Szczegóły publikacji
Opis bibliograficzny
Reservoir parameter classification of a Miocene formation using a fractal approach to well logging, porosimetry and nuclear magnetic resonance / Jadwiga A. JARZYNA, Maria J. BAŁA, Zofia M. MORTIMER, Edyta PUSKARCZYK // Geophysical Prospecting ; ISSN 0016-8025. — 2013 — vol. 61 no. 5, s. 1006–1021. — Bibliogr. s. 1021, Abstr. — Artykuł był prezentowany na 73rd Conference and Exhibition of EAGE incorporating SPE EUROPEC2011, Viena, Austria, 23–26 May, 2011
Autorzy (4)
Słowa kluczowe
Dane bibliometryczne
ID BaDAP | 76542 |
---|---|
Data dodania do BaDAP | 2013-10-07 |
Tekst źródłowy | URL |
DOI | 10.1111/j.1365-2478.2012.01102.x |
Rok publikacji | 2013 |
Typ publikacji | artykuł w czasopiśmie |
Otwarty dostęp | |
Czasopismo/seria | Geophysical Prospecting |
Abstract
A methodology for rock classification is presented that considers lithology and reservoir parameters on the basis of a combined fractal analysis of well logs and mercury porosimetry results with nuclear magnetic resonance outcomes. A sandy-shaly thinly-bedded Miocene gas bearing formation in the Carpathian Foredeep is investigated. Fractal correlation dimensions D-2 calculated for standard logs are used to distinguish sandstone as the most homogeneous lithological group with the highest porosity. The fractal analysis also confirmed observations of gas accumulations in sandstone, shaly sandstone and sandy claystone as rocks of high porosity. The results of two laboratory methods are combined to improve reservoir properties assessment and evaluate movable media in pore space; this technique was based on the similarity of mercury porosimetry results plotted as cumulative intrusion volume versus pressure or pore diameter and also the curves of cumulative porosity and transverse relaxation time distributions using nuclear magnetic resonance. Close values of porosity from logs, recorded in situ and in laboratory measurements, provide the link between fractal analysis and porosimetry and nuclear magnetic resonance measurements.