2000m), including the Barra, Cumbe, Farfan, Moita, Bonita and Muriu fields. The key petroleum system involves source rocks in the Riachuelo and Cotinguiba formations from the Albian-Cenomanian ages, with reservoirs in turbidite sandstones of the Upper Cretaceous Calumbi Formation. Eleven exploration blocks totaling ~7,689 km2">2000m), including the Barra, Cumbe, Farfan, Moita, Bonita and Muriu fields. The key petroleum system involves source rocks in the Riachuelo and Cotinguiba formations from the Albian-Cenomanian ages, with reservoirs in turbidite sandstones of the Upper Cretaceous Calumbi Formation. Eleven exploration blocks totaling ~7,689 km2">
Nothing Special   »   [go: up one dir, main page]

02 Sergipe-Alagoas R14 English

Download as pdf or txt
Download as pdf or txt
You are on page 1of 65

Sergipe-Alagoas Basin

Offshore
Bolívar Haeser

Superintendency of Delimitation of Blocks


Outline

Location
Infrastructure and Operational Conditions
Exploration Overview
Tectonostratigraphic Evolution
Petroleum Systems
Plays
Area on Offer
Final Remarks
Outline

Location
Infrastructure and Operational Conditions
Exploration Overview
Tectonostratigraphic Evolution
Petroleum Systes
Plays
Area on Offer
Final Remarks
Location
Passive Margin Basin

Total Area: 73,000 km²


≃ 60,500 km² offshore
(4,000 m water table)

Traditional onshore and


shallow water producing
basin (mature)
Limits
Northern Limit:
Maragogi High

Southern Limit: Estancia


Platform and Vaza-Barris
Fault

Limit between sub-basins:


Japoata-Penedo High
(onshore and shallow water)
Area on Offer
11 Exploration Blocks
3 Sectors

Aracaju Total Area ~7,689 km²

Ultra-deepwater
water table > 2,000 m

Well with ongoing appraisal plan

Well with hydrocarbons


Infrastructure and
Operational Conditions

RNEST Ports and airports


in Aracaju and
Maceio

Refinery
Gas plant
Oil pipeline
Gas pipeline
Field
Block on Offer R14
R14 Sector
Outline

Location
Infrastructure and Operational Conditions
Exploration Overview
Tectonostratigraphic Evolution
Petroleum Systems
Plays
Area on Offer
Final Remarks
Exploration
Overview

1930s
CNP

1935 – Geophysical surveys


1939 – First well in the basin
Exploration
Overview

1957 – First discovery; first


1930s offshore seismic
CNP 1963 – Carmopolis Field
1968 – Guaricema Field

25
Offshore exploratory wells
20

15
Wells

10

5 GUARICEMA

0
Exploration
Overview

1957 – First discovery; first 1987 – First deepwater well


1930s offshore seismic 2001 – Piranema field
CNP 1963 – Carmopolis Field 2012 – Ultra-deepwater
1968 – Guaricema Field discoveries

25
Offshore exploratory wells
20
BARRA, CUMBE,
15 FARFAN, MOITA
Wells

BONITA and MURIU

10 PIRANEMA

5 GUARICEMA

0
Fields

Production
~ 49,000 boe/d

Dourado
Guaricema Guaricema, Dourado
and Piranema produce
Piranema in Calumbi Fm
Avalable Data

2D Seismic
Available Data

3D Seismic
Available Data

285 offshore
exploratory
wells
Outline

Location
Infrastructure and Operational Conditions
Exploration Overview
Tectonostratigraphic Evolution
Petroleum Systems
Plays
Area on Offer
Final Remarks
Tectonostratigraphic
Evolution

130
152
12279
108 Million
Million
Million
49Million
million
164 Million
years
years
years
yearsago
ago
years ago
agoago
years ago
Current Configuration
of Continents

SINBPA/Petrobras
Scotese
Tectonostratigraphic
Evolution

Regressive Drift
Santonian - Present

Transgressive Drift
Late Aptian - Coniacian
Source: ANP/UFRN/FUNPEC, 2008

Rift and Transitional (Berriasian – Early Albian)

Pre-Rift (Jurassic)

Paleozoic Syneclise (Early Permian - Carboniferous)


Basement (Proterozoic)
Tectonostratigraphic
Evolution

Riachuelo Fm (Albian - Cenomanian)


Shelf carbonates and siliclastic rocks

Fm Cotinguiba (Cenomanian - Coniacian)


Carbonatic Ramp; calcilutites, shales and marls

Transgressive Drift
Late Aptian - Coniacian
Source: ANP/UFRN/FUNPEC, 2008
Tectonostratigraphic
Evolution

Regressive Drift
Santonian - Present

Marituba Fm and Mosqueiro Fm


Shelf carbonates and sandstones
Source: ANP/UFRN/FUNPEC, 2008

Calumbi Fm
Shales and turbidite sandstones
Schematic Section

NW SE

Basement Rift and Trasitional Seq. Regressive Drift Seq. (Paleogene-Present)


Volcanic Rock Transgressive Drift Seq. Sea
SDR Regressive Drift Seq. (Cretaceous) Faults
Outline

Location
Infrastructure and Operational Conditions
Exploration Overview
Tectonostratigraphic Evolution
Petroleum Systems
Plays
Area on Offer
Final Remarks
Petroleum
Systems

Many known petroleum systems;

Most of them active only onshore and in shallow water;

For the ultra deepwater Sergipe-Alagoas basin the


following petroleum systems are to be expected:

Riachuelo-Calumbi (!)
(Piranema Field)

Cotinguiba-Calumbi (.)

Stratigraphic Chart Source: ANP/UFRN/FUNPEC, 2008


Source Rocks

Ultra-deepwater:

Albian-Cenomanian shales of the


Riachuelo Formation

(source rock in the Piranema Field; 42º API oil)

Cenomanian-Turonian shales of the


Cotinguiba Formation

TOC up to 12%

Stratigraphic Chart Source: ANP/UFRN/FUNPEC, 2008


Reservoir Rocks

Upper Cretaceous turbidite


sandstones of the Calumbi
Formation

Φ = 15-23%

Secondarily Paleocene turbidite


sandstones of the Calumbi Formation

Stratigraphic Chart Source: ANP/UFRN/FUNPEC, 2008


Seals

Calumbi Formation shales

Stratigraphic Chart Source: ANP/UFRN/FUNPEC, 2008


Traps

Stratigraphic or combined (pinch-outs and channels)


Play

Play
Upper Cretaceous turbidite sandstones of the
Calumbi Fm

Secondary Play
Paleocene turbidite sandstones of the Calumbi Fm
Outline

Location
Infrastructure and Operational Conditions
Exploration Overview
Tectonostratigraphic Evolution
Petroleum Systems
Plays
Area on Offer
Final Remarks
Area on Offer
9 ultra-deepwater wildcat
wells
5 discoveries under
appraisal

Last decade:
29 deepwater exploration
wells
21 wells with
hydrocarbons

Well with ongoing appraisal plan

Well with hydrocarbons


Leads

NW Moita Bonita Discovery Arbitrary Section –0264_BM_SEAL_4_10_11 Survey SE


Courtesy of PGS
Depth (m)

Paleocene Turonian Lead


Maastrichtian Volcanin Rock
Leads

NW Moita Bonita Discovery Arbitrary Section –0264_BM_SEAL_4_10_11 Survey SE


Courtesy of PGS
Depth (m)

Paleocene Turonian Lead


Maastrichtian Volcanin Rock
Leads
R0257_SEALP1_PSDM Survey
NW Moita Bonita Discovery Courtesy of Spectrum SE
Depth (m)

Paleocene Turonian Lead


Maastrichtian Volcanin Rock
Leads
R0257_SEALP1_PSDM Survey
NW Moita Bonita Discovery Courtesy of Spectrum SE
Depth (m)

Paleocene Turonian Lead


Maastrichtian Volcanin Rock
Leads
NW SE

501
Arbitrary Section –0264_BM_SEAL_4_10_11 Survey
Courtesy of PGS
Depth (m)

Paleocene Turonian Lead


Maastrichtian Volcanin Rock
Leads
NW SE

501
Arbitrary Section –0264_BM_SEAL_4_10_11 Survey
Courtesy of PGS
Depth (m)

Paleocene Turonian Lead


Maastrichtian Volcanin Rock
Leads
SW NE

501
Depth (m)

Crossline 3145–0264_BM_SEAL_4_10_11 Survey


Courtesy of PGS

Paleocene Turonian Lead


Maastrichtian Volcanin Rock
Leads
SW NE

501
Depth (m)

Crossline 3145–0264_BM_SEAL_4_10_11 Survey


Courtesy of PGS

Paleocene Turonian Lead


Maastrichtian Volcanin Rock
Leads
NW SE

501
Inline 2750–0264_BM_SEAL_4_10_11 Survey
Courtesy of PGS
Depth (m)

Paleocene Turonian Lead


Maastrichtian Volcanin Rock
Leads
NW SE

501
Inline 2750–0264_BM_SEAL_4_10_11 Survey
Courtesy of PGS
Depth (m)

Paleocene Turonian Lead


Maastrichtian Volcanin Rock
Leads
NW SE

501
Inline 2480–0264_BM_SEAL_4_10_11 Survey
Courtesy of PGS
Depth (m)

Paleocene Turonian Lead


Maastrichtian Volcanin Rock
Leads
NW SE

501
Inline 2480–0264_BM_SEAL_4_10_11 Survey
Courtesy of PGS
Depth (m)

Paleocene Turonian Lead


Maastrichtian Volcanin Rock
Leads
NW SE

Blocks 633 and 635


R0257_SEALP1_PSDM Survey
Courtesy of Spectrum
Depth (m)

Paleocene Turonian Lead


Maastrichtian Basement
Leads
NW SE

Blocks 633 and 635


R0257_SEALP1_PSDM Survey
Courtesy of Spectrum
Depth (m)

Paleocene Turonian Lead


Maastrichtian Basement
Leads
NW SE

568 Blocks 568 and 633 633 635


R0257_SEALP1_PSDM Survey
Courtesy of Spectrum
Depth (m)

Paleocene Turonian Lead


Maastrichtian Basement
Leads
NW SE

568 Blocks 568 and 633 633 635


R0257_SEALP1_PSDM Survey
Courtesy of Spectrum
Depth (m)

Paleocene Turonian Lead


Maastrichtian Basement
Leads
NW SE

571
R0257_SEALP1_PSDM Survey
Courtesy of Spectrum
Depth (m)

Paleocene Turonian Lead


Maastrichtian Volcanin Rock
Leads
NW SE

571
R0257_SEALP1_PSDM Survey
Courtesy of Spectrum
Depth (m)

Paleocene Turonian Lead


Maastrichtian Volcanin Rock
Leads
SW NE

Blocks 633, 635 and 571


R0257_SEALP1_PSDM Survey
Courtesy of Spectrum
Depth (m)

Paleocene Turonian Lead


Maastrichtian Basement
Leads
SW NE

Blocks 633, 635 and 571


R0257_SEALP1_PSDM Survey
Courtesy of Spectrum
Depth (m)

Paleocene Turonian Lead


Maastrichtian Basement
Leads
SW NE

Blocks 635 and 571


R0257_SEALP1_PSDM Survey
Courtesy of Spectrum
Depth (m)

Paleocene Turonian Lead


Maastrichtian Basement
Leads
SW NE

Blocks 635 and 571


R0257_SEALP1_PSDM Survey
Courtesy of Spectrum
Depth (m)

Paleocene Turonian Lead


Maastrichtian Basement
Leads
NW SE

353
R0257_SEALP1_PSDM Survey
Courtesy of Spectrum
Depth (m)

Paleocene Turonian Lead


Maastrichtian Basement
Leads
NW SE

353
R0257_SEALP1_PSDM Survey
Courtesy of Spectrum
Depth (m)

Paleocene Turonian Lead


Maastrichtian Basement
Leads
NW SE

Blocks 279 and 281


R0257_SEAL_PHASE1_PSDM Survey
Courtesy of Spectrum
Depth (m)

Paleocene Turonian Lead


Maastrichtian Top of Rift
Leads
NW SE

Blocks 279 and 281


R0257_SEAL_PHASE1_PSDM Survey
Courtesy of Spectrum
Depth (m)

Paleocene Turonian Lead


Maastrichtian Top of Rift
Leads
NW SE

Blocks 212 and 281


R0257_SEALP1_PSDM Survey
Courtesy of Spectrum
Depth (m)

Paleocene Turonian Lead


Maastrichtian Top of Rift
Leads
NW SE

Blocks 212 and 281


R0257_SEALP1_PSDM Survey
Courtesy of Spectrum
Depth (m)

Paleocene Turonian Lead


Maastrichtian Top of Rift
Leads
NW SE

214
R0257_SEALP1_PSDM Survey
Courtesy of Spectrum
Depth (m)

Paleocene Turonian Lead


Maastrichtian Top of Rift
Leads
NW SE

214
R0257_SEALP1_PSDM Survey
Courtesy of Spectrum
Depth (m)

Paleocene Turonian Lead


Maastrichtian Top of Rift
Leads

Unrisked
in place
Volume
~15 billion
bbl

Lead

Block on Offer R14


Outline

Location
Infrastructure and Operational Conditions
Exploration Overview
Tectonostratigraphic Evolution
Petroleum Systems
Plays
Area on Offer
Final Remarks
Final Remarks

 Sergipe-Alagoas, a traditional onshore and shallow water


producing basin, is one of the most promising ultra-deepwater
frontiers in Brazil;

 Over the last years, large discoveries of light oil, gas and
condensate were reported in the ultra-deepwater Sergipe-
Alagoas basin;

 These discoveries prove the existence of an active and efficient


petroleum system (Albian-Turonian marine source rock with
accumulations in Upper Cretaceous turbidite reservoirs);
Final Remarks

 The area on offer is in the same geological context of these


discoveries;

 Several leads analogous to the Barra, Farfan, Muriú, Moita


Bonita and Poço Verde discoveries were identified;

 The identified leads exhibit seismic facies favourable to the


presence of turbidite lobes and channels;

 Unrisked in-place volumes were evaluated at 15 billion barrels


of oil.
National Agency of Petroleum, Natural Gas
and Biofuels

Bolívar da Silva Haeser


seminariostecnicos_sdb@anp.gov.br

www.anp.gov.br

You might also like