Abstract
Geological information on the Eldarovsky field, situated in the central part of Tersky anticlinal zone and discovered in 1964, is given. Commercial quantities of oil were discovered in the foraminifera (thickness 40 to 70 m) and Upper Cretaceous (305 to 330 m thickness) deposits, consisting of fissured limestones and marls. Both the foraminifera and Upper Cretaceous deposits are divided into various zones which are hydrodynamically connected with each other and constitute a single pool. No hydrodynamical connection was observed between the Eldarovsky pools and surrounding oil fields. The secondary porosity of the Upper Cretaceous and forammifera deposits is 0.49% and 0.2%, respectively, and is responsible for most of the oil reserves. The analysis of the pressure buildup curves shows that the field has an elastic water drive.
Citation Formats
Lebedinets, N P, Merkulov, A V, Pristanskii, G T, and Postash, M F.
Results of the study of a new Groznensky Field with fissured reservoir rocks.
USSR: N. p.,
1970.
Web.
Lebedinets, N P, Merkulov, A V, Pristanskii, G T, & Postash, M F.
Results of the study of a new Groznensky Field with fissured reservoir rocks.
USSR.
Lebedinets, N P, Merkulov, A V, Pristanskii, G T, and Postash, M F.
1970.
"Results of the study of a new Groznensky Field with fissured reservoir rocks."
USSR.
@misc{etde_5541304,
title = {Results of the study of a new Groznensky Field with fissured reservoir rocks}
author = {Lebedinets, N P, Merkulov, A V, Pristanskii, G T, and Postash, M F}
abstractNote = {Geological information on the Eldarovsky field, situated in the central part of Tersky anticlinal zone and discovered in 1964, is given. Commercial quantities of oil were discovered in the foraminifera (thickness 40 to 70 m) and Upper Cretaceous (305 to 330 m thickness) deposits, consisting of fissured limestones and marls. Both the foraminifera and Upper Cretaceous deposits are divided into various zones which are hydrodynamically connected with each other and constitute a single pool. No hydrodynamical connection was observed between the Eldarovsky pools and surrounding oil fields. The secondary porosity of the Upper Cretaceous and forammifera deposits is 0.49% and 0.2%, respectively, and is responsible for most of the oil reserves. The analysis of the pressure buildup curves shows that the field has an elastic water drive.}
journal = []
volume = {6}
journal type = {AC}
place = {USSR}
year = {1970}
month = {Jun}
}
title = {Results of the study of a new Groznensky Field with fissured reservoir rocks}
author = {Lebedinets, N P, Merkulov, A V, Pristanskii, G T, and Postash, M F}
abstractNote = {Geological information on the Eldarovsky field, situated in the central part of Tersky anticlinal zone and discovered in 1964, is given. Commercial quantities of oil were discovered in the foraminifera (thickness 40 to 70 m) and Upper Cretaceous (305 to 330 m thickness) deposits, consisting of fissured limestones and marls. Both the foraminifera and Upper Cretaceous deposits are divided into various zones which are hydrodynamically connected with each other and constitute a single pool. No hydrodynamical connection was observed between the Eldarovsky pools and surrounding oil fields. The secondary porosity of the Upper Cretaceous and forammifera deposits is 0.49% and 0.2%, respectively, and is responsible for most of the oil reserves. The analysis of the pressure buildup curves shows that the field has an elastic water drive.}
journal = []
volume = {6}
journal type = {AC}
place = {USSR}
year = {1970}
month = {Jun}
}