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Identifying a gas hydrate production zone using a cased-hole borehole acoustic-reflection survey, Aurora/JOGMEC/NRCan Mallik 2L-38 gas hydrate production research well
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In 2007, data were acquired from a borehole acoustic-reflection survey (BARS), using the latest Sonic Scanner tool, in a gas-hydrate-bearing formation in the Mallik field, Mackenzie Delta, Northwest Territories. The BARS data were logged in a cased-hole
environment in which no azimuthal information could be recovered, thus limiting the final migration image-processing and interpretation. Performing BARS in a cased hole is less favourable than in an open-hole environment because the high-amplitude casing arrivals make the identification of reflected
energy very challenging. In addition, no tool orientation data are usable in a cased hole due to the lack of reliable measurement of the Earth's magnetic field. In this paper, we present results acquired in a cased-hole environment and indicate correlations of BARS data with auxiliary logs.
The perforation zone is identified in the raw and filtered wave-form BARS data. Energy in the 1098 to 1105 m depth interval is significantly stronger, and this zone of higher amplitudes appears to extend into the formation. This zone is assumed to be directly related to changes in the formation
caused by the perforations and/or production in the lower half of the production-test interval. Several additional reflections can be observed in the raw and filtered wave forms. The gamma-ray and density logs indicate formation changes at the same depths at which these reflections occur. These
formation boundaries and the reflections also correlate well with the fullbore microresistivity image logs. The results indicate that BARS data can be used to achieve a more complete, detailed, and thus enhanced log interpretation.
Natural Resources Canada/CMSS/Information Management
Title: Identifying a gas hydrate production zone using a cased-hole borehole acoustic-reflection survey, Aurora/JOGMEC/NRCan Mallik 2L-38 gas hydrate production research well
Description:
In 2007, data were acquired from a borehole acoustic-reflection survey (BARS), using the latest Sonic Scanner tool, in a gas-hydrate-bearing formation in the Mallik field, Mackenzie Delta, Northwest Territories.
The BARS data were logged in a cased-hole
environment in which no azimuthal information could be recovered, thus limiting the final migration image-processing and interpretation.
Performing BARS in a cased hole is less favourable than in an open-hole environment because the high-amplitude casing arrivals make the identification of reflected
energy very challenging.
In addition, no tool orientation data are usable in a cased hole due to the lack of reliable measurement of the Earth's magnetic field.
In this paper, we present results acquired in a cased-hole environment and indicate correlations of BARS data with auxiliary logs.
The perforation zone is identified in the raw and filtered wave-form BARS data.
Energy in the 1098 to 1105 m depth interval is significantly stronger, and this zone of higher amplitudes appears to extend into the formation.
This zone is assumed to be directly related to changes in the formation
caused by the perforations and/or production in the lower half of the production-test interval.
Several additional reflections can be observed in the raw and filtered wave forms.
The gamma-ray and density logs indicate formation changes at the same depths at which these reflections occur.
These
formation boundaries and the reflections also correlate well with the fullbore microresistivity image logs.
The results indicate that BARS data can be used to achieve a more complete, detailed, and thus enhanced log interpretation.
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