Scholarly record
POROSITY VARIATIONS OF THE MAIN DOLOMITE ROCKS IN THE P-1 WELL (W POLAND) IN THE SCOPE OF LOW-FIELD NMR
Abstract
The Zechstein Main Dolomite (Ca2) is one of the largest petroleum bearing formations in Poland. Numerous hydrocarbon deposits occur within Ca2 in the carbonate platform sediments of the Polish part of the Southern Permian Basin. Application of modern methods allows evaluation of porosity and pore size distribution and enhances the proper characterization of reservoir rocks in non-invasive way. The study concerns lowfield Nuclear Magnetic Resonance (NMR) measurements conducted on Ca2 carbonate rocks from P-1 well located in Gorzow Block (W Poland). In order to evaluate different types of porosity and pore size distribution variability, The Carr-Purcell-Meiboom-Gill sequence (T2CPMG) experiments were carried out on 25 cylindrical core samples collected from the depth interval of 2630.5пїЅ2677.2 meters. Observations of thin sections made with polarized light microscopy provided a detailed petrographic characterization of samples. Results illustrate the porosity - depth trend and reveal the information about sedimentation environment-related porosity changes.
Publication Impact Profile
- Captures
- Mendeley - Readers: 4
Publication details
References0
Structured references will appear here after the reference import pass. The count is preserved now so the scholarly record is not incomplete.
View or Download full articleAccess options
SWS access login
Login as SWS Scientific CommitteeLogin as SWS Scientific PartnerLogin as SWS AuthorAuthors and approved SWS contributors will read and export their own linked papers after identity matching by SWS profile, email and SGEM GlobalID.
For librarian assistance: [email protected]
Purchase Instant Access
- Article can be downloaded after successful payment.
- Article may be used according to SWS library access terms.
- Article cannot be redistributed.