Poradnik górnika naftowego: Geofizyka naftowa. Geofizyka poszukiwawcza. Geofizyka wiertnicza. T. 1 B. Cz. 1. Cz. 2. Front Cover. Anna Bieda. Stowarzyszenie. Phone, Suggest a phone number AGH, WGGIOS, Geofizyka poszukiwawcza. College Posts about AGH, WGGIOS, Geofizyka poszukiwawcza. There are no. Kilka uwag o interpretacji materiało ́w sejsmicznych w czesci srodkowej i zachodniej przedgo ́rza Karpat (in Polish): Geofizyka Poszukiwawcza i Wiertnicza, v.
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You have to log in to notify your friend by e-mail Login or register account. Like other foreland basins, the Carpathian Foredeep is asymmetric and filled with predominantly clastic sediments of the Miocene age as much as 3 and 6 km 1.
A respectful treatment of one another is important to us. High percentage of grainstones microfacies samples was detected in the analyzed population of the Main Dolomite.
Assign to other user Search user Invite. It also gives information about the physical properties of rock. If the error persists, contact the administrator by writing to support infona. Citing Books via Google Scholar.
The impact of storms on water column resulted in intermittent rises of oxygen content in the otherwise anoxic to dysoxic near-bottom conditions. R Observatories Orlov, A. Kurs geofizicheskikh metodov razvedki neftianykh mestorozhdenii Book 1 edition published in in Russian and held by 1 WorldCat member library worldwide.
Librarian Administrator Sign In. The molasse geofizgka of the Carpathian Foredeep are underlain by the basement of the European Platform, covered mainly by Permian-Mesozoic terrestrial and shelf sediments and locally by the Paleogene deposits.
V Sorokin Book 3 editions published in in Polish and held by 5 WorldCat member libraries worldwide. Volume 31 Issue 4 Decpp. This interval is capped with a Ludlow calcite-cemented, laminated siltstone that forms a regional correlation marker and shows soft-sediment deformations attributable to gravitational collapse on a NE-dippingpaleoslope.
The early to middle Miocene Carpathian Foredeep developed as a peripheral foreland basin related to the moving Carpathian front. You do not currently have access to this article.
Kierunki studiów na Uniwersytecie Warszawskim
The portal can access those files and use them to remember the user’s data, such as their chosen settings screen view, interface language, etc. This volume of 30 chapters authored by geologists and geophysicists from Austria, Czech Republic, Hungary, Poland, Romania, Slovakia, Ukraine, United Kingdom, and the USA provides a comprehensive and understandable account of geology and hydrocarbon resources of the entire Carpathian system from northeastern Austria to southern Romania, including the Neogene foredeep, the foreland platform both in front and beneath the thrust belt, the Carpathian thrust belt, and the late and post orogenic intermontane basins.
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Therefore, it could be assumed that the parameters analysis on the entire set of data were representative in terms of reservoir properties for the samples belonging to the grainstones microfacies. About the article Published Online: It was found that grainstones were characterized by the best reservoir parameters. Volume 32 Issue 4 Decpp. V Sorokin Book 2 editions geofizyma between and in Russian and Undetermined and held by 6 WorldCat member libraries worldwide.
Change font size You can adjust the font size by pressing a combination of keys: Radio-frequency capacitively-coupled plasma generators: The employment of modern and advanced equipment enables to effectively determine deposit borders and depth.
Seventeen chapters of Memoir 84 have been printed in full. Przyokopowa 31, Warszawa.
High contrast On Off. See all formats and pricing Online. Laboratory measurements results, especially mercury porosimetry, extended considerably information about poszukiwswcza reservoir rock the Main Dolomite and contributed to the separation of diverse microfacies and paleogeographic zones.
Prices do not include postage and handling if applicable. V Sorokin in Chinese and held by 1 WorldCat member library worldwide. FMI based structural geology and geomechanics. However, the geochemical signature of the mudrocks is consistent with a cratonic rather than orogenic sourcing, the proximal part of the foredeep basin-fill is apparently missing, and the shale succession juxtaposes in part across the Teisseyre-Tornquist Zone against suspected ter- ranes with no evidence of Silurian tectonism.