Blocks 31, 32, 33, 34, 35 & 36/03 Southeast Offshore Vietnam

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Arnold Snow
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Blocks 31, 32, 33, 34, 35 & 36/03 Southeast Offshore Vietnam Block 31 32 33 34 35

50 50 50 Seismic 2D (km) 1,294 685 431 477 380 593 Well 1 - - - - - HC Potential

Oligocene Miocene Interbeded Shales Tilted fault blocks Oil fields in adjacent Cuu

1 Blocks 31, 32, 33, 34, 35 & 36/03 Southeast Offshore Vietnam Block /03 Area (km 2) 5,036 4,440 4,630 4,700 4,630 2,950 Sea level (m) Seismic 2D (km) 1, Well HC Potential Oligocene Shales Oligocene Miocene Sandstones Oil and gas discoveries/shows Oligocene Miocene Interbeded Shales Tilted fault blocks Oil fields in adjacent Cuu Long. Block 31 - Vinh Chau Trough Stratigraphic distribution of source, reservoir and seal of Block 31

2 Block 37 - Phu Quoc Basin Block 37 Area : 5,020 sq. km Sea level: m Seismic : 775 km 2D HC Potential in Mesozoic The Phuquoc Kampot Som Basin is a Late Jurassic to Early Cretaceous foreland developed in response to the buildup of the paleo-pacific magmatic arc. It forms an elongated, more than 500 km long sediment-filled depression extending from south-western Cambodia in the north to the central southern part of the Gulf of Thailand This is upto 150 km wide belt with its axis along approximately latitudes The Cretaceous Phu Quoc Formation which contains coal layers (the socalled jet coal ) & Triassic black shales Sketch of trap types of Phu Quoc MZ Basin Jurassic-Cretaceous sandstones; Late Triassic sandstones; Permian limestones (Ratthuri group) Regional seal: Tertiary marine mudstones are regional seal Local seal: Interbedded shales and fault seal related structures; Stratigraphic traps: Carbonate build-ups and combined structural-stratigraphic traps., Thailand onshore.

3 Block 38 - Phu Quoc Basin Block 38: Area : 6,060 sq. km Sea level: m Seismic : 800 km 2D seismic HC Potential in Mesozoic The Phuquoc Kampot Som Basin is a Late Jurassic to Early Cretaceous foreland developed in response to the buildup of the paleo-pacific magmatic arc. It forms an elongated, more than 500 km long sediment-filled depression extending from south-western Cambodia in the north to the central southern part of the Gulf of Thailand This is upto 150 km wide belt with its axis along approximately latitudes The Cretaceous Phu Quoc Formation which contains coal layers (the socalled jet coal ) & Triassic black shales Jurassic-Cretaceous sandstones, Late Triassic sandstones, Permian limestones (Ratthuri group). Regional seal: Tertiary marine mudstones are regional seal Local seal: Interbedded shales and fault seal related structures Stratigraphic traps: Carbonate build-ups and combined structural-stratigraphic traps., Thailand onshore. Sketch of trap types in Phu Quoc MZ

build-up of the paleo-pacific magmatic arc.

4 Block 41 - Phu Quoc Basin Block 41: Area : 5,020 sq. km Sea level: 20 m Seismic : 1145 km 2D Prospects & Leads: 4 HC Potential in Mesozoic The Phuquoc Kampot Som Basin is a Late Jurassic to Early Cretaceous foreland developed in response to the build-up of the paleo-pacific magmatic arc. It forms an elongated, more than 500 km long sediment-filled depression extending from south-western Cambodia in the north to the central southern part of the Gulf of Thailand This is upto 150 km wide belt with its axis along approximately latitudes The Cretaceous Phu Quoc Formation which contains coal layers (the socalled jet coal ) ; Triassic black shales Jurassic-Cretaceous sandstones; Late Triassic sandstones; Permian limestones (Ratthuri group) Regional seal: Tertiary marine mudstones are regional seal Local seal: Interbedded shales and fault seal Structural traps: Inversion /compression related structures Stratigraphic traps: Carbonate buildups and combined structuralstratigraphic traps. Gas fields/discoveries in Khorat Mesozoic, Thailand onshore. Yallow Marker (Jurasic) B 2 B 1 B 3 Structural Elements in Phu Quoc MZ

5 Block 43 - Phu Quoc Basin Block 43: Area : 4,850 sq. km Sea level: 20 m Seismic : 2461 km 2D seismic Prospects & Leads: 5 HC Potential in Mesozoic The Phuquoc Kampot Som Basin is a Late Jurassic to Early Cretaceous foreland developed in response to the build-up of the paleo-pacific magmatic arc. It forms an elongated, more than 500 km long sediment-filled depression extending from south-western Cambodia in the north to the central southern part of the Gulf of Thailand This is upto 150 km wide belt with its axis along approximately latitudes The Cretaceous Phu Quoc Formation which contains coal layers (the socalled jet coal ) & Triassic black shales Jurassic-Cretaceous sandstones, Late Triassic sandstones, Permian limestones (Ratthuri group). Regional seal: Tertiary marine mudstones are regional seal Local seal: Interbedded shales and fault seal related structures Stratigraphic traps: Carbonate build-ups and combined structural-stratigraphic traps., Thailand onshore. Orange Marker (Permian) 43-E Structural Elements in Phu Quoc MZ

Block 44 - Phu Quoc Basin Block 44: Area : 4,760 sq.

Kampot Som Basin is a Late Jurassic to Early Cretaceous foreland developed in response to the build-up of

It forms an elongated, more than 500 km long sediment-filled depression extending from south-western

with its axis along approximately latitudes 103 0 104 0.

shales Jurassic-Cretaceous sandstones, Late Triassic sandstones, Permian limestones (Ratthuri group).

6 Block 44 - Phu Quoc Basin Block 44: Area : 4,760 sq. km Sea level: 20 m Seismic : 1,109 km 2D seismic Prospects & Leads: 2 Potential in Mesozoic The Phuquoc Kampot Som Basin is a Late Jurassic to Early Cretaceous foreland developed in response to the build-up of the paleo-pacific magmatic arc. It forms an elongated, more than 500 km long sediment-filled depression extending from south-western Cambodia in the north to the central southern part of the Gulf of Thailand This is upto 150 km wide belt with its axis along approximately latitudes The Cretaceous Phu Quoc Formation which contains coal layers (the socalled jet coal ) & Triassic black shales Jurassic-Cretaceous sandstones, Late Triassic sandstones, Permian limestones (Ratthuri group). Purple Marker (Carbon) Regional seal: Tertiary marine mudstones are regional seal Local seal: Interbedded shales and fault seal related structures Stratigraphic traps: Carbonate build-ups and combined structural-stratigraphic traps., Thailand onshore. Structure 44-A Structural Elements in Phu Quoc MZ

Block 47/01 - Phu Quoc Basin Block 47/01: Area : 5,850 sq.

developed in response to the build-up of the paleo-pacific magmatic arc.

This is upto 150 km wide belt with its axis along approximately latitudes 103 0 104 0.

7 Block 47/01 - Phu Quoc Basin Block 47/01: Area : 5,850 sq. km Sea level: m Seismic : 1,457 km 2D seismic Prospects & Leads: 5 MZ Potential in Mesozoic The Phuquoc Kampot Som Basin is a Late Jurassic to Early Cretaceous foreland developed in response to the build-up of the paleo-pacific magmatic arc. It forms an elongated, more than 500 km long sediment-filled depression extending from south-western Cambodia in the north to the central southern part of the Gulf of Thailand This is upto 150 km wide belt with its axis along approximately latitudes The Cretaceous Phu Quoc Formation which contains coal layers (the socalled jet coal ) & Triassic black shales Jurassic-Cretaceous sandstones, Late Triassic sandstones, Permian limestones (Ratthuri group). Regional seal: Tertiary marine mudstones are regional seal Local seal: Interbedded shales and fault seal related structures Stratigraphic traps: Carbonate build-ups and combined structural-stratigraphic traps., Thailand onshore. Purple Marker (Permian) C Structural Elements in Phu Quoc MZ

Block 48/05 - Malay-Tho Chu-Phu Quoc Basin Block 48/05: Area : 4,260 sq.

feature, 500 km long and 200 km wide, with a steep southwestern margin and more than 8,000 meters of Tertiary fill.

opening of the South China and Andaman seas. The SW VietNam offshore is located in NE flank of MaLay.

terrestrial organic material, oil prone generation.

8 Block 48/05 - Malay-Tho Chu-Phu Quoc Basin Block 48/05: Area : 4,260 sq. km Sea level: 50 m Seismic : 2,311 km 2D seismic HC Potential for and Mesozoic structural traps The Malay is a NW-SE trending asymmetric feature, 500 km long and 200 km wide, with a steep southwestern margin and more than 8,000 meters of Tertiary fill. The origin of this is related to major Paleogene plate tectonic movements which led to the collision of India with Eurasia and the resultant opening of the South China and Andaman seas. The SW VietNam offshore is located in NE flank of MaLay. Basin Proven petroleum containing oil and gas fields/discoveries in Oligocene lacustrine organic mater and mixture of lacustrine and terrestrial organic material, oil prone generation. Lower Miocene source rocks are mainly gas prone with minor oil potential; they contain mainly kerogen type III and a mixture of type I & III. Miocene deltaic clastic Local interbedded shales and regional Late Mio & Pliocene shales Purple Marker Structure 48/05 A Fault ed closure anticlines, stratigraphy traps Gas and condensate fiield s in adjacent Blocks B&52/97. Mesozoic

EGAS. Ministry of Petroleum

EGAS. Ministry of Petroleum EGAS Ministry of Petroleum EGAS Ministry of Petroleum About The Block Location: N. Thekah offshore block is located at about 56 km to the north of the Mediterranean shore line, 85 km to the north west