Home JOURNAL HEADINGS Author Index SUBJECT INDEX INDEX OF ORGANIZATIONS Article Index
 
Arctic: ecology and economy
ISSN 2223-4594
RuEn
Advanced
Search
ABOUT|EDITORIAL|INFO|ARCHIVE|FOR AUTHORS|SUBSCRIBE|CONTACTS
Home Archive of journals Issue 1(37) 2020 Engineering and geological conditions for the development of the water part of the Kruzenshtern deposit in the Kara Sea

ENGINEERING AND GEOLOGICAL CONDITIONS FOR THE DEVELOPMENT OF THE WATER PART OF THE KRUZENSHTERN DEPOSIT IN THE KARA SEA

JOURNAL: 2020, 1(37), p. 95-108

HEADING: Study and development of nature resources of the Arctic

AUTHORS: Dzublo A.D., Alekseeva K.V.

ORGANIZATIONS: Oil and Gas Research Institute of RAS, Gubkin Russian State University of Oil and Gas (National Research University)

DOI: 10.25283/2223-4594-2020-1-95-108

UDC: 553.44:553.061

The article was received on: 31.10.2019

Keywords: Kruzenshtern deposit, shallow water shelf, engineering and geological surveys, geocryological conditions, near-surface intervals of abnormally high reservoir pressure (AHRP), gas resources

Bibliographic description: Dzublo A.D., Alekseeva K.V. Engineering and geological conditions for the development of the water part of the Kruzenshtern deposit in the Kara Sea. Arctic: ecology and economy, 2020, no. 1(37), pp. 95-108. DOI: 10.25283/2223-4594-2020-1-95-108. (In Russian).


Abstract:

The authors consider engineering surveys necessary to obtain data on the bottom topography, sea depth, characteristics of engineering-geological, hydrometeorological and ice conditions, which later will help to choose methods and technical means for exploration drilling, and will allow making the necessary calculations for setting the drilling rig at detailed site. As a result of engineering surveys at the Kruzenshtern deposit, dangerous physical and geological phenomena are identified: the presence of frozen rocks in the section at depths from 50 to 200 meters; the possible presence of abnormally high reservoir pressure (AHRP) intervals, while the most dangerous, from this point of view, are the intervals associated with the base of the permafrost rocks (PR).


References:

1. Nikitin B. A., Dzyublo A. D., Shuster V. L. Geologo-geofizicheskaya otsenka perspektiv neftegazonosnosti glubokozalegayushchikh gorizontov poluostrova Yamal i Priyamal’skogo shel’fa Karskogo morya. [Geological and geophysical assessment of the prospects for oil and gas presence in the deep-lying horizons of the Yamal Peninsula and the Priyamalsky shelf of the Kara Sea]. Neftyanoe khoz-vo, 2014, no. 11, . 102—106. (In Russian).
2. Nauchno-tekhnicheskiy otchet “Razrabotka tekhnicheskikh resheniy po osvoeniyu mestorozhdeniy uglevodorodov na predel’no melkovodnom arkticheskom shel’fe RF (na primere Priyamal’skogo shel’fa Karskogo morya)” po dogovoru s PAO “Gazprom”. [Scientific and technical report “Development of technical solutions for the development of hydrocarbon deposits on the extremely shallow Arctic shelf of the Russian Federation (using the Priyamalsky shelf of the Kara Sea as an example)” under an agreement with Gazprom]. RGU nefti i gaza (NIU) imeni I. M. Gubkina. Moscow, 2013. (In Russian).
3. Dzyublo A. D., Alekseeva K. V. Tekhnologii i osobennosti osvoeniya mestorozhdeniy uglevodorodov v melkovodnykh tranzitnykh zonakh Priyamal’skogo shel’fa Karskogo morya. [Technologies and features of the development of hydrocarbon deposits in the shallow-water transit zones of the Priyamalsky shelf of the Kara Sea]. Tr. RGU nefti i gaza imeni I. M. Gubkina, 2019, no. 1 (294), . 17—29. (In Russian).
4. Rokos S. I., Kulikov S. N., Korotkov S. V. et al. Tekhnicheskiy otchet po ob”ektu “Inzhenernye izyskaniya v predelakh Kruzenshternskogo uchastka”. [Technical report on the object: “Engineering surveys within the Kruzenshternsky site”]. OAO “AMIGE”. Murmansk, 2011, 181 . (In Russian).
5. Yakushev V. S. Prirodnyy gaz i gazovye gidraty v kriolitozone. [Natural gas and gas hydrates in the cryolithozone]. Moscow, VNIIGAZ, 2009, 192 . (In Russian).
6. Badu Yu. B. Gazonosnye struktury i kriogennaya tolshcha kriolitologicheskikh provintsiy Yamala. [Gas-bearing structures and cryogenic strata of the cryolitological provinces of Yamal]. Inzhener. geologiya, 2017, no. 1, . 39—52. (In Russian).
7. Bondarev V. N., Dlugach A. G., Kostin A. D., Lisunov V. K., Rokos S. I. Akusticheskie fatsii postkriogennykh obstanovok melkovodnykh rayonov Pechorskogo i Karskogo morey. [Acoustic facies of post-cryogenic conditions in shallow areas of the Pechersk and Kara Seas]. Razvedka i okhrana nedr, 1999, no. 7—8, . 10—14. (In Russian).
8. Rokos S. I. Inzhenerno-geologicheskie osobennosti pripoverkhnostnykh zon anomal’no vysokogo plastovogo davleniya na shel’fe Pechorskogo i yuzhnoy chasti Karskogo morey. [Geotechnical features of the near-surface zones of abnormally high reservoir pressure on the shelf of the Pechora and the southern part of the Kara Sea]. Inzhener. geologiya, 2008, no. 4, . 22—28. (In Russian).
9. Bogoyavlensky V. I., Sizov O. S., Bogoyavlensky I. V., Nikonov R. A. Distantsionnoe vyyavlenie uchastkov poverkhnostnykh gazoproyavleniy i gazovykh vybrosov v Arktike: poluostrov Yamal. [Remote detection of areas of surface gas manifestations and gas emissions in the Arctic: Yamal Peninsula]. Arktika: ekologiya i ekonomika, 2016, no. 3 (23), . 4—15. (In Russian).


Download »


© 2011-2020 Arctic: ecology and economy
DOI 10.25283/2223-4594