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High-resolution well-log derived dielectric properties of gas-hydrate-bearing sediments, Mount Elbert Gas Hydrate Stratigraphic Test Well, Alaska North Slope
被引:23
|作者:
Sun, Y.
[1
]
Goldberg, D.
[2
]
Collett, T.
[3
]
Hunter, R.
[4
]
机构:
[1] Texas A&M Univ, Dept Geol & Geophys, College Stn, TX 77843 USA
[2] Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY USA
[3] US Geol Survey, Denver, CO 80225 USA
[4] ASRC Energy Serv, Anchorage, AK USA
关键词:
Gas hydrates;
Saturation;
Dielectric property;
METHANE HYDRATE;
RESERVOIR;
D O I:
10.1016/j.marpetgeo.2010.03.001
中图分类号:
P [天文学、地球科学];
学科分类号:
07 ;
摘要:
A dielectric logging tool, electromagnetic propagation tool (EPT), was deployed in 2007 in the BPXA-DOE-USGS Mount Elbert Gas Hydrate Stratigraphic Test Well (Mount Elbert Well), North Slope, Alaska. The measured dielectric properties in the Mount Elbert well, combined with density log measurements, result in a vertical high-resolution (cm-scale) estimate of gas hydrate saturation. Two hydrate-bearing sand reservoirs about 20 m thick were identified using the EPT log and exhibited gas-hydrate saturation estimates ranging from 45% to 85%. In hydrate-bearing zones where variation of hole size and oil-based mud invasion are minimal, EPT-based gas hydrate saturation estimates on average agree well with lower vertical resolution estimates from the nuclear magnetic resonance logs; however, saturation and porosity estimates based on EPT logs are not reliable in intervals with substantial variations in borehole diameter and oil-based invasion. EPT log interpretation reveals many thin-bedded layers at various depths, both above and below the thick continuous hydrate occurrences, which range from 30-cm to about 1-m thick. Such thin layers are not indicated in other well logs, or from the visual observation of core, with the exception of the image log recorded by the oil-base microimager. We also observe that EPT dielectric measurements can be used to accurately detect fine-scale changes in lithology and pore fluid properties of hydrate-bearing sediments where variation of hole size is minimal. EPT measurements may thus provide high-resolution in-situ hydrate saturation estimates for comparison and calibration with laboratory analysis. (C) 2010 Elsevier Ltd. All rights reserved.
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页码:450 / 459
页数:10
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