIU 2
FAULT A MAJOR
FAULT A
BIU 3A
Fault compartmentalisation
Trang 13• Well and fracture orientation
Schematic path down borehole (69* / 210*)
Mesozoic carbonate Oil staining
OBLIQUE-SLIP
Fracture distribution
Trang 14• Increased compartmentalisation
– Permeability barriers
• Increased communication
– Permeability conduits
• Overall objective - producibility
– Fracture model inputs
– Fault seal predictions
– Production enhancement
– Completion strategy
GO
Fracture characterisation
Trang 15• Image facies assigned on basis of image
character, open hole log response
• Image response is related to electrical or
acoustic properties, responds to rock
texture, fluid saturation and mineralogy
• Not possible to distinguish all core
lithofacies
• Calibration with core allows a meaningful
geological interpretation of image logs
Image facies
Trang 16Stylolitic seams
Conductive, tension gashes
Resistive cemented limestone
Dissolution seam
Stylolites and dissolution seams
Trang 17Cross-bedding
Trang 18STATIC DYNAMC STATIC DYNAMC STATIC DYNAMC
STATIC DYNAMC STATIC DYNAMC
STATIC DYNAMC
Nodular limestone image facies
Trang 190 10 20 30 40 50 60
Trang 20• Identification, orientation and
analysis of primary stratification
•porosity and permeability
distribution
Depositional heterogeneities
Trang 21Thin bed identification below the resolution of
openhole logs
STAT DYN
MINIPERM PROFILE
High resolution image log response
Trang 22Resistivity Image Acoustic Image Resistivity Image Acoustic Image
Resistivity Image Acoustic Image Resistivity Image Acoustic Image
Image log facies analysis – reef facies
Trang 23Oil based mud
Facies stacking patterns and dip analysis
Trang 24Image facies show
wackestone units
Trang 25Reservoir architecture
Trang 27Porosity classification
Trang 28Porosity classification
Fenestral
Shelter
Growth framework
Trang 29Pore fabric analysis
Trang 30Conductive (open?) fracture
Mouldic and vuggy porosity
Trang 31Vuggy carbonates seen in both acoustic and resistivity images
Image analysis can be used to threshold the imageand determine the % vuggy macroporosity and
degree of interconnectivity
Vuggy porosity
Trang 32_ 3.41
_ 1.64 _ 2.35
_ 0.21 _ 0.75
Microporous nodular limestones
Trang 33Cemented tight limestone
Microporous high permeability limestone
Porosity distribution from images
Trang 34A RRT has a unique reservoir quality but not
necessarily lithofacies
• Typically established in cored wells on basis of thin
section and SCAL data
• Extrapolation into uncored wells using openhole logs
and used to predict permeability
– fine scale permeability heterogeneity below resolution of
standard openhole logs.
– subtle changes in pore system can result in similar
porosities but permeability can vary by several orders of
magnitude.
Reservoir rock typing
Trang 35Conductive, high K vuggy skeletal grainstones
at base of units
Resistive, low K wackestones at top of
Trang 36Calculate K statistics and define K rank
Organise core poro-perm data by image
facies (cross-plots)
Group image facies into K classes:
“image rock types”
Assign image image rock types using porosity from openhole log data as guide to ‘background’ rock type
Assign K rank and value side image rock types interpretation
along-RRT/ permeability prediction workflow
Trang 37Image facies grouped
into image rock type
0.1 1 10 100 1000 10000
Trang 38Results from blind
test showing
predicted
permeability against
permeability from
core analysis data
RRT and permeability prediction
Trang 39Permeability prediction - dipmeter data
Trang 40RRT/permeability variations
Trang 41IRT
RRT & permeability prediction
Trang 42• Borehole image logs provide high resolution, oriented
data sets
– Provide key information on nature, orientation and scale of
fracture and fault systems, and compartmentalisation
– Provide information on texture, lithofacies and reservoir rock
types.
– Porosity and permeability distribution
– Identification of small-scale heterogeneity below resolution of
standard openhole logs
• Make more effective use of uncored wells to build,
constrain & validate 3D reservoir model realisations