
Vol. 59 No. 9
September 2007
The Thylacine gas field is in the Otway basin (offshore southeast Australia). The interplay of intrafield faulting and the layered geology provide potential for a high degree of compartmentalization. A significant proportion of the reserves is thought to reside in reservoirs of the Thylacine sandstone member, which contains poor-quality marine sands interbedded with successions of shale and thinly bedded sand/shale. Key to designing wells to achieve satisfactory deliverability was an understanding of the distribution of net reservoir in the background of nonreservoir.
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