TIDMTRP
RNS Number : 9200C
Tower Resources PLC
16 June 2023
16 June 2023
Tower Resources plc
("Tower" or the "Company")
Namibia Technical Update
Tower Resources plc (TRP.L, TRP LN), the AIM-listed oil and gas
company with a focus on Africa, is pleased to provide an update on
activity in respect of license PEL 96 in Namibia, covering offshore
blocks 1910A, 1911 and 1912B (the "Namibian Blocks") and, in
particular, the recent basin modelling work undertaken over the
license area.
Tower is the operator of license PEL 96 with an 80% working
interest.
Highlights
-- A basin and thermal maturity study has been undertaken within
PEL 96 which has significantly progressed the understanding of the
hydrocarbon prospectivity of the license. This basin modelling
study has been carefully integrated with seismic sequence
stratigraphic interpretation of the large 2D seismic datasets and
integrated with the well data within PEL96 and available well data
elsewhere in the Walvis Basin region.
-- The integrated analysis of the seismic, wells and the basin
modelling results shows clear evidence of a working petroleum
system present within the Dolphin Graben in PEL 96; in the form of
oil recovered from cores in the 1911/15-1 well and direct
hydrocarbon indicators (DHIs) observed on seismic.
-- The objectives of the basin modelling study were to assess
the critical elements of the hydrocarbon charging system, i.e.
thermal maturity, distribution of generative source kitchens,
volumetric estimation of generative capacity of mature source
rocks, timing of generation/expulsion of hydrocarbons and mapping
of migration pathways.
-- Main conclusions of basin modelling study:
o Generative source kitchens have been calculated and have been
mapped within PEL 96. Lower Cretaceous syn-rift sediments within
the main depocenters of the Dolphin Graben calculate as mature for
main oil and late oil generation.
o Timing of the main and late oil generation phases calculated
to be mid-Tertiary (Oligocene) to present-day.
o Migration pathways for oil charge have been mapped and the
main foci of migration identified. The volumes of hydrocarbons
generated have been calculated for each source kitchen.
o The main fetch areas that are able to focus migration towards
each of the main prospects are calculated as having potentially
generated oil within the following volumetric ranges; Alpha
Prospect fetch area - ca. 45 to 79 billion barrels ("bbls") oil,
Gamma Prospect fetch area - ca. 15 to 23 billion bbls oil.
o The potential for stratigraphic traps is recognised on the 2D
seismic data where Cretaceous reservoir targets onlap onto highs
along the western and eastern flanks of the Dolphin Graben. These
potential stratigraphic traps are located directly on several of
the main migration pathways out of the generative kitchens. These
potential stratigraphic traps show similarities to the recent major
discoveries in South Africa and Namibia.
-- The Company is currently undertaking an oil seep analysis to
accompany the basin modelling work, and a review of the existing
volumetric data on the prospects and leads that have already been
identified is underway.
Jeremy Asher, Tower's Chairman and CEO, commented:
"We are excited by the results of the basin modelling work and
its indication of the prospectivity of Tower's licenses in Namibia.
It explains neatly the results of the Norsk Hydro well, the source
of the lacustrine oil found within it, and the reasons why that oil
found its way into that well and subsequently migrated away from
it. The conclusions indicate the potential for either of the giant
billion-barrel-plus structures in the West of the license to be
charged; furthermore, the migration pathways, coupled with the
recent impressive industry successes in drilling stratigraphic
plays in the Orange Basin to the South, enhance our interest in the
similar stratigraphic leads that we interpret on the flanks of the
Alpha Prospect structure in particular. We look forward to updating
investors further as our work progresses."
Background
As part of its work programme, Tower has recently concluded a
geochemical and thermal maturity basin modelling study, the results
of which have positive implications for the prospectivity of the
license and which are now being incorporated into a play fairway
analysis covering the full PEL 96 license area.
The 1911/15-1 well drilled by Norsk Hydro in 1994 within the
Dolphin Graben encountered several potential source horizons in
both the Upper and Lower Cretaceous and has provided the most
valuable and well-documented calibration point for the basin
modelling. This well has been critical for identifying the most
regionally geologically consistent input parameters for the
computer models and has provided crucial geochemical data for
optimising the basin modelling inputs, and ensuring a very close
fit between the output predictions of the computer models and the
real-world measurements from the wells and seismic data. The
careful optimisation of the basin models to achieve a very close
calibration of outputs to the actual observed well data is
essential to having useful predictive model outcomes. PEL 96 (and
the northern Walvis Basin generally) is an expansive area and
therefore it has taken a substantial amount of new work to refine
the models.
There is clear evidence of a working petroleum system present in
PEL 96. The presence of an oil-mature early Cretaceous (and/or
potentially older) source rock is proven by:
a. The presence of a light (thermally mature) oil which was
recovered from core samples taken from an Albian-aged carbonate in
the exploration well 1911/15-1. The well drilled an intra-basinal
high within the central part of the Dolphin Graben. The basin
modelling outputs are consistent with the observed well data. This
implies that this oil represents hydrocarbons that have migrated
from a nearby mature source kitchen within the adjacent
half-grabens during Oligo-Miocene times. Additionally, the oil
samples recovered from 1911/15-1 have biomarkers indicative of a
lacustrine source (of likely syn-rift origin), which implies
Barremian and/or older early Cretaceous source rocks. This new
technical work conducted by Tower, especially the detailed
migration pathway analyses, suggests the presence of only residual
hydrocarbons was due to trap breaching, caused by later structural
movement and tilting, which spilled any accumulation to the
East.
b. The presence of compelling seismic evidence of widespread
direct hydrocarbon indicators. These are in the form of large gas
chimneys, where gas is observed to be migrating up and along
deep-seated faults from half graben depocenters, and also from the
presence of seismic anomalies indicating shallow gas accumulations
above and in the vicinity of the gas chimneys. These shallow gas
anomalies and gas chimneys are particularly prevalent along the
western margin of the Dolphin Graben and directly along mapped
major migration pathways, and are associated with major extensional
faults that extend into the deepest parts of the half graben
basins.
The purpose of the basin modelling analysis was to assess three
critical elements of the hydrocarbon charging system:
(i) to provide an evaluation of thermal maturity of the main
known source rocks and their areal extent (i.e. the areal
distribution of the generative kitchens);
(ii) to estimate the generative capacity of the mature source
rocks within the generative kitchens within PEL96 and volumes of
hydrocarbons generated; and,
(iii) to assess the timing of generation/expulsion of
hydrocarbons, phase of hydrocarbons expelled and map main migration
pathways for hydrocarbons, and to assess volumetrics of the
principal fetch areas for each exploration target.
Initial conclusions:
The main conclusions of the basin modelling study are:
1. The results of the basin modelling analysis, integrated with
seismic sequence stratigraphic interpretation of the extensive 2D
seismic data sets, indicate that oil-mature Lower Cretaceous source
prone intervals belonging to the early Cretaceous syn-rift phase of
the basin are widespread within PEL 96 and present over much of the
Dolphin Graben throughout PEL 96. Note that additional sub-basins
are present in the western part of PEL 96 that may extend the
presence of source-prone early Cretaceous, with the potential for
additional hydrocarbon generation in this area.
2. Lower Cretaceous source-prone intervals are calculated to sit
within the oil window over a large part of the Dolphin Graben
within PEL 96, reaching Main and Late Oil Maturity Windows over
much of the area.
3. Timing of the source-prone intervals entering the main and
late oil generation windows (the critical maturity zones which
account for the major component of oil generated that has the
capability to migrate) calculates to be mid-Tertiary (Oligocene) to
present-day.
4. Migration pathways have been analysed and mapped. The main
foci of migration out of the source kitchens have been identified
and the volumes of hydrocarbons generated in each fetch area have
been quantified. Note that the basin has undergone a significant
young structural tilting event (Mio-Pliocene age) which has
re-orientated several of the major migration pathways. Therefore,
it has been necessary to construct migration maps for both the
present-day and also back-strip the basin configuration to map the
main migration pathways at a time pre-dating the tilting and
coinciding with onset of main oil generation (mid-Oligocene).
5. Source kitchens have been calculated and have been mapped
within PEL 96. Several of these have configurations that would
focus any hydrocarbon migration towards several of the key
prospects and play fairways (note that each of these sub-divisions
of the generative kitchen which define migration of oil into any
individual prospect or play are termed 'fetch areas'). Generally,
the Dolphin Graben is more mature towards the north and therefore
the main volumes of migrations generated and migrated are in the
northern parts of the basin, i.e. within PEL 96 and especially
within the northern and central parts.
6. The fetch areas that focus migration towards each of the main
prospects are calculated as having generated oil within the
following volumetric ranges (note that some gas and gas condensates
are also calculated to have been generated in some deeper parts of
the basin and the volumetrics of these additional generated
hydrocarbons are still being assessed):
a. Alpha Prospect fetch area - is calculated to have generated
in the range 45 to 79 billion bbls oil,
b. Gamma Prospect fetch area - is calculated to have generated
in the range 15 to 23 billion bbls oil,
7. Phoenix High play fairway (with potential for stratigraphic
trapping up-dip to the east) - is calculated to have generated in
the range 45 to 59 billion bbls oil. Note that the ranges in
volumes of hydrocarbons generated per fetch area is in part a
reflection of the late tilting of the basin which causes a
reorganisation of the migration pathways from Oligocene to
present-day and which changes the areal extent of each fetch area
over time; this therefore changes the volume of hydrocarbons
capable of being focused towards each prospect with time.
8. The potential for stratigraphic traps with major regional
onlaps of the main Cretaceous reservoir targets are identified on
the seismic data to be located directly on several of the main
migration pathways out of the generative kitchens. This is
especially interesting for prospectivity since any oil migrating
towards the western mega-high prospects, for instance, the Alpha or
Gamma Highs, must first pass through these stratigraphic trapping
areas with potential for these stratigraphic traps to be
substantially oil charged.
Potential stratigraphic traps are recognised in western areas of
PEL 96 along the eastern flanks of the Alpha and Gamma highs in
both Lower and Upper Cretaceous reservoir-target sequences. These
potential stratigraphic traps have an up-dip towards the ocean
(west) architecture, similar to recent major discoveries by
TotalEnergies in South Africa.
Potential stratigraphic traps are also recognised in central
areas of PEL 96 along the western flanks of the Phoenix High, and
potentially the Elephant High slightly to the South. These
potential stratigraphic traps have an up-dip to the coast (east)
architecture similar to some of the major recent discoveries
further south in Namibia.
Next steps
The Company is currently undertaking an oil seep analysis to
accompany the basin modelling work, and a review of the existing
volumetric data on the leads that have already been identified.
This will result in a revised evaluation of the prioritisation, and
volumetrics associated with those leads, which the Company will
share with investors in due course.
In addition to highlighting the potential of the Tower Resources
Namibian Blocks, the results of the recent technical work will
provide a good foundation in ensuring the remaining initial
exploration phase of the PEL 96 work programme, including the
acquisition of new 3D seismic data as set out in the Company's work
programme, is sufficiently optimised and targeted to unlock the
full prospectivity of the license.
The Company is currently finalising a technical presentation on
the basin modelling, which will be posted to the Company's website
in due course. The Company will notify investors when this is
available.
Contacts:
Tower Resources plc +44 20 7157 9625
Jeremy Asher
Chairman and CEO
Andrew Matharu
VP - Corporate Affairs
SP Angel Corporate Finance
LLP
Nominated Adviser and Joint
Broker
Stuart Gledhill + 44 20 3470
Kasia Brzozowska 0470
Novum Securities Limited
Joint Broker
Jon Bellis + 44 20 7399
Colin Rowbury 9400
Axis Capital Markets Limited
Joint Broker +44 0203 026
Richard Hutchison 2689
Panmure Gordon (UK) Limited
Joint Broker
John Prior + 44 20 7886
Hugh Rich 2500
BlytheRay
Financial PR
Tim Blythe
Megan Ray +44 20 7138 3204
Notes:
Dr Mark Enfield, BSc, PhD, and a member of the Board of Tower
Resources plc, who has over 30 years' experience in the oil &
gas industry, is the qualified person that has reviewed and
approved the technical content of this announcement.
Market Abuse Regulation (MAR) Disclosure
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the Company to constitute inside information as stipulated under
the Market Abuse Regulations (EU) No. 596/2014 as it forms part of
UK domestic law by virtue of the European Union (Withdrawal) Act
2018 ('MAR'). Upon the publication of this announcement via
Regulatory Information Service ('RIS'), this inside information is
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