1887
PDF

Abstract

Bitumen fields feature a complicated mechanism by which reservoirs are formed. Of most interest are bed and lenticular-bed reservoirs sited at depths down to 400 m, since the largest bitumen reserves are related to those reservoirs. The confinement of such reservoirs to shallow water sediments of the lagoon and bar types defines the specific features of reservoir-beds interlayer texture, varied thickness of reservoirs up to wedging out. By and large such reservoirs are characterized by the occurrence of gas accumulations, bitumen viscosity varying in depth and extension, alteration of various bitumen-saterated interlayers and bitumen- ree and water-saturated ones.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201409748
1995-05-29
2024-03-28
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409748
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