The Southern Amadeus Basin is a large and underexplored region characterised by northwest trending structures in the northern area, and a central area dominated by an east-west central structural ridge. The southern area has a variety of structural styles including basement involved structural highs, compressional folds and salt-cored thrusted anticlines. The proven Larapintine petroleum system in the Northern Amadeus is not present southwards, however, source rocks are also recorded deeper in the stratigraphic succession including in the Cambrian Tempe Formation and Chandler Salt. The Neoproterozoic Pertatataka, Aralka, Finke Beds and Bitter Springs formations also show oil and gas source characteristics, in particular in the basal Gillen Member which provides the source for the Heavitree/basement play.
Gas was discovered at Magee‑1 in 1992 where a test at a depth of 2,340 m flowed gas at a stabilised rate of 63 Mscfd, comprising natural gas, helium and nitrogen from a 6m zone of Heavitree Formation. Seismic data indicates a possible up dip location (Mahler) which requires additional seismic acquisition to confirm closure. Other Heavitree/fractured basement leads within the block (Jackalope and Wolpertinger) are based on potential field data and are targets for natural gas and helium, however, additional seismic acquisition will be needed to delineate the leads.
This permit is immediately east of and geologically similar to EP 82. Several leads have been identified from potential field data, the extensive 2013 regional seismic program, and field (outcrop) mapping. Regional seismic was acquired in 2013/14 and interpretation has identified the Mahler lead in adjacent EP 82 may extend into this permit. Other Heavitree/fractured basement leads within the block (Wolpertinger, Kraken, Thunderbird) are based on potential field data and are targets for natural gas and helium, however, additional seismic/fieldwork will be needed to delineate the leads.
This permit contains a variety of structural styles, and several leads have been identified from potential field data and the extensive 2013 regional seismic program. Seismic acquired in 2013/14 and 2016/2018 identified the giant Dukas prospect at basement level. The Dukas-1 well was spudded 16 April 2019 targeting natural gas and helium from the Heavitree Formation, which flowed at sub-commercial rates from Magee 1. Drilling was suspended due to extremely high pressures before penetration of the Heavitree Formation or basement. Drilling mud samples indicate the presence of hydrocarbons and helium and further analysis will be completed on well logs and gas samples. Central and Santos are planning a return to the well in 2022.This permit contains a variety of structural styles, and additional Heavitree Formation/fractured basement leads (Sculthorpe, Beethoven, Grainger, Percy, Mozart) have been identified from potential field data as well as the 2013/14 and 2016/2018 seismic programs.
In 2014, the joint venture operated by Santos drilled the exploration well Mt Kitty 1 to test a large basement structure with closure up to approximately 200 km². The target Heavitree Formation reservoir was absent, but hydrocarbon and helium gas flows were recorded from fractured igneous basement, opening a new play type. This permit contains a variety of structural styles, and additional opportunities have been identified from potential field data and the extensive 2013 and 2016/2018 seismic data.