Itajaí-Açu Formation | |
---|---|
Stratigraphic range:
Cenomanian-
Maastrichtian ~ | |
Type | Geological formation |
Unit of | Frade Group |
Underlies | Marambaia Formation |
Overlies | Itanhaém Formation |
Thickness | up to 2,000 m (6,600 ft) |
Lithology | |
Primary | Shale |
Other | Sandstone |
Location | |
Coordinates | 26°6′S 43°43′W / 26.100°S 43.717°W |
Region | Santos Basin, South Atlantic |
Country | Brazil |
Type section | |
Named for | Itajaí-Açu River |
Location of the Santos Basin |
The Itajaí-Açu Formation ( Portuguese: Formacão Itajaí-Açu) is a geological formation of the Santos Basin offshore of the Brazilian states of Rio de Janeiro, São Paulo, Paraná and Santa Catarina. The predominantly shale with interbedded turbiditic sandstones formation dates to the Late Cretaceous period; Cenomanian- Maastrichtian epochs and has a maximum thickness of 2,000 metres (6,600 ft). The formation is a reservoir rock of the fields in the Santos Basin.
The formation is named after the Itajaí-Açu River, Santa Catarina.
The Itajaí-Açu Formation is 1,545 to 2,000 metres (5,069 to 6,562 ft) thick, [1] and comprises a thick interval of dark grey clayey rocks, interbedded with the clastics of the Santos and Juréia Formations. Within this formation, the Ilhabela Member includes the turbiditic sandstones occurring along the section. The sedimentary environment is thought to be marine talus to open basin. Biostratigraphic data from palynomorphs, calcareous nannofossils and planktonic foraminifera indicate a Late Cretaceous age ( Cenomanian- Maastrichtian). [2]
The formation, mainly its Ilhabela Member, is the main post-salt reservoir rock of the Santos Basin. [3] [4] The formation also is the main post-salt source rock and a seal for the post-salt reservoirs. [5]
Field | Year | Operator | Reserves (in place) | Notes |
---|---|---|---|---|
Panoramix | 2009 | Repsol | 176 million bbl (28.0 million m3) | |
Piracucá | 2009 | Petrobras | 321.4 million bbl (51.1 million m3) | |
Cedro | 2005 | Petrobras | 95.76 million bbl (15.2 million m3) | |
Lagosta | 2003 | El Paso Corp. | 0.173 trillion cu ft (4.9 billion m3) | |
Uruguá | 2003 | Petrobras | 174.27 million bbl (27.7 million m3) 1 trillion cu ft (28 billion m3) |
|
Carapiá | 2002 | Petrobras | 63.52 million bbl (10.1 million m3) | |
Mexilhão | 2001 | Petrobras | 532.23 million bbl (84.6 million m3) 3.4 trillion cu ft (96 billion m3) |
|
Tambuatá | 1999 | Petrobras | 212.8 million bbl (33.8 million m3) |
{{
citation}}
: CS1 maint: DOI inactive as of July 2024 (
link)Itajaí-Açu Formation | |
---|---|
Stratigraphic range:
Cenomanian-
Maastrichtian ~ | |
Type | Geological formation |
Unit of | Frade Group |
Underlies | Marambaia Formation |
Overlies | Itanhaém Formation |
Thickness | up to 2,000 m (6,600 ft) |
Lithology | |
Primary | Shale |
Other | Sandstone |
Location | |
Coordinates | 26°6′S 43°43′W / 26.100°S 43.717°W |
Region | Santos Basin, South Atlantic |
Country | Brazil |
Type section | |
Named for | Itajaí-Açu River |
Location of the Santos Basin |
The Itajaí-Açu Formation ( Portuguese: Formacão Itajaí-Açu) is a geological formation of the Santos Basin offshore of the Brazilian states of Rio de Janeiro, São Paulo, Paraná and Santa Catarina. The predominantly shale with interbedded turbiditic sandstones formation dates to the Late Cretaceous period; Cenomanian- Maastrichtian epochs and has a maximum thickness of 2,000 metres (6,600 ft). The formation is a reservoir rock of the fields in the Santos Basin.
The formation is named after the Itajaí-Açu River, Santa Catarina.
The Itajaí-Açu Formation is 1,545 to 2,000 metres (5,069 to 6,562 ft) thick, [1] and comprises a thick interval of dark grey clayey rocks, interbedded with the clastics of the Santos and Juréia Formations. Within this formation, the Ilhabela Member includes the turbiditic sandstones occurring along the section. The sedimentary environment is thought to be marine talus to open basin. Biostratigraphic data from palynomorphs, calcareous nannofossils and planktonic foraminifera indicate a Late Cretaceous age ( Cenomanian- Maastrichtian). [2]
The formation, mainly its Ilhabela Member, is the main post-salt reservoir rock of the Santos Basin. [3] [4] The formation also is the main post-salt source rock and a seal for the post-salt reservoirs. [5]
Field | Year | Operator | Reserves (in place) | Notes |
---|---|---|---|---|
Panoramix | 2009 | Repsol | 176 million bbl (28.0 million m3) | |
Piracucá | 2009 | Petrobras | 321.4 million bbl (51.1 million m3) | |
Cedro | 2005 | Petrobras | 95.76 million bbl (15.2 million m3) | |
Lagosta | 2003 | El Paso Corp. | 0.173 trillion cu ft (4.9 billion m3) | |
Uruguá | 2003 | Petrobras | 174.27 million bbl (27.7 million m3) 1 trillion cu ft (28 billion m3) |
|
Carapiá | 2002 | Petrobras | 63.52 million bbl (10.1 million m3) | |
Mexilhão | 2001 | Petrobras | 532.23 million bbl (84.6 million m3) 3.4 trillion cu ft (96 billion m3) |
|
Tambuatá | 1999 | Petrobras | 212.8 million bbl (33.8 million m3) |
{{
citation}}
: CS1 maint: DOI inactive as of July 2024 (
link)