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1
Content available remote Badania geologiczne Jeana-Etienne Guettarda w Rzeczypospolitej (1760-1762)
Tarkowski R., Daszkiewicz P.
Przegląd Górniczy
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2010
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T. 66, nr 1-2
63-68
PL
Przedstawiono wyniki badań geologicznych francuskiego przyrodnika J.-E. Guettarda (1715-1786) przeprowadzonych w Polsce w latach 1760-1762. Jest on autorem jednego z pierwszych opisów geologii wraz z pierwszą mapą geologiczną Rzeczypospolitej, opisu kopalni soli w Wieliczce, pierwszych ilustracji skamieniałości i innych. Guettard był jednym z najlepszych znawców geologii Polski w XVIII w., a jego monografie są pionierską próbą analizy głównych elementów geologicznych obszaru Polski. Jego prace geologiczne wywarły znaczący wpływ na późniejsze badania geologiczne w Polsce. Rozważania Guettarda z kopalni soli w Wieliczce umożliwiły mu wyciągnięcie wniosków dotyczących tworzenia się złóż soli kamiennej, jak również podjęcie próby opracowania metod poszukiwań nowych złóż soli kamiennej na innych obszarach.
EN
The results of geologic research of French naturalist J.E. Guetard (1715-1786) carried out in Poland in the years 1760-1786 are presented. He is the author of the early descriptions of geology together with geologic map of the Republic, description of salt mine at Wieliczka, first illustrations of fossils and others. Guettard was one of the best experts on geology of Poland in 18th century, and his monographs pioneer attempt of analysis of main geologic elements of Polish territory. His geologic works had the significant on the later geological research in Poland. Guettard.s considerations about the salt mine at Wieliczka enabled him to draw conclusions referring to rock-salt deposits formation as well as to take up attempts to work out the methods of new rock-salt deposits exploration on other territories.
2
Content available remote Wstępny podział geologiczno-inżynierski dna polskiej części Morza Bałtyckiego
Kaszubowski L. J., Coufal R.
Inżynieria Morska i Geotechnika
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2010
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nr 3
392-401
PL
Jednostki geologiczno-inżynierskie dna polskiej części Morza Bałtyckiego na podstawie szczegółowej analizy map geologicznych dna Bałtyku oraz geologicznej interpretacji materiałów sejsmoakustycznych. Przypisane poszczególnym jednostkom geologiczno-inżynierskim określone kryteria geologiczne i charakterystyczne parametry geotechniczne.
EN
Geological units of Polish part of the Baltic seabed based on detailed analysis of geological maps and geological interpretation of seismic-acoustic investigations. Determination of characteristic geological criteria and geotechnical parameters for the designated geological units.
3
Content available remote Współczesne pionowe ruchy skorupy ziemskiej na obszarze Bałtyku południowego
Kaszubowski L. J.
Inżynieria Morska i Geotechnika
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2010
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nr 3
406-409
PL
Zagadnienie współczesnych ruchów pionowych skorupy ziemskiej na obszarze południowego Bałtyku. Mapa sumarycznych ruchów pionowych na analizowanym obszarze w ciągu ostatnich 8000 lat.
EN
Problems of current vertical movements of the Earth’s crust in Southern Baltic region. Map of vertical movements during last 8000 years.
4
Content available remote Jednostki sejsmostratygraficzne Mierzei Dziwnowskiej
Kaszubowski L. J.
Inżynieria Morska i Geotechnika
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2010
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nr 3
387-392
PL
Wydzielenie szeregu jednostek sejsmostratygraficznych plejstocenu i holocenu na podstawie przeprowadzonych badań geologicznych i sejsmicznych w rejonie Mierzei Dziwnowskiej. Charakterystyka poszczególnych jednostek sejsmostratrygraficznych. Występowanie ruchów neotektonicznych.
EN
Identification of the series of Pleistocene and Holocene seismic-stratigraphic units based on geological and seismic investigations made in the Dziwnów Spit region. Description of particular seismic-stratigraphic units. Presence of neotectonic movements.
5
Content available remote Geodetic and geologic research of recent tectonic activity in Dinarides
Pribicevic B., Medak D., Prelogovic E.
Reports on Geodesy
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2006
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z. 4/79
173-180
EN
Initial tectonic movements of Adriatic Microplate result in dominating compression in the area of Dinarides. Collected structural data, compared with surface and depth data, with seismological and geodetic measurements taken in the account enabled the classifications of structures. Deformations and movements of structures directly depend on the stress orientation. This orientation varies from between 340-160° to 30-210°. In order to visualize the stress orientation, formation of different types of structures and their movements, examples of compressional structures are shown, as well as rotations of structures and conditions of creation of extensional structures. Finally, the map with fault zones is included, too. The data show narrowing of the area of Adriatic Microplate and the existence of its southern and northern part. Both parts are changing movement directions, leading to more tectonic activity. In active areas, formation of structures is recognized, and causality with fault locations and seismic activity is established. The amplitudes of tectonic movements derived from geodetic measurements between 1994 and 1998 represent important contribution for better understanding the tectonic activities in the area.
6
Content available remote Geodetic and geologic research of recent tectonic activity in Dinarides
Pribičević B., Medak D., Prelogović E.
Reports on Geodesy
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2004
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nr 2/69
125--131
EN
Initial tectonic movements of Adriatic Microplate result in dominating compression in the area ofDinarides. Collected structural data, compared with surface and depth data, with seismological and geodetic measurements taken in the account enabled the classifications of structures. Deformations and movements of structures directly depend on the stress orientation. This orientation varies from between 340-160° to 30-210°. In order to visualize the stress orientation, formation of different types of structures and their movements, examples of compressional structures are shown, as well as rotations of structures and conditions of creation of extensional structures. Finally, the map with fault zones is included, too. The data show narrowing of the area of Adriatic Microplate and the existence of its southern and northern part. Both parts are changing movement directions, leading to more tectonic activity. In active areas, formation of structures is recognised, and causality with fault locations and seismic activity is established. The amplitudes of tectonic movements derived from geodetic measurements between 1994 and 1998 represent important contribution for better understanding the tectonic activities in the area.
7
Content available remote Geodetic and geologic research of recent tectonic activity Dinarides
Pribičević B., Medak D., Prelogović E.
Reports on Geodesy
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2004
|
nr 4/71
125--131
EN
Initial tectonic movements of Adriatic Microplate result in dominating compression in the area of Dinarides. Collected structural data, compared with surface and depth data, with seismological and geodetic measurements taken in the account enabled the classifications of structures. Deformations and movements of structures directly depend on the stress orientation. This orientation varies from between 340-160° to 30-210°. In order to visualize the stress orientation, formation of different types of structures and their movements, examples of compressional structures are shown, as well as rotations of structures and conditions of creation of extensional structures. Finally, the map with fault zones is included, too. The data show narrowing of the area of Adriatic Microplate and the existence of its southern and northern part. Both parts are changing movement directions, leading to more tectonic activity. In active areas, formation of structures is recognized, and causality with fault locations and seismic activity is established. The amplitudes of tectonic movements derived from geodetic measurements between 1994 and 1998 represent important contribution for better understanding the tectonic activities in the area.
8
Content available remote Geologiczne uwarunkowania optymalizacji składowania odpadów
Drągowski A.
Przegląd Geologiczny
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2002
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Vol. 50, nr 10/2
953-958
EN
The paper presents basic problems of research and evaluation of geologic conditions, which are essential for optimization of municipal and industrial (non-municipal) waste storage sites. The topic was analyzed in context of the new legal regulations, and the new draft of the Ministry of the Environment regulation on the issue of dumps, using the author's own large research experience, and data from the literature on the subject and from archive materials. Special attention was paid to the issue of geologic conditions of prospective dumping sites localization, to mineral isolation barriers, to the research scope and techniques for wet dumps (deposit ponds) and dumping grounds, geologic inspection during exploitation, monitoring, liquidation and dump area recultivation.
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