Szczegóły publikacji
Opis bibliograficzny
3D modellling, as a tool of spatial representation of Miocene clastic reservoir of natural gas : case study: Husow-Nienadowa area, the Carpathian Foredeep, Poland / Bartosz PAPIERNIK, Magdalena KRZYSZTOFIK, Grzegorz MACHOWSKI, Michał Cierzniak // W: SGEM 2016 : 16th international multidisciplinary scientific geoconference : science and technologies in geology, exploration and mining : 30 June – 6 July, 2016, Albena, Bulgaria : conference proceedings. Vol. 4, Oil and gas exploration. — Sofia : STEF92 Technology Ltd., cop. 2016. — (International Multidisciplinary Scientific GeoConference SGEM ; ISSN 1314-2704). — Na okł. dod.: Book 1. — Na str. tyt. inne miejsce i data odbycia konferencji: 2-5 November 2016, Vienna, Austria. — ISBN: 978-619-7105-80-3. — S. 11–18. — Bibliogr. s. 18, Abstr.
Autorzy (4)
Słowa kluczowe
Dane bibliometryczne
| ID BaDAP | 102316 |
|---|---|
| Data dodania do BaDAP | 2016-12-17 |
| Rok publikacji | 2016 |
| Typ publikacji | materiały konferencyjne (aut.) |
| Otwarty dostęp |  |
| Konferencja | 16th international multidisciplinary scientific geoconference |
| Czasopismo/seria | International Multidisciplinary Scientific GeoConference SGEM |
Abstract
3D structural and parametric test model was created in aim to perform quantitative analysis of conventional and unconventional reservoirs variability and quality in the area Husow-Nienadowa (eastern part of Polish Carpathian Foredeep). The input parameters for the model include interpreted 2D seismic lines (ca 65 km), well data, comprising stratigraphy and geophysical logs (lithological composition, petrophysical parameters) as well as structural and thickness maps of 5 main stratigraphic horizons and 8 structural cross sections. The result of completed work is the structural model covering area of approximately 360 km(2). The area is located close to Husow and Raczyna gas fields which are present in this zone. Structural framework of the model is divided into 5 geological complexes located between Miocene basement and Carpathian overthrust surface. Miocene interval has been divided into major stratigraphic complexes: Lower Badenian (sub evaporitic), Evaporitic complex, Upper Badenian and Sarmatian. Vertical resolution of the model is moderate resulting in approximately 14,4 min 3D cells. Parametric modelling comprised shale volume (VSH) and porosity (PHI) models which were used as an input for development of the discrete "pseudo-facies" model with an implication of neural net Train Estimation tool of Petrel software package. As a result, a preliminary model was developed for the 5 "pseudo-facies", indicating spatial distribution of prospective conventional and unconventional reservoirs.
