Deep-Water Reservoirs of the World: 20th Annual 2000
DOI: 10.5724/gcs.00.15.0263
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The Inter-Relationships of Scales of Heterogeneity in Subsurface, Deep Water E&P Projects—Lessons Learned from the Mount Messenger Formation (Miocene), Taranaki Basin, New Zealand

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Cited by 5 publications
(3 citation statements)
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“…High-resolution, near-surface geophysical data has the advantage of sampling a comparative large area behind outcrop cliff-faces given the right site and ground conditions (Table 1) which can be integrated into digital surface models. Shallow seismic data have been acquired behind outcrop cliff-faces, but usually with little success, chiefly due to the cemented nature of the sediments providing little or no acoustic impedance contrast between different sedimentary intervals (Coleman et al, 2000). Typically relatively thin target zones are still below near-surface seismic resolution.…”
Section: High Technology Near-surface Methodsmentioning
confidence: 99%
“…High-resolution, near-surface geophysical data has the advantage of sampling a comparative large area behind outcrop cliff-faces given the right site and ground conditions (Table 1) which can be integrated into digital surface models. Shallow seismic data have been acquired behind outcrop cliff-faces, but usually with little success, chiefly due to the cemented nature of the sediments providing little or no acoustic impedance contrast between different sedimentary intervals (Coleman et al, 2000). Typically relatively thin target zones are still below near-surface seismic resolution.…”
Section: High Technology Near-surface Methodsmentioning
confidence: 99%
“…High-resolution, shallow seismic geophysical data have been obtained behind outcrop cliff faces, but usually with little success (see Coleman et al 2000). This is chiefly due to the cemented nature of the sediments, providing little or no acoustic impedance contrast between sedimentary intervals.…”
Section: Introductionmentioning
confidence: 99%
“…With this in mind, the acquisition of seismic data over outcrop analogues has been tested, but, to date, has largely proved unsuccessful (Coleman et al 2000), most probably due to the cemented and commonly fractured nature of ancient rocks, which reduces density and impedance contrasts across lithological boundaries. Ground Penetrating Radar (or GPR) was used successfully to obtain 3D cubes of data behind outcrop cliff-faces (Jol et al 2003;Pringle et al 2003;Staggs et al 2003;Young et al 2003), albeit at a shallow level, normally a maximum penetration of 10 m below ground level.…”
Section: Introductionmentioning
confidence: 99%