8
* Corresponding author, Tel: * Corresponding author, Tel: * Corresponding author, Tel: * Corresponding author, Tel: +234 +234 +234 +234-806 806 806 806-2 2 2 2 HY HY HY HYDROCARBON PROSP DROCARBON PROSP DROCARBON PROSP DROCARBON PROSP PETROPHYSICA PETROPHYSICA PETROPHYSICA PETROPHYSICA O. O. O. O. O O O O 1, 2 DEPARTMENT OF CHEMICAL A 3 INSTITUTE FOR GROUNDWATER E E E- - -mail addresses: mail addresses: mail addresses: mail addresses: 1 toyin.ol ABSTRACT ABSTRACT ABSTRACT ABSTRACT Reservoir evaluation of “OK” field Reservoir evaluation of “OK” field Reservoir evaluation of “OK” field Reservoir evaluation of “OK” field in so in so in so in so lithological uni lithological uni lithological uni lithological units and ts and ts and ts and quantify the hydro quantify the hydro quantify the hydro quantify the hydro and structural and structural and structural and structural analys analys analys analyse e es s s. . . To achieve thes To achieve thes To achieve thes To achieve thes the geometry of the identified the geometry of the identified the geometry of the identified the geometry of the identified reserv reserv reserv reserv characteristics characteristics characteristics characteristics. . . . It was ded It was ded It was ded It was deduced uced uced uced that that that that intercalation and wi intercalation and wi intercalation and wi intercalation and with a rhythmi th a rhythmi th a rhythmi th a rhythmic str c str c str c str bearing reservoirs were bearing reservoirs were bearing reservoirs were bearing reservoirs were delineated on delineated on delineated on delineated on estimates estimates estimates estimates in the in the in the in the reservoirs; R reservoirs; R reservoirs; R reservoirs; R 1 1 1 and R and R and R and R 2 2 2 w w w w Amplitude analysis sh Amplitude analysis sh Amplitude analysis sh Amplitude analysis showed that most owed that most owed that most owed that most anomalies) anomalies) anomalies) anomalies). . . . In terms of structure, In terms of structure, In terms of structure, In terms of structure, 3 3 3- - -D s D st D s D st anticline, with a closed trapping mech anticline, with a closed trapping mech anticline, with a closed trapping mech anticline, with a closed trapping mech Hence the reservoir units within the fie Hence the reservoir units within the fie Hence the reservoir units within the fie Hence the reservoir units within the fie Keywords: Keywords: Keywords: Keywords: Reservoirs, Fault, Hydrocar 1. 1. 1. 1. INTRODUCTION INTRODUCTION INTRODUCTION INTRODUCTION Petroleum resources remain vital to several nations of the world, but the e exploitation makes interpretation of e with a high level of precision in petroleum production [1]. At the ex Petroleum Geoscientist needs to minimum five critical ingredients tha with petroleum accumulation; the thermal maturity, reservoir, trap significant of well articulated explo petroleum prospecting necessitate involving petrophysical evaluation interpretation within the Niger Delta. The Niger-Delta is one of the hydrocarbon provinces with pr recoverable reserves of approximatel of oil and a vast gas resources [2]. Th the most explored in terms of oil a numerous acquired wireline and seism 266 266 266 266-4338 4338 4338 4338 PECTING OVER ‘OK’ PECTING OVER ‘OK’ PECTING OVER ‘OK’ PECTING OVER ‘OK’ FIELD, NIGER FIELD, NIGER FIELD, NIGER FIELD, NIGER AL AND AL AND AL AND AL AND SEISMIC SEISMIC SEISMIC SEISMIC ATTRIBUTE ATTRIBUTE ATTRIBUTE ATTRIBUTES AN AN AN AN Ol Ol Ol Ologe oge oge oge 1 , , , , A. S. A. S. A. S. A. S. Bankole ankole ankole ankole 2, * , * , * , * and and and and A. S. Oke A. S. Oke A. S. Oke A. S. Oke 1, , , , 3 AND GEOLOGICAL SCIENCES, AL-HIKMAH UNIVERSITY STUDIES, UNIVERSITY OF FREE STATE, BLOEMFONTE [email protected], 2 [email protected], 3 s southwestern offshore Niger Delta was carried southwestern offshore Niger Delta was carried southwestern offshore Niger Delta was carried southwestern offshore Niger Delta was carried out out out out rocarbon within the reservoir rocarbon within the reservoir rocarbon within the reservoir rocarbon within the reservoir using an interplay a using an interplay a using an interplay a using an interplay a ese ese ese ese aim aim aim aims s s, , , the work the work the work the work involved analysing and interpre involved analysing and interpre involved analysing and interpre involved analysing and interpre rvoir rvoir rvoir rvoir s s sand and and ands s s which which which which consequently consequently consequently consequently led to the dete led to the deter led to the dete led to the deter t the lithological units were t the lithological units were t the lithological units were t the lithological units were shale shale shale shales s s and sands and sands and sands and sands tructure. The shale to sand ratio increase tructure. The shale to sand ratio increase tructure. The shale to sand ratio increase tructure. The shale to sand ratio increased d d with with with with n well logs namely; r n well logs namely; r n well logs namely; r n well logs namely; reservoir R eservoir R eservoir R eservoir R 1 1 1 and and and and R R R 2 2 2 . . . . Hydrocarb Hydrocarb Hydrocarb Hydrocarb were very high varying between were very high varying between were very high varying between were very high varying between 0.6 and 0.75 an 0.6 and 0.75 an 0.6 and 0.75 an 0.6 and 0.75 an st structural highs st structural highs st structural highs st structural highs coincided with zones of anom coincided with zones of anom coincided with zones of anom coincided with zones of anom struc struc struc structural int tural int tural int tural interpretation erpretation erpretation erpretation revealed that revealed that revealed that revealed that“ “OK OK OK OK” field is field is field is field is chanism for the D series and fault/dip trapping m chanism for the D series and fault/dip trapping m chanism for the D series and fault/dip trapping m chanism for the D series and fault/dip trapping m eld are porous and with substantial hydrocarbon t eld are porous and with substantial hydrocarbon t eld are porous and with substantial hydrocarbon t eld are porous and with substantial hydrocarbon t rbon, Seismic, Amplitudes, Structures the economy of enormous cost of exploratory data ndispensable in xploration stage establish the at are associated e source rock, and seal. The oration data in ed this work; n and seismic world’s major roven ultimate ly 26 billion bbl he basin remains and gas with a mic data. The ease to find reservoi while the need for oil and g are difficulties in findin reservoirs with higher risk within this hydocarbon pro presence of structural anom successful hydrocarbon pro for quantitative seismic inte initial qualitative seismic ap of petrophysical and seism become a key strategy interpretation [5]. A bro integrated approach is r quantitative assessment of [6]. Therefore a comprehen field with a suite of softwar complex seismic attributes needed especially for hydr light of these, this work is fo potential reservoirs using p inferences, assessment of Nigerian Journa Vol. 33. No. 3 Copyrig University of Nige http://dx.doi.org/ R DELTA USING R DELTA USING R DELTA USING R DELTA USING NALYSIS NALYSIS NALYSIS NALYSIS Y, ILORIN, NIGERIA. EIN, SOUTH AFRICA [email protected] ut with a view to identify the ut with a view to identify the ut with a view to identify the ut with a view to identify the among petrophysics, seismic among petrophysics, seismic among petrophysics, seismic among petrophysics, seismic reting reting reting reting seismic attributes and seismic attributes and seismic attributes and seismic attributes and ermination of ermination of ermination of ermination of the reservoir the reservoir the reservoir the reservoir dstone dstone dstone dstones s s which occur as an which occur as an which occur as an which occur as an h depth. h depth. h depth. h depth. Two Two Two Two hydrocarbon hydrocarbon hydrocarbon hydrocarbon- - - rbon saturation rbon saturation rbon saturation rbon saturation and and and and porosity porosity porosity porosity nd 0.21 to 0.27 respectively. nd 0.21 to 0.27 respectively. nd 0.21 to 0.27 respectively. nd 0.21 to 0.27 respectively. omalous amplitude omalous amplitude omalous amplitude omalous amplitude (seismic (seismic (seismic (seismic is characterized by a rollover is characterized by a rollover is characterized by a rollover is characterized by a rollover mechanism in the E mechanism in the E mechanism in the E mechanism in the E series. series. series. series. that that that that were were were were well trapped well trapped well trapped well trapped. . . irs are decreasing rapidly gas is increasing [3]. There ng smaller, more subtle ks and costs. Also, drilling ovince has shown that the malies does not guarantee oduction. These have called erpretation rather than the pproach [4]. An integration mic attributes analyses has in quantitative seismic oad multidisciplinary and required for a thorough petroleum prospect areas nsive interpretation of the re that enhance imaging the s within the subsurface is rocarbon mapping. In the ocused towards identifying petrophysical analysis and hydrocarbon prospective al of Technology (NIJOTECH) 3, July 2014, pp. 401 – 408 ght© Faculty of Engineering, eria, Nsukka, ISSN: 1115-8443 www.nijotech.com /10.4314/njt.v33i3.19

HYHHYYHY DROCARBON PROSPECTING OVER ‘OK’ …

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Microsoft Word - Nijotech_vol_33_no_3_pp_401_408PETROPHYSICAL ANDPETROPHYSICAL ANDPETROPHYSICAL ANDPETROPHYSICAL AND
O.O.O.O. OlOlOlOl 1111,,,, 2222 DEPARTMENT OF CHEMICAL AND
3333 INSTITUTE FOR GROUNDWATER
ABSTRACTABSTRACTABSTRACTABSTRACT
Reservoir evaluation of “OK” field Reservoir evaluation of “OK” field Reservoir evaluation of “OK” field Reservoir evaluation of “OK” field in southwestern offshore Niger Delta was carriedin southwestern offshore Niger Delta was carriedin southwestern offshore Niger Delta was carriedin southwestern offshore Niger Delta was carried
lithological unilithological unilithological unilithological units andts andts andts and quantify the hydrocarbon within the reservoirquantify the hydrocarbon within the reservoirquantify the hydrocarbon within the reservoirquantify the hydrocarbon within the reservoir
and structural and structural and structural and structural analysanalysanalysanalyseeeessss.... To achieve theseTo achieve theseTo achieve theseTo achieve these
the geometry of the identified the geometry of the identified the geometry of the identified the geometry of the identified reservoir reservoir reservoir reservoir
characteristicscharacteristicscharacteristicscharacteristics. . . . It was dedIt was dedIt was dedIt was deduceduceduceduced that the lithological units werethat the lithological units werethat the lithological units werethat the lithological units were
intercalation and wiintercalation and wiintercalation and wiintercalation and with a rhythmith a rhythmith a rhythmith a rhythmic structure. The shale to sand ratio increasec structure. The shale to sand ratio increasec structure. The shale to sand ratio increasec structure. The shale to sand ratio increase
bearing reservoirs werebearing reservoirs werebearing reservoirs werebearing reservoirs were delineated on well logs namely; rdelineated on well logs namely; rdelineated on well logs namely; rdelineated on well logs namely; r
estimatesestimatesestimatesestimates in the in the in the in the reservoirs; Rreservoirs; Rreservoirs; Rreservoirs; R1111 and Rand Rand Rand R2222 were very high varying between were very high varying between were very high varying between were very high varying between
Amplitude analysis shAmplitude analysis shAmplitude analysis shAmplitude analysis showed that most structural highsowed that most structural highsowed that most structural highsowed that most structural highs
anomalies)anomalies)anomalies)anomalies). . . . In terms of structure, In terms of structure, In terms of structure, In terms of structure, 3333----D strucD strucD strucD struc
anticline, with a closed trapping mechanism for the D series and fault/dip trapping mechanism in the Eanticline, with a closed trapping mechanism for the D series and fault/dip trapping mechanism in the Eanticline, with a closed trapping mechanism for the D series and fault/dip trapping mechanism in the Eanticline, with a closed trapping mechanism for the D series and fault/dip trapping mechanism in the E
Hence the reservoir units within the field are porous and with substantial hydrocarbon that Hence the reservoir units within the field are porous and with substantial hydrocarbon that Hence the reservoir units within the field are porous and with substantial hydrocarbon that Hence the reservoir units within the field are porous and with substantial hydrocarbon that
Keywords:Keywords:Keywords:Keywords: Reservoirs, Fault, Hydrocarbon,
Petroleum resources remain vital to the economy of
several nations of the world, but the enormous cost of
exploitation makes interpretation of exploratory data
with a high level of precision indispensable in
petroleum production [1]. At the exploration stage
Petroleum Geoscientist needs to
with petroleum accumulation; the source rock
thermal maturity, reservoir, trap and
significant of well articulated exploration data in
petroleum prospecting necessitated this work;
involving petrophysical evaluation and seismic
interpretation within the Niger Delta.
The Niger-Delta is one of the wor
hydrocarbon provinces with proven ultimate
recoverable reserves of approximately 26 billion bbl
of oil and a vast gas resources [2]. The basin remains
the most explored in terms of oil and gas with a
numerous acquired wireline and seismic
266266266266----4338433843384338
DROCARBON PROSPECTING OVER ‘OK’DROCARBON PROSPECTING OVER ‘OK’DROCARBON PROSPECTING OVER ‘OK’DROCARBON PROSPECTING OVER ‘OK’ FIELD, NIGER DELTA USINGFIELD, NIGER DELTA USINGFIELD, NIGER DELTA USINGFIELD, NIGER DELTA USING
PETROPHYSICAL ANDPETROPHYSICAL ANDPETROPHYSICAL ANDPETROPHYSICAL AND SEISMICSEISMICSEISMICSEISMIC ATTRIBUTEATTRIBUTEATTRIBUTEATTRIBUTESSSS ANALYSISANALYSISANALYSISANALYSIS
OlOlOlOlogeogeogeoge1111, , , , A. S. A. S. A. S. A. S. BBBBankoleankoleankoleankole2222, *, *, *, * andandandand A. S. OkeA. S. OkeA. S. OkeA. S. Oke1111, , , , 3333
HEMICAL AND GEOLOGICAL SCIENCES, AL-HIKMAH UNIVERSITY
ROUNDWATER STUDIES, UNIVERSITY OF FREE STATE, BLOEMFONTEIN
[email protected], 2222 [email protected], 3333 [email protected]
in southwestern offshore Niger Delta was carriedin southwestern offshore Niger Delta was carriedin southwestern offshore Niger Delta was carriedin southwestern offshore Niger Delta was carried out with a view to identify the out with a view to identify the out with a view to identify the out with a view to identify the
quantify the hydrocarbon within the reservoirquantify the hydrocarbon within the reservoirquantify the hydrocarbon within the reservoirquantify the hydrocarbon within the reservoir using an interplay among petrophysics, seismic using an interplay among petrophysics, seismic using an interplay among petrophysics, seismic using an interplay among petrophysics, seismic
To achieve theseTo achieve theseTo achieve theseTo achieve these aimaimaimaimssss,,,, the work the work the work the work involved analysing and interpreting involved analysing and interpreting involved analysing and interpreting involved analysing and interpreting
reservoir reservoir reservoir reservoir ssssandandandandssss which which which which consequently consequently consequently consequently led to the determination of led to the determination of led to the determination of led to the determination of
that the lithological units werethat the lithological units werethat the lithological units werethat the lithological units were shaleshaleshaleshalessss and sandstoneand sandstoneand sandstoneand sandstone
c structure. The shale to sand ratio increasec structure. The shale to sand ratio increasec structure. The shale to sand ratio increasec structure. The shale to sand ratio increasedddd with depth.with depth.with depth.with depth.
delineated on well logs namely; rdelineated on well logs namely; rdelineated on well logs namely; rdelineated on well logs namely; reservoir Reservoir Reservoir Reservoir R1111 andandandand RRRR2222. . . . Hydrocarbon saturationHydrocarbon saturationHydrocarbon saturationHydrocarbon saturation
were very high varying between were very high varying between were very high varying between were very high varying between 0.6 and 0.75 and 0.21 to 0.27 respectively.0.6 and 0.75 and 0.21 to 0.27 respectively.0.6 and 0.75 and 0.21 to 0.27 respectively.0.6 and 0.75 and 0.21 to 0.27 respectively.
owed that most structural highsowed that most structural highsowed that most structural highsowed that most structural highs coincided with zones of anomalous amplitudecoincided with zones of anomalous amplitudecoincided with zones of anomalous amplitudecoincided with zones of anomalous amplitude
D strucD strucD strucD structural inttural inttural inttural interpretation erpretation erpretation erpretation revealed thatrevealed thatrevealed thatrevealed that““““OKOKOKOK”””” field is characterized by a rollover field is characterized by a rollover field is characterized by a rollover field is characterized by a rollover
anticline, with a closed trapping mechanism for the D series and fault/dip trapping mechanism in the Eanticline, with a closed trapping mechanism for the D series and fault/dip trapping mechanism in the Eanticline, with a closed trapping mechanism for the D series and fault/dip trapping mechanism in the Eanticline, with a closed trapping mechanism for the D series and fault/dip trapping mechanism in the E
Hence the reservoir units within the field are porous and with substantial hydrocarbon that Hence the reservoir units within the field are porous and with substantial hydrocarbon that Hence the reservoir units within the field are porous and with substantial hydrocarbon that Hence the reservoir units within the field are porous and with substantial hydrocarbon that
ydrocarbon, Seismic, Amplitudes, Structures
the enormous cost of
indispensable in
articulated exploration data in
Delta is one of the world’s major
with proven ultimate
The basin remains
the most explored in terms of oil and gas with a
seismic data.
while the need for oil and gas is increasing
are difficulties in finding smaller, more subtle
reservoirs with higher risks and costs
within this hydocarbon province has shown tha
presence of structural anomalies does not guarantee
successful hydrocarbon production.
become a key strategy in quantitative seismic
interpretation [5]. A broad multidisciplinary and
integrated approach is required for a thoro
quantitative assessment of
needed especially for hydrocarbon mapping.
light of these, this work is focused
potential reservoirs using petrophysical analysis
inferences, assessment of hydrocarbon prospective
Nigerian Journal of Technology (NIJOTECH)
Vol. 33. No. 3
Copyright© Faculty of Engineering,
http://dx.doi.org/10.4314/njt.v33i3.19
FIELD, NIGER DELTA USINGFIELD, NIGER DELTA USINGFIELD, NIGER DELTA USINGFIELD, NIGER DELTA USING
ANALYSISANALYSISANALYSISANALYSIS
[email protected]
out with a view to identify the out with a view to identify the out with a view to identify the out with a view to identify the
using an interplay among petrophysics, seismic using an interplay among petrophysics, seismic using an interplay among petrophysics, seismic using an interplay among petrophysics, seismic
involved analysing and interpreting involved analysing and interpreting involved analysing and interpreting involved analysing and interpreting seismic attributes and seismic attributes and seismic attributes and seismic attributes and
led to the determination of led to the determination of led to the determination of led to the determination of the reservoirthe reservoirthe reservoirthe reservoir
and sandstoneand sandstoneand sandstoneand sandstonessss which occur as an which occur as an which occur as an which occur as an
with depth.with depth.with depth.with depth. TwoTwoTwoTwo hydrocarbonhydrocarbonhydrocarbonhydrocarbon----
Hydrocarbon saturationHydrocarbon saturationHydrocarbon saturationHydrocarbon saturation and and and and porosity porosity porosity porosity
0.6 and 0.75 and 0.21 to 0.27 respectively.0.6 and 0.75 and 0.21 to 0.27 respectively.0.6 and 0.75 and 0.21 to 0.27 respectively.0.6 and 0.75 and 0.21 to 0.27 respectively.
coincided with zones of anomalous amplitudecoincided with zones of anomalous amplitudecoincided with zones of anomalous amplitudecoincided with zones of anomalous amplitude (seismic (seismic (seismic (seismic
field is characterized by a rollover field is characterized by a rollover field is characterized by a rollover field is characterized by a rollover
anticline, with a closed trapping mechanism for the D series and fault/dip trapping mechanism in the Eanticline, with a closed trapping mechanism for the D series and fault/dip trapping mechanism in the Eanticline, with a closed trapping mechanism for the D series and fault/dip trapping mechanism in the Eanticline, with a closed trapping mechanism for the D series and fault/dip trapping mechanism in the E series. series. series. series.
Hence the reservoir units within the field are porous and with substantial hydrocarbon that Hence the reservoir units within the field are porous and with substantial hydrocarbon that Hence the reservoir units within the field are porous and with substantial hydrocarbon that Hence the reservoir units within the field are porous and with substantial hydrocarbon that werewerewerewere well trappedwell trappedwell trappedwell trapped....
find reservoirs are decreasing rapidly
oil and gas is increasing [3]. There
difficulties in finding smaller, more subtle
rs with higher risks and costs. Also, drilling
within this hydocarbon province has shown that the
presence of structural anomalies does not guarantee
successful hydrocarbon production. These have called
ntitative seismic interpretation rather than the
approach [4]. An integration
seismic attributes analyses has
A broad multidisciplinary and
quantitative assessment of petroleum prospect areas
. Therefore a comprehensive interpretation of the
field with a suite of software that enhance imaging the
complex seismic attributes within the subsurface is
needed especially for hydrocarbon mapping. In the
is focused towards identifying
3, July 2014, pp. 401 – 408
Copyright© Faculty of Engineering,
www.nijotech.com
HHHHYDROCARBON YDROCARBON YDROCARBON YDROCARBON PPPPROSPECTING OVER ROSPECTING OVER ROSPECTING OVER ROSPECTING OVER ‘O‘O‘O‘OKKKK’’’’ FFFFIELDIELDIELDIELD,,,, NNNNIGER IGER IGER IGER DDDDELTA USING ELTA USING ELTA USING ELTA USING PPPPETROPHYSICAL AND ETROPHYSICAL AND ETROPHYSICAL AND ETROPHYSICAL AND SSSSEISMIC EISMIC EISMIC EISMIC AAAATTRIBUTES TTRIBUTES TTRIBUTES TTRIBUTES O. OlogeO. OlogeO. OlogeO. Ologe, et al, et al, et al, et al
Nigerian Journal of Technology, Nigerian Journal of Technology, Nigerian Journal of Technology, Nigerian Journal of Technology, Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014 402402402402
areas using seismic attributes; and to describe the
geometry of the identified reservoirs.
2. 2. 2. 2. GEOLOGY OF THE AREAGEOLOGY OF THE AREAGEOLOGY OF THE AREAGEOLOGY OF THE AREA
The study area covers an area of approximately 41km2
which is located within the offshore southwestern,
Niger Delta (Figure 1). The Niger Delta province has
one identified petroleum system which is referred to
as Akata-Agbada petroleum system [7]. The
stratigraphic units in chronological order are; Akata,
Agbada and Benin Formations [8]. The Akata
Formation is the oldest which unconformably rest on
a Precambrian Basement Complex. It is made up of
mostly marine shale and it is the main source rock in
the basin. The Akata Formation is overlain by Agbada
Formation which is characterised by sandstone and
shale. With increasing depth, the volume of the shale
tends to increase relative to the sand volume. The
Agbada Shale is the main reservoir rock in the Niger
Delta, though it might also serve as a secondary source
rock due to its shale content. The Benin Formation is
the youngest and it overlies the Agbada Formation
and it is typical of coastal sands.
3. 3. 3. 3. MATERIALS AND METHODSMATERIALS AND METHODSMATERIALS AND METHODSMATERIALS AND METHODS
The data set for this study included soft copy data of
3D seismic volume, composite well logs comprising
gamma ray, resistivity, density and neutron logs from
two wells. Schlumberger’s Petrel software was used to
interpret the data. The interpretation procedure
involved integration of well logs with seismic data,
seismic structural analysis, seismic attributes analysis
and petrophysical analysis. Gamma-ray log measures
natural radioactivity in formations [9], therefore
enabling qualitative identification of zones of shale
(interpreted from high gamma readings) and sand
(low gamma readings). Identification of hydrocarbon
bearing zones was done following the concept of [10];
using deep resistivity log (LLD). Reservoir properties
of the delineated geologic pay zones such as net
reservoir thickness, gross reservoir thickness,
porosity, water saturation and hydrocarbon
saturations were determined from logs and using
relevant equations such as:
NW = 1 − (NO) (2)
In (1) and (2), NO is the water saturation of the
uninvaded zone (Archie method), RO is the resistivity
of formation water at formation temperature, RU is the
true resistivity of formation, Φ is the porosity, a is the
tortuosity factor, m is the cementation exponent, n is
the saturation exponent which varies from 1.8 to 2.5
and NW is the hydrocarbon saturation.
Figure 1: Location Map of Nigeria showing the Niger Delta and the Study Area.
HHHHYDROCARBON YDROCARBON YDROCARBON YDROCARBON PPPPROSPECTING OVER ROSPECTING OVER ROSPECTING OVER ROSPECTING OVER ‘O‘O‘O‘OKKKK’’’’ FFFFIELDIELDIELDIELD
Nigerian Journal of Technology, Nigerian Journal of Technology, Nigerian Journal of Technology, Nigerian Journal of Technology,
Porosity values for the identified hydroc
reservoirs were estimated using (3):
S = (ma – b)
the fluid density (flushed zone) and
matrix density.
reservoirs, the measured porosity was corrected for
the volume of shale using [11].
S\]^^ = S_ − aW × SbaW
Dsh is the density porosity of nearby shale.
Well-to-seismic tie of the hydrocarbon reservoirs
using check-shot data was done followed
and fault interpretation. Interpretation procedure of
the main structural framework can be summarized as
follows:
ties using checkshots.
2) Manual picking of horizons at this spot on inlines
and crosslines. A combination of volume
autotracking and interpolation were then used to
infill the interpretation.
and other related secondary faults) on the seism
sections.
Figure 2: Seismic section showing the picked horizons and the fault types
IELDIELDIELDIELD,,,, NNNNIGER IGER IGER IGER DDDDELTA USING ELTA USING ELTA USING ELTA USING PPPPETROPHYSICAL AND ETROPHYSICAL AND ETROPHYSICAL AND ETROPHYSICAL AND SSSSEISMIC EISMIC EISMIC EISMIC AAAATTRIBUTES TTRIBUTES TTRIBUTES TTRIBUTES
Nigerian Journal of Technology, Nigerian Journal of Technology, Nigerian Journal of Technology, Nigerian Journal of Technology, Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014
Porosity values for the identified hydrocarbon
(3)
the fluid density (flushed zone) and ma is the rock
Because of the considerable presence of shale in the
reservoirs, the measured porosity was corrected for
(4)
hale volume and
seismic tie of the hydrocarbon reservoirs
was done followed by horizon
. Interpretation procedure of
be summarized as
of horizons at this spot on inlines
and crosslines. A combination of volume
autotracking and interpolation were then used to
3) Identification of faults networks (synthetic faults
and other related secondary faults) on the seismic
Amplitude extractions were generated for all the
interpreted horizons and were
structural maps to conf
amplitude were analyzed using the horizon slices
4. 4. 4. 4. RESULTS AND DISCUSSIONRESULTS AND DISCUSSIONRESULTS AND DISCUSSIONRESULTS AND DISCUSSION
4.1 4.1 4.1 4.1 Structural AnalysisStructural AnalysisStructural AnalysisStructural Analysis
Faults are significant tools in the trapping of
hydrocarbon. A growth fault tagged fault A and B
(Figure 2) are regional fault
mechanism. The trapping configurations of the faults
along with the embedding shale
responsible for the creation of multiple reservoir
compartments of hydrocarbon bearing formations
that is witnessed from one
this conforms with [12]
faults show that the amount of throw of both major
and minor faults are small and varied from line to line
in the seismic survey but increases in the northern
part of the field for all the horizons considered
data were tied to the seismic data after the mapped
horizons were digitized and this was done with the aid
of synthetic seismogram. The reflections that match
the depth to top of the hydrocarbon zones on the wel
logs were noted. The top of hydrocarbon bearing sand
tied with horizon picking started on this reflection
(Figure 3).
Figure 2: Seismic section showing the picked horizons and the fault types
TTRIBUTES TTRIBUTES TTRIBUTES TTRIBUTES O. OlogeO. OlogeO. OlogeO. Ologe, et al, et al, et al, et al
Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014 403403403403
were generated for all the
and were superimposed on the
structural maps to confirm the presence of
Vertical and lateral variations in
amplitude were analyzed using the horizon slices.
RESULTS AND DISCUSSIONRESULTS AND DISCUSSIONRESULTS AND DISCUSSIONRESULTS AND DISCUSSION
Faults are significant tools in the trapping of
. A growth fault tagged fault A and B
regional faults with high trapping
. The trapping configurations of the faults
along with the embedding shale were presumed to be
responsible for the creation of multiple reservoir
compartments of hydrocarbon bearing formations
one horizon to the other and
(Figure 2). The vertical
faults show that the amount of throw of both major
and minor faults are small and varied from line to line
in the seismic survey but increases in the northern
field for all the horizons considered. Well
data were tied to the seismic data after the mapped
digitized and this was done with the aid
of synthetic seismogram. The reflections that match
the depth to top of the hydrocarbon zones on the well
logs were noted. The top of hydrocarbon bearing sand
tied with horizon picking started on this reflection
Figure 2: Seismic section showing the picked horizons and the fault types
HHHHYDROCARBON YDROCARBON YDROCARBON YDROCARBON PPPPROSPECTING OVER ROSPECTING OVER ROSPECTING OVER ROSPECTING OVER ‘O‘O‘O‘OKKKK’’’’ FFFFIELDIELDIELDIELD,,,, NNNNIGER IGER IGER IGER DDDDELTA USING ELTA USING ELTA USING ELTA USING PPPPETROPHYSICAL AND ETROPHYSICAL AND ETROPHYSICAL AND ETROPHYSICAL AND SSSSEISMIC EISMIC EISMIC EISMIC AAAATTRIBUTES TTRIBUTES TTRIBUTES TTRIBUTES O. OlogeO. OlogeO. OlogeO. Ologe, et al, et al, et al, et al
Nigerian Journal of Technology, Nigerian Journal of Technology, Nigerian Journal of Technology, Nigerian Journal of Technology, Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014 404404404404
Figure 3: Well to seismic tie from well OK-010.
Figure 4: Well log Section showing the reservoirs delineated and correlated across OK-010 and OK-005 Wells.
4.2 4.2 4.2 4.2 Petrophysical AnalysisPetrophysical AnalysisPetrophysical AnalysisPetrophysical Analysis
The well log data provided information about the
geology of the surrounding formations. The
formations of interest in this study were the
hydrocarbon bearing formations, hence they were
carefully identified and analysed. Interpretation of the
lithology shows that the study area is composed of
sand-shale intercalations with the shale layers
increasing with depth (Figure 4). The lithology panels
showed the position of the two reservoirs mapped.
The reservoir R1 has a gross and a net thickness
between 15-27 m, net to gross of 1 and effective
porosity value was between 0.21-0.24 while water
saturation was 0.15. The summary of the results
obtained from well logs for reservoirs; R1 and R2 were
presented in Table 1 and 2 respectively.
Fault A
HHHHYDROCARBON YDROCARBON YDROCARBON YDROCARBON PPPPROSPECTING OVER ROSPECTING OVER ROSPECTING OVER ROSPECTING OVER ‘O‘O‘O‘OKKKK’’’’ FFFFIELDIELDIELDIELD,,,, NNNNIGER IGER IGER IGER DDDDELTA USING ELTA USING ELTA USING ELTA USING PPPPETROPHYSICAL AND ETROPHYSICAL AND ETROPHYSICAL AND ETROPHYSICAL AND SSSSEISMIC EISMIC EISMIC EISMIC AAAATTRIBUTES TTRIBUTES TTRIBUTES TTRIBUTES O. OlogeO. OlogeO. OlogeO. Ologe, et al, et al, et al, et al
Nigerian Journal of Technology, Nigerian Journal of Technology, Nigerian Journal of Technology, Nigerian Journal of Technology, Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014 405405405405
Table 1: Computed Petrophysical Parameters of Reservoirs R1
Well OK 10 OK 005
Top (m) 3107 3121
Net/Gross 1 1
Well OK 10 OK 005
Top (m) 3359 3390
Net/Gross 0.56 0.57
Fault interpretation was performed using the petrel
work flow tool. The continuity of the fault segments
and their assignment were checked on the seismic
sections. Faults were mapped on the seismic section
shown on dip attribute time slice extracted from the
seismic volume. (Figure 5 and 6). The vertical
displacement of the major and subsidiary growth
faults showed that the amount of throws of both major
and minor faults were small and varied from line to
line in the seismic survey but increases in the
northern part of the field for all the horizons
considered
Figure 5: Dip attribute extracted 10ms above E1.0 horizon showing the fault patterns.
Figure 6: Dip attribute extracted 10ms above E4.2 horizon showing the fault patterns.
HHHHYDROCARBON YDROCARBON YDROCARBON YDROCARBON PPPPROSPECTING OVER ROSPECTING OVER ROSPECTING OVER ROSPECTING OVER ‘O‘O‘O‘OKKKK’’’’ FFFFIELDIELDIELDIELD
Nigerian Journal of Technology, Nigerian Journal of Technology, Nigerian Journal of Technology, Nigerian Journal of Technology,
Figure 7 showed an amplitude distribution over
horizon E4.2 with depth overlay. The high amplitude
zones at the western part of the field correspond to
bright spots. The high amplitude zone
as the boundaries of the hydrocarbon reservoirs (fluid
contact) conform to the structure
conforms to the structure and therefore
were better defined and well established which
indicated accumulation of hydrocarbon
Figure 7: Horizon E 4.2 amplitude with depth overlay.
Figure 8: Horizon E 1.0 amplitude with depth overlay.
IELDIELDIELDIELD,,,, NNNNIGER IGER IGER IGER DDDDELTA USING ELTA USING ELTA USING ELTA USING PPPPETROPHYSICAL AND ETROPHYSICAL AND ETROPHYSICAL AND ETROPHYSICAL AND SSSSEISMIC EISMIC EISMIC EISMIC AAAATTRIBUTES TTRIBUTES TTRIBUTES TTRIBUTES
Nigerian Journal of Technology, Nigerian Journal of Technology, Nigerian Journal of Technology, Nigerian Journal of Technology, Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014
litude distribution over
can also double
structures. Amplitude
accumulation of hydrocarbon [13]. The
ude distribution over horizon E1.0
(Figure 8) showed high amplitude zones mostly at the
western part corresponding
reflection amplitude conforms
the field. The contacts we
established. Figure 9 presents the
distribution over horizon D7.5 with depth overlay.
The low amplitude zones cor
which showed little lateral coverage of the
hydrocarbon bearing reservoir
Figure 7: Horizon E 4.2 amplitude with depth overlay.
Figure 8: Horizon E 1.0 amplitude with depth overlay.
TTRIBUTES TTRIBUTES TTRIBUTES TTRIBUTES O. OlogeO. OlogeO. OlogeO. Ologe, et al, et al, et al, et al
Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014 406406406406
amplitude zones mostly at the
ing to bright spots. The
reflection amplitude conforms to structure, therefore
the assumed distribution of gas and oil within
were better defined and
The low amplitude zones correspond to dim spot
little lateral coverage of the
bearing reservoir.
Nigerian Journal of Technology, Nigerian Journal of Technology, Nigerian Journal of Technology, Nigerian Journal of Technology,
Figure 9: Horizon D 7.5 amplitude with depth overla
5. 5. 5. 5. CONCLUSION CONCLUSION CONCLUSION CONCLUSION
The subsurface geology and hydrocarbon potential of
“OK” field offshore Niger Delta have been studied
using 3D seismic, well logs and check
data. Two hydrocarbon-producing reser
estimates in the two reservoirs were v
ranging from 0.6 to 0.75 and 0.21 to 0.27 respectively.
Well to seismic tie showed that hydrocarbon bearing
reservoirs tied on the seismic section. Three horizons
were studied and two major faults A and B with minor
fault C, D and E were mapped for the purpose of
carrying out 3-D structural interpretation. This
interpretation was further enhanced with
attribute extracted from 3-D structural interpretation
This was combined with well log analysi
delineating suitable traps for the reservoirs.
maps such as amplitude were extracted to
complement the structural interpretation.
amplitude maps for the two horizons (E 1.0 and E 4.2)
were similar and zones of high anomalou
that were associated with structural highs matched
with the regions where wells have been drilled. There
was a good well synthetic match particularly with zero
IELDIELDIELDIELD,,,, NNNNIGER IGER IGER IGER DDDDELTA USING ELTA USING ELTA USING ELTA USING PPPPETROPHYSICAL AND ETROPHYSICAL AND ETROPHYSICAL AND ETROPHYSICAL AND SSSSEISMIC EISMIC EISMIC EISMIC AAAATTRIBUTES TTRIBUTES TTRIBUTES TTRIBUTES
Nigerian Journal of Technology, Nigerian Journal of Technology, Nigerian Journal of Technology, Nigerian Journal of Technology, Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014
Figure 9: Horizon D 7.5 amplitude with depth overlay.
hydrocarbon potential of
using 3D seismic, well logs and check-shot survey
producing reservoirs were
saturation and porosity
Well to seismic tie showed that hydrocarbon bearing
seismic section. Three horizons
D structural interpretation. This
D structural interpretation.
the reservoirs. Attributes
the structural interpretation. The
amplitude maps for the two horizons (E 1.0 and E 4.2)
were similar and zones of high anomalous amplitudes
re associated with structural highs matched
wells have been drilled. There
a good well synthetic match particularly with zero
phased data. Most synthetic seismograms also show
a reflection coinciding with th
most of the matched wells.
There was a strong relationship between the maps as
most structural highs coincided with zones of
anomalous amplitude. This study was able to show
enhancing imaging subsurface reservoirs
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TTRIBUTES TTRIBUTES TTRIBUTES TTRIBUTES O. OlogeO. OlogeO. OlogeO. Ologe, et al, et al, et al, et al
Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014 Vol. 33, No. 3, July 2014 407407407407
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HHHHYDROCARBON YDROCARBON YDROCARBON YDROCARBON PPPPROSPECTING OVER ROSPECTING OVER ROSPECTING OVER ROSPECTING OVER ‘O‘O‘O‘OKKKK’’’’ FFFFIELDIELDIELDIELD,,,, NNNNIGER IGER IGER IGER DDDDELTA USING ELTA USING ELTA USING ELTA USING PPPPETROPHYSICAL AND ETROPHYSICAL AND ETROPHYSICAL AND ETROPHYSICAL AND SSSSEISMIC EISMIC EISMIC EISMIC AAAATTRIBUTES TTRIBUTES TTRIBUTES TTRIBUTES O. OlogeO. OlogeO. OlogeO. Ologe, et al, et al, et al, et al
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