1887

Abstract

Summary

Data received by seismic reflection profiling show that in the Gulf of Ob starting from the depth of 1–2 meters under mudline almost everywhere sediments saturated by non-associated gas are presented. The presence of nonassociated gas does not allow exploring deeper levels of sedimentation masses. Usage of thorough interpretation of magnetic response allowed to locate the area of tectonic tension of earth material, which was apparently the fault zone complicated with intrusive formations. Due to the lack of a priory information and possibility to make a comprehensive assessment of geology and geophysics data, the 2d modeling was impossible on the present stage. A case study of computational methods shows that the depth of tectonic dislocation area cannot be more than 250 meters.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201901824
2019-04-22
2024-04-19
Loading full text...

Full text loading...

References

  1. Методические рекомендации по подготовке Технических Проектов разработки месторождения углеводородного сырья. Утверждены распоряжением Минприроды России от 18.05.2016 № 12-р.
  2. СП 11-114-2004 Инженерные изыскания на континентальном шельфе для строительства морских нефтегазопромысловых сооружений, Москва, 2004.
  3. TóthZ, SpiessV, MogollónJ., JensenJ.
    Estimating the free gas content in Baltic Sea sediments using compressional wave velocity from marine seismic data. Journal of Geophysical Research: Solid Earth. Volume 119, issue 12. 2014. P. 8577−8593.
    [Google Scholar]
  4. Metodicheskie rekomendacii po podgotovke Tekhnicheskih Proektov razrabotki mestorozhdeniya uglevodorodnogo syr'ya. Utverzhdeny rasporyazheniem Miprirody Rossii ot 18.05.2016 № 12-r.
  5. SP 11-114-2004 Inzhenernye izyskaniya na kontinental'nom shel'fe dlya stroitel'stva morskih neftegazopromyslovyh sooruzhenij, Moskva, 2004.
  6. TóthZ, SpiessV, MogollónJ., JensenJ.
    Estimating the free gas content in Baltic Sea sediments using compressional wave velocity from marine seismic data. Journal of Geophysical Research: Solid Earth. Volume 119, issue 12. 2014. P. 8577−8593.
    [Google Scholar]
http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201901824
Loading
/content/papers/10.3997/2214-4609.201901824
Loading

Data & Media loading...

This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error