BADANIA FRAKCJI CIĘŻKICH W ŚWIETLE ODBITYM
Journal Title: Biuletyn Państwowego Instytutu Geologicznego - Year 2010, Vol 439, Issue 439
Abstract
Badaniom mineralogicznym poddano 12 próbek okruchowych pobranych z różnych miejsc i środowisk geologicznych. Badania potwierdziły konieczność wykorzystania metod mineralogicznych i rentgenostrukturalnych do jednoznacznej identyfikacji urozmaiconego składu frakcji ciężkich. Kompleksowa analiza mineralogiczna próbek wykazała obecność materiału frakcji ciężkiej z różnych typów skał i pozwoliła na określenie przypuszczalnego Ľródła minerałów kruszcowych.
Authors and Affiliations
Adam PIESTRZYŃSKI, Jacek RUTKOWSKI
Evaluation of exploitation possibilities of the Bełchatów – Kamieńsk field lignite deposit
In view of the shrinking reserves of the Bełchatów lignite deposit in the currently exploited Bełchatów and Szczerców fields, the prolongation of the Bełchatów power plant activity, producing about 20% of Polish electric...
DEVONIAN CARBONATE SUCCESSION IN THE TROJANOWICE 2 BOREHOLE
The Devonian carbonate succession was examined in the Trojanowice 2 borehole located northwest of Kraków. It is represented by dolomites with infrequent intrastratal breccias and a micrite limestone layer. The dolomites...
Estimation of sampler influence on uncertainty associated with sampling in groundwater monitoring
According to European Union directives (RDW, 2000; DWP, 2006) the identification and determination of uncertainty – also this associated with sampling, preservation and transport of samples – is an important part of the...
Characteristic of coaly shale aggregate and its application for the road construction
The waste obtained directly from exploitation of coal and/or from storage is the subject of the paper. The purpose is to describe the properties such material called in this paper the coaly shale aggregate and their appl...
RIVER VALLEYS AND ICE-MARGINAL VALLEYS AS SEPARATE AQUIFER SYSTEMS IN HYDROGEOLOGICAL STUDIES
River valleys, ice–marginal valleys indicate clear hydrostructural, hydrodynamic and water qualitative separateness in relation to the hydrogeological units within the adjacent uplands. They are distinguished by strong r...