Geoteric | April 4, 2014

Case Study: The use of geological expression workflows for basin scale reconnaisance

Case Study: The use of geological expression workflows for basin scale reconnaisance

Geoteric on 04 Apr 2014
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The use of geologic expression workflows for basin scale reconnaissance: A case study from the Exmouth Subbasin, North Carnarvon Basin, northwestern Australia

by: N. McArdle (ffA), D.Iacopini (University of Aberdeen), M. KunleDare (ffA) and G.Paton (ffA) 

The focus of this study is to demonstrate how seismic attributes can be used in the interpretation workflow to  rapidly obtain a high-resolution view of the geology that is imaged within a seismic data set.

Basemap showing location of Indian, Vincent and HCA200A 3D surveys
of the Exmouth subbasin, northwestern Australia 
To demonstrate the  efficacy of seismic attribute analysis to basin scale reconnaissance, we apply a workflow to seismic data sets from  the Exmouth Subbasin, northwestern Australia, with the aim of determining the geologic expression of the subsurface.  Of specific interest are Barrow Group Jurassic and Cretaceous fluvial and marine sediments, that were  faulted during the Jurassic-Cretaceous rifting associated with the breakup of East Gondwana. 
Regional-scale interpretations  are made to develop a tectonostratigraphic context to the investigation. Target-level analyses, focused  on features of exploration interest identified using regional reconnaissance, are made to calibrate attribute  response and demonstrate the effectiveness of seismic attributes for rapid evaluation of prospectivity in the initial  stages of exploration. 
The main structural episodes are distinguished using dip and azimuth attributes, and faulting  is expressed using a combination of edge attributes which are used to create fault trend lineations. We observe  three main structural trends: the main northeast–southwest Jurassic-Cretaceous syn-rift primary fault orientation  of 48°, a secondary trend of 108°, taken to represent secondary conjugate faulting and a third trend of 100° interpreted  as the reactivation of these faults into the postrift sediments.
Stratigraphic attributes that respond to  amplitude and frequency are used to create reservoir scale geobodies of faulted Macedon turbidites, which in turn  are used for detailed tuning sensitivity analysis.
The final part of the investigation is of the syn-riftmagmatic system  responsible for sills and dikes that exploit the normal fault network. These intrusive and extrusive features are important as are potential drilling hazards and can act as baffles to hydrocarbon migration.

Examples of structural and fault attributes applied to the Exmouth Subbasin seismic data to distinguish structural elements within HCA2000A, imaged using dip-azimuth, composite SOS-tensor-SOD, fault trends and frequency decomposition RGB blend.  

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