Abstract
The paper describes the results in identifying the prevalent directions of elongated quartz grains being the major oil-producing layer component in sand reservoirs. Studying the orientation of quartz to its grain shapes in paleogeographical oriented core samples made it possible to identify the hydrodynamic reservoir regimes and facies type. The spatial confinement of pore spaces and cataclasis fractures in grain material to the prevalent elongated quartz grain directions was defined.
| Original language | English |
|---|---|
| Article number | 012050 |
| Journal | IOP Conference Series: Earth and Environmental Science |
| Volume | 33 |
| Issue number | 1 |
| DOIs | |
| Publication status | Published - 15 Apr 2016 |
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ASJC Scopus subject areas
- Environmental Science(all)
- Earth and Planetary Sciences(all)
Cite this
Sedimentological sand grain orientation in oil-producing U1 layer Kazan oil-gas-condensate field (Tomsk Oblast). / Krasnoshchekova, L.; Cherdansteva, D.; Vologdina, I.
In: IOP Conference Series: Earth and Environmental Science, Vol. 33, No. 1, 012050, 15.04.2016.Research output: Contribution to journal › Article
}
TY - JOUR
T1 - Sedimentological sand grain orientation in oil-producing U1 layer Kazan oil-gas-condensate field (Tomsk Oblast)
AU - Krasnoshchekova, L.
AU - Cherdansteva, D.
AU - Vologdina, I.
PY - 2016/4/15
Y1 - 2016/4/15
N2 - The paper describes the results in identifying the prevalent directions of elongated quartz grains being the major oil-producing layer component in sand reservoirs. Studying the orientation of quartz to its grain shapes in paleogeographical oriented core samples made it possible to identify the hydrodynamic reservoir regimes and facies type. The spatial confinement of pore spaces and cataclasis fractures in grain material to the prevalent elongated quartz grain directions was defined.
AB - The paper describes the results in identifying the prevalent directions of elongated quartz grains being the major oil-producing layer component in sand reservoirs. Studying the orientation of quartz to its grain shapes in paleogeographical oriented core samples made it possible to identify the hydrodynamic reservoir regimes and facies type. The spatial confinement of pore spaces and cataclasis fractures in grain material to the prevalent elongated quartz grain directions was defined.
UR - http://www.scopus.com/inward/record.url?scp=84971426897&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=84971426897&partnerID=8YFLogxK
U2 - 10.1088/1755-1315/33/1/012050
DO - 10.1088/1755-1315/33/1/012050
M3 - Article
AN - SCOPUS:84971426897
VL - 33
JO - IOP Conference Series: Earth and Environmental Science
JF - IOP Conference Series: Earth and Environmental Science
SN - 1755-1307
IS - 1
M1 - 012050
ER -