BP describes
their recent oil discovery in the Bumerangue Block Offshore Brazil, targeting
carbonates in the sub-salt Santos Basin, as its biggest find in 25 years.
According to BP’s press release, the well was drilled:
“…404 kilometres (218 nautical miles) from Rio de
Janeiro, in a water depth of 2,372 metres. The well was drilled to a total
depth of 5,855 metres.”
“The well intersected the reservoir about 500 metres
below the crest of the structure and penetrated an estimated 500 metre gross
hydrocarbon column in high-quality pre-salt carbonate reservoir with an areal
extent of greater than 300 square kilometres.”
“Results from the rig-site analysis indicate elevated
levels of carbon dioxide. bp will now begin laboratory analysis to further
characterize the reservoir and fluids discovered, which will provide additional
insight into the potential of the Bumerangue block. Further appraisal
activities are planned to be undertaken, subject to regulatory approval.”
This discovery also dovetails
nicely with the South American emergence as the leader in oil production growth in the Western Hemisphere,
which I wrote about last month.
The abundance of CO2 in the
pre-salt Santos Basin is well-established. Due to this, the CO2 is mitigated by
capturing it and re-injecting it. Brazil’s Petrobras reinjected 14.2 million
tons of CO2 in 2024 from 22 floating production, storage, and offloading (FPSO)
vessels. It is injected for enhanced oil recovery, which makes it useful as a
working fluid. Injection of produced CO2 into these pre-salt
reservoirs makes up more than a quarter (28%) of the global capacity reported
for 2024. Thus, the Santos Basin is a major CCS hub, or more specifically, a
CCUS-EOR hub.
A 2019 paper in Geosciences
explores the geotectonic controls on the accumulation of CO2 in Brazilian
pre-salt basins. Mantle intrusions associated with rifting are thought to be
the source of high-CO2 areas, with small faults possibly connecting the
magmatic body to the sedimentary section above it. The abstract below explains
the geological hypothesis, and the maps show locations, stratigraphy, and
structural features of the Santos Basin. I assume BP’s block is within or very
near to the Santos Outer High, as depicted.
Below, they explain different
geological ideas about the sources and distribution of CO2 in the reservoirs.
“The large concentrations CO2 in Santos
Basin were unexpected during the early exploratory process of its deep-water
areas. However, drilled pre-salt prospects have shown a wide range of CO2 contents
bringing together environmental and production complications. The mantellic
origin of these CO2 occurrences was established via noble gases
isotopic analyses [4]. Nevertheless, processes and mechanisms
responsible for the fate (introduction, migration, and preservation) of CO2 in
petroleum systems still remain unclear.”
“Many authors have suggested that the “CO2-risk”
in sedimentary basins could be related to the proximity of igneous intrusions
and deep-seated faults, or to geothermal gradient higher than 30° C/km [3,5]. Other geoscientists suggested empirically
that in some areas as, for example, in the Southeast Asia, CO2 accumulations
must be controlled by type and age of crustal basement, fault density,
temperature, and pressure of reservoirs [6].”
“More recently, strong evidence has been gathered
indicating that mantle helium and occurrences with higher percentages of CO2 were
related to areas of crustal thinning in depths of about 26–28 km, with thermal
flux higher than 61 mW/m2 [7].”
“Such conditions suggest rock melting due to the
asthenosphere rising towards the crust. However, the occurrence of just one or
more factors described above is not an unequivocal proxy for large
accumulations of CO2 in petroleum reservoirs. Such
uncertainties are the main reason to investigate more thoroughly processes and
mechanisms that generate, introduce, and accumulate CO2 in
petroleum systems. Independently of such myriad of details to be studied, a
tool with the power to recognize deep related magmatic processes would be an
excellent proxy to infer “CO2-risk” in petroleum reservoirs.”
“In this way, our work focused on crustal studies is
based mainly on potential method data associated with the geologic
interpretation of the Jupiter Prospect data, where the highest CO2 concentrations
are reported up to date. The obtained results allow us to propose an
association of the CO2 and intracrustal intrusions of
mantle-derived material.”
“Both gravity and magnetic data indicate the existence
of a highly stretched continental crust under the São Paulo Plateau and a
rather unique and conspicuous anomaly under the Jupiter Prospect. Modeling
indicates that this anomaly corresponds to an intracrustal intrusion that
reached almost to the top of the basement rocks in this area. We interpret this
intrusion as the main responsible agent to transport CO2 from
the mantle into the reservoir levels in the pre-salt section of this area.
Other occurrences of CO2 in Santos Basin are all located in the
stretched crust of the basin and are also interpreted as provenient from mantle
material ascending along major fault segments.”
References:
bp
announces hydrocarbon discovery at Bumerangue exploration well, offshore Brazil.
BP. August 4, 2025. bp
announces hydrocarbon discovery at Bumerangue exploration well, offshore Brazil
| News and insights | Home
BP
Announces Major Oil and Gas Discovery Off Brazil Coast. Pipeline Technology Journal.
August 5, 2025. BP
Announces Major Oil and Gas Discovery Off Brazil Coast | Pipeline Technology
Journal
22
FPSOs in Brazil’s pre-salt enable Petrobras to break CO2 reinjection record. Melisa
Cavcic. Offshore Energy. March 31, 2025. 22
FPSOs in Brazil’s pre-salt enable Petrobras to break C02 reinjection record -
Offshore Energy
Geotectonic
Controls on CO2 Formation and Distribution Processes in the Brazilian Pre-Salt
Basins. Luiz Gamboa, André Ferraz, Rui Baptista and Eugênio V. Santos Neto. Geosciences
2019, 9(6), 252. May 14, 2019. Geotectonic
Controls on CO2 Formation and Distribution Processes in the Brazilian Pre-Salt
Basins
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