Sedimentological sand grain orientation in oil-producing U1 layer Kazan oil-gas-condensate field (Tomsk Oblast)

Detaylı Bibliyografya
Parent link:IOP Conference Series: Earth and Environmental Science
Vol. 33 : Contemporary Issues of Hydrogeology, Engineering Geology and Hydrogeoecology in Eurasia.— 2016.— [012050, 4 p.]
Yazar: Krasnoshchekova L. A. Lubov Afanasievna
Müşterek Yazar: Национальный исследовательский Томский политехнический университет (ТПУ) Институт природных ресурсов (ИПР) Кафедра гидрогеологии, инженерной геологии и гидрогеоэкологии (ГИГЭ)
Diğer Yazarlar: Cherdansteva D., Vologdina I.
Özet:Title screen
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.
Dil:İngilizce
Baskı/Yayın Bilgisi: 2016
Seri Bilgileri:Geology, Hydrogeology and Engineering Geology
Konular:
Online Erişim:http://dx.doi.org/10.1088/1755-1315/33/1/012050
http://earchive.tpu.ru/handle/11683/34006
Materyal Türü: Elektronik Kitap Bölümü
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=649510
Diğer Bilgiler
Özet:Title screen
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.
DOI:10.1088/1755-1315/33/1/012050