The world’s largest oil fields are contained in limestones. By contrast, New Zealand’s oil deposits are mostly sandstone based. However, limestone associated with the Tikorangi Formation in the Taranaki Basin  is a hydrocarbon reservoir. 

Oil and gas reserves

There is no such thing as a ‘pool’ of oil or gas trapped underground that can be tapped into and pumped to the surface. Almost all oil and gas is found within the tiny spaces in deeply buried sedimentary rocks such as sandstones and coarse-grained limestones. These porous rocks can be likened to a hard sponge, full of tiny holes, but not compressible. The oil or gas is trapped inside the rock’s porosity.

When the well bore penetrates into the reservoir, the great pressure that the gases and fluids are under, due to deep burial, is released. This then pushes fluids into the well bore and lifts them to the surface.

Oil and limestone

The world’s largest oil and gas fields are mostly contained in porous limestones, formed millions of years ago in tropical marine environments. New Zealand limestones are mostly of the cool-water or temperate category, and because of deep burial in their conversion from sediment to rock, they have very low porosity. However, these hard rocks have been fractured by compression caused by tectonic plate movements and have developed a fracture porosity. These fractures can be infilled with gas, oil and/or water depending on the make-up of the deeper rock layers.

Taranaki Basin oil and gas

Taranaki Basin covers an area of about 330,000 km2 and is currently the only oil and gas-producing basin in New Zealand. Although the reservoir rocks are mostly sandstones, one of them is fractured Oligocene limestone similar to that found in the Waitomo region of the mid-west North Island. This block of limestone is located in the Tikorangi Formation, and the onshore Waihapa-Ngaere oil field taps into this hydrocarbon-bearing 170-metre thick limestone deposit.

This oil field was discovered in 1988 and is part of what is commonly known as the TAWN field complex. The TAWN fields currently produce an estimated 2400 barrels per day of oil and condensate and 21 million cubic feet per day of gas. (The oil industry most often uses non-SI units to express volumes of gases and liquids: 1 barrel ~ 159 L; 1 cubic foot ~ 28.3 L.)

Tikorangi limestone compared to Ōtorohanga limestone

The Tikorangi limestone lies 2 km below the surface just to the east of the Taranaki town of Stratford. It is muddier, finer and compositionally slightly different from the Ōtorohanga limestone, some of which is being extracted from the Ōparure Road quarry at Te Kūiti situated 150 km north-east of Stratford. However, it is of the same age, so it was forming at the same time as the quarry limestone.

Given that the Tikorangi limestone is hydrocarbon bearing indicates that its underlying source rocks have a different structure and composition from those associated with the Ōtorohanga limestone. The sediments that developed into these source rocks contained an accumulation of once-living plant and animal remains. Over many millions of years, exposure to high pressures, high temperatures and a changing chemical environment has converted these remains into hydrocarbons. These have then migrated upwards, filling in the tiny cracks and fissures present in the fractured limestone sitting above.

Researchers from the Earth and Ocean Sciences Department at the University of Waikato have worked alongside oil industry and New Zealand Government Ministries to unravel the geologic transformations that have led to the establishment of the Tikorangi Formation.

    Published 28 September 2012