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Jadestone Energy (Australia) Pty Ltd
The Atrium Building
Level 2, 168 St Georges Terrace
Perth, Western Australia, 6000

+61 8 9486 6600

Jadestone Energy (S) Pte Ltd
Talavera Suite 10th Floor, Unit 05-06
Talavera Office Park, Jl. TB Simatupang
Kav.22-26, Jakarta 12430 Indonesia

+62 21 8066 9020

Jadestone Energy (Singapore) Pte Ltd
3 Anson Road
#13-01 Springleaf Tower
Singapore 079909

+65 6324 0359

Mitra Energy (Vietnam Phu Khanh) Pte Ltd
Unit 07-22 The Executive Centre, Level 7
Friendship Tower, 31 Le Duan Boulevard
Ben Nghe Ward, District 1
Ho Chi Minh City, Vietnam

+84 28 38 237 111

Jadestone Energy plc
Human Resources team

careers@jadestone-energy.com

Phil Corbett
Investor Relations Manager

+44 7713 687467
ir@jadestone-energy.com

James Crothers, Billy Clegg
CAMARCO (Financial PR)

+44 (0)203 7574980
jse@camarco.co.uk

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Vietnam

Block 46/07 PSC (Nam Du)

Jadestone Energy has a 100% operated working interest in the Block 46/07 PSC.

The Nam Du discovery is located within the Block 46-07 PSC on the north-eastern margin of the Malay-Tho Chu Basin, approximately 200 kilometres offshore Vietnam in a water depth of 48 metres.

The Nam Du Channel 22 reservoir is a fluvial channel of Lower Miocene age. It is approximately 20 metres thick and has two thin coal intervals. Wireline logs show a coarsening-upwards sequence with the upper 10-15 metres appearing to be cleaner and a higher porosity interval.

Block 51 PSC (U Minh and Tho Chu)

Jadestone Energy has a 100% operated working interest in the Block 51 PSC.

The U Minh and Tho Chu discoveries are located within the boundaries of the Block 51 PSC in the Malay-Tho Chu Basin, approximately 200 kilometres offshore Vietnam in a water depth of 64 metres.

The U Minh H100 reservoir is a moderately sinuous channel-point bar system of Miocene age, trending downdip from northeast to southwest where it is folded over the U Minh four-way dip closure structure. The channel-point bar complex is at least 12 kilometres long and 1.3 kilometres wide. There are also several other reservoir horizons to be tested in the future, with potential over-lapping channel systems.

The Tho Chu reservoirs were deposited in the Lower to Middle Miocene ages. The depositional environment ranges from fluvial to marginal marine. Reservoir sands are typically 1-5 metres and are separated by flooding surfaces that are thought to act as seals. An abundance of coals deposited throughout the Lower to Middle Miocene interval allow for a robust stratigraphic correlation.

At present, no development plan has been submitted for the Tho Chu gas discovery and contingent resources are consequently classified as development unclarified. 

Nam Du/U Minh development plan

Jadestone plans to jointly develop the Nam Du and U Minh gas fields, which contain independently estimated gross 2P reserves of c.187 Bscf of gas and c. 1 MMboe of condensate (c.32 MMboe in aggregate). The field development plan (FDP) for the Nam Du and U Minh fields was approved in March 2026. The FDP includes two unmanned wellhead platforms (WHP), one located at each field, with production delivered to a central floating production, storage, and offloading (FPSO) vessel located close to the Nam Du WHP.

Processed gas from Nam Du and U Minh will be exported via a 34km tie-in to the existing 18 inch pipeline owned by Petrovietnam that transports gas from the PM-03-CAA Block to the Ca Mau power and industrial complex in southern Vietnam. Condensate would be exported by shuttle tanker. Vietnam gas imports from the PM-03-CAA Block to the south of Nam Du and U Minh are currently in decline, and with no additional gas resource available, will result in sufficient pipeline ullage that Jadestone intends to utilise.

Development of the Nam Du/U Minh resource would lessen Vietnam’s future dependence on expensive LNG imports and would contribute towards the country’s energy transition and stated goal of Net Zero greenhouse gas emissions by 2050.

Vietnam GSPA signing ceremony video