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Banda Arc: Broadband 2D

BandaSeis 2D seismic line Seismic Unlocks Frontier Area locations by phase, and corresponding offshore areas. CGG’s high quality BandaSeis 2D seismic data set, acquired and recently reprocessed with the latest imaging technology, and accompanying comprehensive Jumpstart™ geological study enhance the exploration potential of the Banda Arc region. Enhanced velocity model resolution. Original 2012 vs 2018 reprocessing. Interpreted BandaSeis 2D seismic section showing The BandaSeis multi-client programme is located within Eastern ’s Banda Arc region enhanced imaging of which, although a proven hydrocarbon province, is largely underexplored with large undrilled decollement and Mesozoic successions below the fold and areas and poorly understood petroleum system elements. thrust belt.

The surveys were acquired and processed using CGG’s BroadSeis broadband imaging solution to clearly define new play levels in the area, including Mesozoic sub-thrust plays.

BandaSeis 2D line intersecting the Trough. Enhanced imaging enables interpretation of Late Palaeozoic and N Mesozoic successions, pushed down into the hydrocarbon generation window beneath the fold and thrust belt. S JARRAD GRAHAME New Broadband Imaging Reveals and PEDRO MARTINEZ DURAN, Prospectivity Insights CGG New high quality seismic datasets and a regional prospectivity study bring greater understanding of the distribution and extent of resource plays throughout the Banda Arc.

CGG acquired its BandaSeis broadband multi-client 2D and orogeny (Hall, 2012). This highly dataset around the entire Banda Arc region of Eastern complicated and hence poorly understood geological CGG Indonesia using its advanced BroadSeis™ acquisition and region represents one of the most tectonically active Legacy vs reprocessing velocity model showing the high level of geologically consistent detail provided by HF-FWI. imaging solution. areas in the world. The key objectives of the programme were to provide The Banda Arc exhibits a characteristic curvilinear BandaSeis 2D - Key Technologies detailed prospect-level interpretation. CGG also correlated enhanced imaging of sub-thrust successions and geometry and can be divided into four main tectonic The BandaSeis 2D seismic programme was acquired in five the seismic interpretation with structural and potential field structuring and to better constrain the Palaeozoic and regions: an outer arc comprising a continental lithosphere successive phases over a period of three years, from 2012 data analyses undertaken in parallel in a regional context. Mesozoic petroleum system elements, which are widely and the larger , the major ones being Timor and to 2015. It used CGG’s proprietary BroadSeis broadband Some key highlights from the interpretation and analyses regarded as equivalent to the northern Bonaparte and Seram; an inner ; the Weber Deep between acquisition and imaging solution with 10 km maximum included identification of a new Jurassic sub-basin; mapping Browse Basins of the North West Shelf of . the Inner and Outer arcs at the area of greatest curvature; offset streamers. It utilises a unique variable-depth streamer of a Mesozoic palaeo-high that changes the understanding of The five phases of the BandaSeis programme represent and the fold-and-thrust belts that formed outboard of the profile and CGG’s proprietary broadband processing deposition and thermal history; new structural insights into 16,409 line-km of 2D broadband seismic data, with Outer Arc (Baillie et al., 2014). technology, including ghost wavefield elimination, to the whole Banda Arc tectonic evolution; and identification coverage from the of Timor in the south to Seram Eight key petroleum systems within the southern Banda produce superior imaging results compared to conventional and evaluation of 42 new leads throughout the Banda Arc in the north, including a single regional line across the Arc region can be summarised, analogously based on datasets. offshore areas. These key highlights, which underlie the Weber Deep and the entire Banda Sea. geological and geochemical information derived from the The first three phases of the data set were reprocessed by discovery of new prospectivity insights, can be directly The data was processed to PSDM using CGG’s Bonaparte Basin (Barrett et al., 2004). They range from CGG utilising an updated broadband processing sequence attributed to the ability to image beneath the fold and thrust advanced techniques to significantly enhance image late Palaeozoic to late Mesozoic, including three Jurassic and advanced full-waveform inversion (FWI) velocity belt, since, for the first time, geological structures can be quality, with further reprocessing undertaken in 2018 on systems, one Triassic, three Permian, and one Permo- model building to enhance visualisation of potential targets clearly seen below more than 5,000m of orogenic wedge three of the five phases of the dataset. The resulting PSDM Carboniferous system. underlying highly-deformed fold and thrust belts, and to sediments. Most importantly, the new level of imaging products provided unrivalled image quality, particularly Within the central Banda Arc/Tanimbar region the improve the low-frequency content of the data (Ping et al., quality enables a greater understanding of the distribution below the fold and thrust belts of the arc system. hydrocarbon-generative sequences are considered to be an 2019). High-frequency FWI (HF-FWI) was applied to the and extent of resource plays. CGG has also conducted a comprehensive regional extension of those within the Timor area, and therefore data to produce a higher-resolution velocity model with A comprehensive regional study produced to Jumpstart™ prospectivity study leveraging new also North West Shelf equivalents. For the Tanimbar area, greatly improved correlation with the geology, as seen in complement the dataset will enhance understanding of information derived from the enhanced data. these petroleum systems include two Jurassic and three the velocity model comparison above. The FWI technology the palaeogeography and petroleum systems of the Banda Palaeozoic sourced systems, equivalent to the Jurassic overcomes the limitations of conventional reflection Arc. This integrated approach to understand the total Geological Overview Echuca Shoals and Plover Formations of the Browse tomography in complex settings where the curvature picking depositional systems in a geodynamic context allows for The Banda Arc is located within a complex convergence Basin, and the Permo-Carboniferous Milligans-Kuriyippi and inversion are less reliable and stable. progressive de-risking of emerging plays and will underpin zone between the Eurasian, Australian and Pacific systems of the Bonaparte Basin. Another key technology employed was joint source future exploration success in the region. tectonic plates, resulting in intense deformation, The northern Banda Arc region, including Seram and designature and deghosting, which produces a more stable its offshore area, hosts Lower Jurassic source rocks with wavelet phase, particularly in the low-frequency range. Acknowledgements Banda Arc regional tectonic elements. potential contribution from Cretaceous, Application of these key technologies enhanced data quality The authors wish to thank CGG Multi-Client for permission Triassic and Permian intervals. and the ability to constrain geological features below the to publish this work and CGG Geoscience for their Abundant onshore and offshore complex deformation zone. significant contribution to these results. seeps attest to the widespread presence of active source rocks throughout the Prospectivity Insights from Regional Interpretation References available online. Banda Arc, making the area of particular Given significant knowledge gaps in the geology of the interest for hydrocarbon exploration. region, and a number of supporting indicators of active Detailed imaging: decollement beneath fold and thrust belt revealed by the reprocessing of Phase 1 using the latest broadband processing and HF-FWI. Factors influencing the limited petroleum systems, CGG initiated a major regional

exploration to date include remoteness study, deriving key insights from the data. The Banda Arc CGG and water depths. However, seismic Jumpstart study involved an integrated methodology, imaging challenges, particularly beneath leveraging the company’s extensive multidisciplinary the fold and thrust belts, represent geoscience resources. This work included new interpretation the key contributor to exploration of the dataset, correlation of satellite slicks and seismic uncertainty. CGG has sought to data, onshore field studies, including source rock and live ameliorate this by providing high quality oil seep sampling for geochemical analyses, integration images beneath zones of significant of seismic, well and potential fields data, basin modelling, deformation and by undertaking and palaeogeographic reconstructions. The new seismic complementary, integrated geological interpretation, covering the entire BandaSeis dataset, interpretation and analyses to mitigate was undertaken in two phases: firstly, within a regional CGG exploration risk. structural and stratigraphic context; and secondly, with a

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