Carnarvon Basin Architecture and Structure Defined by the Integration of Mineral and Petroleum Exploration Tools and Techniques

Abstract

The Barrow and Dampier Sub-basins of the Northern Carnarvon Basin developed by repeated reactivation of long-lived basement structures during Palaeozoic and Mesozoic tectonism. Inherited basement fabric specific to the terranes and mobile belts in the region comprise northwest, northeast, and north–south-trending Archaean and Proterozoic structures. Reactivation of these structures controlled the shape of the sub-basin depocentres and basement topography, and determined the orientation and style of structures in the sediments.The Lewis Trough is localised over a reactivated NEtrending former strike-slip zone, the North West Shelf (NWS) Megashear. The inboard Dampier Sub-basin reflects the influence of the fabric of the underlying Pilbara Craton. Proterozoic mobile belts underlie the Barrow Sub-basin where basement fabric is dominated by two structural trends, NE-trending Megashear structures offset sinistrally by NS-trending Pinjarra structures.The present-day geometry and basement topography of the basins is the result of accumulated deformation produced by three main tectonic phases. Regional NESW extension in the Devonian produced sinistral strikeslip on NE-trending Megashear structures. Large Devonian-Carboniferous pull-apart basins were introduced in the Barrow Sub-basin where Megashear structures stepped to the left and are responsible for the major structural differences between the Barrow and Dampier Sub-basins. Northwest extension in the Late Carboniferous to Early Permian marks the main extensional phase with extreme crustal attenuation. The majority of the Northern Carnarvon basin sediments were deposited during this extensional basin phase and the subsequent Triassic sag phase. Jurassic extension reactivated Permian faults during renewed NW extension. A change in extension direction occurred prior to Cretaceous sea floor spreading, manifest in basement block rotation concentrated in the Tithonian. This event changed the shape and size of basin compartments and altered fluid migration pathways.The currently mapped structural trends, compartment size and shape of the Barrow and Dampier Sub-basins of the Northern Carnarvon Basin reflect the “character” of the basement beneath and surrounding each of the subbasins.Basement character is defined by the composition, lithology, structure, grain, fabric, rheology and regolith of each basement terrane beneath or surrounding the target basins. Basement character can be discriminated and mapped with mineral exploration methods that use non-seismic data such as gravity, magnetics and bathymetry, and then calibrated with available seismic and well datasets. A range of remote sensing and geophysical datasets were systematically calibrated, integrated and interpreted starting at a scale of about 1:1.5 million (covering much of Western Australia) and progressing to scales of about 1:250,000 in the sub-basins. The interpretation produced a new view of the basement geology of the region and its influence on basin architecture and fill history. The bottom-up or basement-first interpretation process complements the more traditional top-down seismic and well-driven exploration methods, providing a consistent map-based regional structural model that constrains structural interpretation of seismic data.The combination of non-seismic and seismic data provides a powerful tool for mapping basement architecture (SEEBASE™: Structurally Enhanced view of Economic Basement); basement-involved faults (trap type and size); intra-sedimentary geology (igneous bodies, basement-detached faults, basin floor fans); primary fluid focussing and migration pathways and paleo-river drainage patterns, sediment composition and lithology.

Fault inversion contributes to ground deformation above inflating igneous sills

“…Our study area is located within the Exmouth Plateau, a region of the North Carnarvon Basin containing <10 km thick, stretched continental crust and an up to 18 km thick sedimentary sequence (Figure 1) [e.g. Exon et al 1992;Karner and Driscoll 1999;Pryer et al 2002;Stagg et al 2004]. To the north and west of the Exmouth Plateau are the Argo and Gascoyne abyssal plains, respectively, which consist of oceanic crust; between the Exmouth Plateau and the Gascoyne Abyssal Plain is a 200-250 km wide continent-ocean transition zone comprising heavily intruded continental crust ( Figure 1A) [e.g.…”

Middle Miocene–Pliocene siliciclastic influx across a carbonate shelf and influence of deltaic sedimentation on shelf construction, Northern Carnarvon Basin, Northwest Shelf of Australia

“…Since the Early Cretaceous, the dominant tectonic control has been thermal subsidence (Veevers et al ., ; Baillie et al ., ; Driscoll & Karner, ; Cathro & Karner, ). Several studies have suggested an interruption of such subsidence because of collision between the Banda Arc and Australia, which began in the late Miocene (Veevers et al ., ; Baillie et al ., ; Lee & Lawver, ; Driscoll & Karner, ; Hull & Griffiths, ; Pryer et al ., ; Cathro & Karner, ). However, the impact of this collision on the NCB has been limited to localized uplift (only up to 75 m) at the northwest end of the Rosemary–Legendre structural trend during the Miocene, inferred from seismic stratigraphy integrated with kinematic and flexural modelling in the adjacent Dampier sub‐basin (Figs a and ; Cathro & Karner, ).…”

“…The locations of other figures shown in this paper are indicated by bold numbers. which began in the late Miocene (Veevers et al, 1991;Baillie et al, 1994;Lee & Lawver, 1995;Driscoll & Karner, 1998;Hull & Griffiths, 2002;Pryer et al, 2002;Cathro & Karner, 2006). However, the impact of this collision on the NCB has been limited to localized uplift (only up to 75 m) at the northwest end of the Rosemary-Legendre structural trend during the Miocene, inferred from seismic stratigraphy integrated with kinematic and flexural modelling in the adjacent Dampier sub-basin (Figs 1a and 2; Cathro & Karner, 2006).…”

Fault inversion can accommodate ground deformation above inflating igneous sills

“…Our study area is located within the Exmouth Plateau, a region of the North Carnarvon Basin containing <10 km thick, stretched continental crust and an up to 18 km thick sedimentary sequence (Fig. 1) [e.g., Exon et al, 1992;Karner and Driscoll, 1999;Pryer et al, 2002;Stagg et al, 2004]. To the north and west of the Exmouth Plateau are the Argo and Gascoyne abyssal plains, respectively, which consist of oceanic crust; between the Exmouth Plateau and the Gascoyne Abyssal Plain is a 200-250 km wide continent-ocean transition zone 5 comprising heavily intruded continental crust (Fig.…”