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COMPOSITIONAL DATA : GAS : GAS PROPERTIES Puffin Fm RFT ...

COMPOSITIONAL DATA : GAS : GAS PROPERTIES Puffin Fm RFT ...

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Accumulation Number: 59SWANORIGINAL OPERATOR:TYPE:STATUS:LOCATION:STATE:ORIGINAL TITLE(S):BASIN:SUB-BASIN:DISCOVERY WELL:Longitude (E): 124.4928Latitude (S): -12.1882Date total depth reached: 30 JAN 73Water Depth:Kelly bushing:Operator:Total Depth:NUMBER OF WELLS DRILLED:STRUCTURE/TRAP:AREAL CLOSURE: 6 km 2VERTICAL CLOSURE:270 mRESERVOIR UNITS:NET PAY:NET TO GROSS RATIO:HYDROCARBON SATURATION:BOTTOM HOLE TEMPERATURE:Arco Australia LtdGasOther Discovery700 km west of DarwinTerritory of Ashmore and Cartier Islands Adjacent Area(Northern Territory)NT/P2BonaparteVulcan Sub-basinSwan-1109 m34 mArco Australia Ltd3,284 mKB4 (including 1 sidetrack)Northeast-southwest trending horst block with updipclosure dependent on fault seal against a salt diapir.Several, thin gas bearing sands identified on logs in theLate Cretaceous section (informally named the P1, P2, P3and P4 reservoir sands).11.25 m (Swan-1, P1 and P2 sands)22.1 m (Swan-2, P1, P2 and P3 sands)19.4 m (Swan-3, P1 and P2 sands)32.7 m (Swan-3/ST1, P1, P2 and P3 sands)75% (Swan-3, 2,306-2,332 mKB, P1 and P2 sands)55% (Swan-3/ST1, 2,342-2,375 mKB, P1 and P2 sands)93% (Swan-3/ST1, 2,445-2,461 mKB, P3 sand).57% (Swan-1, P1 and P2 sands)82% (Swan-2, P1, P2 and P3 sands)32% (Swan-3, P1 and P2 sands)75% (Swan-3/ST1, P1, P2 and P3 sands)100 o CPETROLEUM BEARING UNIT No.1:CONTENTS:FORMATION:AGE:LITHOLOGY:DEPOSITIONAL ENVIRONMENT:FORMATION TOP (mKB):POROSITY:Bathurst Island GroupGas<strong>Puffin</strong> FormationLate CretaceousSandstone, clean, fine to medium grained, subangular,well sorted, excellent visual porosity. Fluid escapestructures, dish structures, flame structures and waterescape pipes are observed in cores.Stacked, submarine fan sandstone sequence.2,152.8 m (Bathurst Island Group)18.9% (average log porosity, Swan-1, P1 and P2 sands)23% (average log porosity, Swan-3, P1 and P2 sands)20% (average log porosity, Swan-3/ST1, P1, P2 and P3sands).

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