Overview
This integrated Upper Permian study focuses on the upper part of the Wagina and Dongara Sandstones and their transition into the Hovea Member across a 2000+ km² area, encompassing both mature petroleum fields and new discoveries in the Dandaragan Trough.
Through detailed core logging, cross-sectional stratigraphic analysis, and new quantitative palynological sampling, this multi-client study aims to improve depositional models and identify untapped prospectively across these key intervals.
Updated Depositional Model
Better characterisation of reservoir facies within an updated depositional and paleogeographic model.
Revised Sequence Stratigraphy
A revised sequence-stratigraphic framework that will increase the confidence in well-to-well correlations.
New Palynological Data
New palynological assignments for the upper Permian–lower Triassic intervals in wells with limited or absent biostratigraphic control.
Greater Stratigraphic Control
Better prediction of the type and regional extent of upper Permian reservoir units.
Background
The northern Perth Basin has long been regarded as a proven and mature hydrocarbon province undergoing progressive field depletion (e.g. Dongara, Yardarino, Mondarra, Beharra Springs, Woodada) of mostly upper Permian sandstone and limestone plays at depths 1600–3300 m since first production in the 1970s. The basin’s prospectivity has, however, been considerably revitalised in the past 10 years following discovery of the Waitsia Field and some of the largest conventional onshore reservoirs in Australia hosted in previously marginally appraised lower Permian plays.
Renewed petroleum activity in the northern Perth Basin has unsurprisingly led to focus exploration endeavours on the lower Permian reservoirs. Nevertheless, a 2MMscfd gas flow rate in Strike Energy’s L24 (2022) and two oil discoveries representing 20.5 MMboe (2C contingent resources) in Mineral Resources’ EP426 (2023–2024) in the upper Permian Dongara–Wagina sandstones demonstrated porosity preservation at depth >3000 m and untapped economic potential in areas that were previously considered high-risk and unattainable.
Despite the recent discoveries, considerable uncertainties remain as to the spatial distribution of late Permian facies belts, the depositional and structural controls that drove sediment deposition, and the stratigraphic evolution of the upper Permian succession. Ferdinando and Longley (2015) identified that nearly a quarter of dry wells targeting upper Permian plays are due to a lack of porous reservoir lithologies.
| Well | Sub-basin | Formation(s) | Material |
|---|---|---|---|
| Jingemia 4 | Dongara Terrace | Hovea Mbr, Dongara Sst, Wagina Sst, Carynginia Fm | Core 1-3 |
| Senecio 3 | Dandaragan Trough | Dongara Sst, Wagina Sst | Core 1 |
| Lockyer 1 | Dandaragan Trough | Dongara Sst | Core 1 |
| Yardarino 2 | Dandaragan Trough | Hovea Mbr, Dongara Sst | Core 2-7 |
| Hovea 3 | Beharra Springs Terrace | Hovea Mbr, Dongara Sst, Wagina Sst | Core 1-3 |
| Mondarra 1 | Dandaragan Trough | Dongara Sst | Core 4-6 |
| Mondarra 7 | Dandaragan Trough | Hovea Mbr, Dongara Sst, Wagina Sst | Core 1 |
| Apium 1 | Dandaragan Trough | Dongara Sst, Hovea Mbr | Core 1-2 |
| Dongara 11 | Dongara Terrace | Dongara Sst, Wagina Sst | Core 1-4 |
| Dongara 27 | Beharra Springs Terrace | Dongara Sst | Core 1 |
| Central Yardarino 1 | Dandaragan Trough | Dongara Sst, Bookara Sst | Core 1 |
| Yardarino 1 | Dandaragan Trough | Dongara Sst, Wagina Sst | Core 11-17 |
| Warradong 1 | Dandaragan Trough | Dongara Sst | Core 1-2 |
| Centella 1 | Dandaragan Trough | Dongara Sst, Hovea Mbr | Core 1 |
Table 1: Fourteen cored wells selected for the sedimentological analysis.
Figure 1: Location of proposed cross-sections (click on the image to enlarge).
Deliverables
Along with a detailed sedimentology report outlining lithofacies, depofacies, a proposed depositional model, and paleogeographic maps, this study includes:
Detailed Core Descriptions
Core descriptions at the 1:50 scale of 14 wells totalling 509 m of sedimentary strata.
Integrated Datasets
Integration with wireline logs, core photographs and RCA data. Core to well log shifts, where applicable.
Digital Exports
Tabulated cm-scale exports of sedimentological attributes (grain size, sorting, lithology, lithofacies, depofacies).
Basin-wide Cross-sections
Five basin-scale cross-sections with correlations of interpreted sequence-stratigraphic surfaces and units.
Sequence Stratigraphy
Stratigraphic report detailing the proposed sequence-stratigraphic framework.
Updated Palynology
New palynological assignments across the study interval.
