Underground storage of oil and gas in salt deposits and other non-hard rocks

1985 ◽  
Vol 22 (3) ◽  
pp. 238-239 ◽  
Author(s):  
H.J. Pincus
1999 ◽  
Vol 35 (1) ◽  
pp. 77-83
Author(s):  
A. V. Mikhalyuk ◽  
V. V. Zakharov ◽  
P. A. Parshukov

1969 ◽  
Vol 26 ◽  
pp. 45-48
Author(s):  
Troels Laier

Groundwater in the Stenlille area is regularly analysed for light hydrocarbons after a natural gas underground storage facility was established there in 1989. The monitoring is carried out by the Geological Survey of Denmark and Greenland and is part of the authorities’ requirements for the environmental approval of the natural gas storage run by the state-owned Danish Oil and Gas company DONG A/S. Groundwater from observation wells and water wells in the area was analysed every month during the first year of operation and four times a year in the following years. More frequent analyses are undertaken on special occasions.


Author(s):  
S. M. Abravets ◽  
I. A. Yashin

Lower Famenian inter-salt deposits (Belarus) have been studied comprehensively. The microlithofacies are as follows: laminated organic-carbonate-silica rock; massive limestone; radiolarite; algal limestone; massive dolomite; porous dolomite; dolomite of indistinct lumpy texture. Rocks contain pores of dissolved radiolarians, cracks of fluid auto-fracturing and weakened zones encountered in the secondary transformations. Rocks of Domanic type in the Central oil area of the Pripyat can be oil-bearing and oil-generating ones.


Neft i gaz ◽  
2020 ◽  
Vol 6 (120) ◽  
pp. 20-34
Author(s):  
О.S. TURKOV ◽  

The Caspian Basin is a unique geological object, the most notable features of which are the anomalously large thickness of the sedimentary cover and its enormous hydrocarbon potential. It is generally known that the main reserves in the identified fields and the prospects for discovering new large deposits of oil, gas and gas condensate here are associated with a subsalt complex of terrigenous and carbonate strata, submerged in the central part of the basin to depths of over 10 km. To date, this complex has been most studied in the edges of the depression at depths of 4-5 km. Confident forecasting of oil prospecting operations for deeper-lying objects is constrained by low researched of their structural, lithological, thermobaric and other parameters. In the debate about these very complex problems, one rarely recalls such a simple and at the same time crucial fact as direct signs of oil and gas potential. Indeed, every year we receive more and more new data on the “breathing of resources”, on the hydrocarbons migration from subsalt sediments into post-salt reservoirs, but we do not give them due attention. The article provides convincing, in the author's opinion, examples of the formation of post-salt deposits on salt domes due to the vertical migration of hydrocarbons. Taking this process into account, recommendations were made both НЕФТЬ И ГАЗ 2020 6 (120) 21 ГЕОЛОГИЯ on the general method of oil prospecting in subsalt deposits, and specific proposals for the search for subsalt and post-salt deposits of oil and gas.


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