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South Pars/North Dome Gas-Condensate field

Natural gas field in the Persian Gulf

  • 20 min read
  • 5 chapters

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Through Natural gas, Europe and Iraq

As of early 2026, before the beginning of the 2026 Iran war, Qatar was producing approximately 18.5 billion cubic feet (520 million cubic metres) per day from the field, accounting for around 80% of Qatari government revenues, while daily production on the Iranian side was estimated to be around only 2 billion cubic feet (57 million cubic metres). Iran's inefficient exploitation of the shared gas field is often attributed to Western sanctions, isolation and mismanagement. These have also caused the Iranian government to lag behind on pressurization efforts on their side of the field, which causes more gas to migrate to the Qatari side of the field.

On 18 March 2026, the field was attacked by the Israeli Air Force. United States officials denied coordination and approval of the Israeli attack. Initial reports revealed that the damage caused to sections of South Pars gas field make up nearly 12 percent of Iran's total gas production. Iran's Ministry of Petroleum said that a number of facilities were damaged and that a fire at the gas field was being put under control. No casualties were immediately reported. The attack halted output at two refineries with a combined capacity of 100 million cubic metres per day. Parts of the gas field were closed to stop the fire from spreading. Following news of the attack, international oil prices increased from $103 a barrel to $108. Gas prices in Europe increased by 7 percent amid fears of Iranian retaliatory action against energy infrastructure in the Gulf Arab states. Iran halted its gas flows to Iraq, which relies on Iran for between a third and 40 percent of its gas and power needs.

Field geology

The field is 3,000 metres (9,800 ft) below the seabed at a water depth of 65 metres (213 ft), and consists of two independent gas-bearing formations: Kangan (Triassic) and Upper Dalan (Permian). Each formation is divided into two different reservoir layers, separated by impermeable barriers. The field consists of four independent reservoir layers K1, K2, K3, and K4.

The K1 and K3 units are mainly composed of dolomites and anhydrites, while K2 and K4, which constitute major gas reservoirs, comprise limestone and dolomite. A massive anhydrite (the Nar member) separates the K4 from the underlying K5 unit which has poor reservoir qualities. The gross pay zone in the South Pars field is approximately 450 m thick, extending from depths of approximately 2750 to 3200 m. Reservoir strata dip gently to the NE. The average thickness of the reservoir units declines from South Pars (some 450 metres (1,480 ft)) to North field (385 metres (1,263 ft)). As in other reservoir structures in neighboring areas, the reservoir in the Qatar Arch is cut by a set of NNW-SSE trending faults. Diagenesis has a major effect on reservoir quality of the field.

The field is a part of the N-trending Qatar Arch structural feature that is bounded by the Zagros fold and thrust belt to the north and northeast.

In the field, gas accumulation is mostly limited to the Permian–Triassic stratigraphic units. These units known as the Kangan–Dalan Formations constitute very extensive natural gas reservoirs in the field and Persian Gulf area, which composed of carbonate–evaporite series also known as the Khuff Formation.

Permian–Early Triassic has been divided into Faraghan (Early Permian), Dalan (Late Permian) and Kangan (Early Triassic) Formations.

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