BROWSE - VOLUME LIST
- A - Physics of the Earth's Interior
- B - Seismology
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C - Geomagnetism
C-119, C-118, C-117, C-116, C-115, C-114, C-113, C-112, C-111, C-110, C-109, C-108, C-107, C-106, C-105, C-104, C-103, C-102, C-101, C-100, C-99, C-98, C-97, C-96, C-95, C-94, C-93, C-92, C-91, C-90, C-89, C-88, C-87, C-86, C-85, C-84, C-83, C-82, C-81, C-80, C-79, C-78, C-77, C-76, C-75, C-74, C-73, C-72, C-71, C-70, C-69, C-68, C-67, C-66, C-65, C-64, C-63, C-62, C-61, C-60, C-59, C-58, C-57, C-56, C-55, C-54, C-53, C-52, C-51, C-50, C-49, C-48, C-47, C-46, C-45, C-44, C-43, C-42, C-41, C-40, C-39, C-38, C-37, C-36, C-35, C-33, C-32, C-31, C-30, C-29, C-28, C-27, C-26, C-25, C-24, C-23, C-22, C-21, C-20, C-19, C-18, C-17, C-16, C-15, C-14, C-13, C-12, C-11, C-10, C-9, C-8, C-7, C-6, C-5, C-4, C-3, C-2, C-1
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D - Physics of the Atmosphere
D-79, D-78, D-77, D-76, D-75, D-74, D-73, D-72, D-71, D-70, D-69, D-68, D-67, D-66, D-65, D-64, D-63, D-62, D-61, D-60, D-59, D-58, D-57, D-56, D-55, D-54, D-53, D-52, D-51, D-50, D-49, D-48, D-47, D-46, D-44, D-45, D-43, D-42, D-41, D-40, D-39, D-38, D-37, D-35, D-34, D-33, D-32, D-31, D-30, D-28, D-27, D-26, D-25, D-24, D-23, D-22, D-21, D-20, D-19, D-18, D-17, D-16, D-15, D-14, D-13, D-12, D-11, D-10, D-9, D-8, D-7, D-6, D-5, D-4, D-3, D-2, D-1
- E - Hydrology
- P - Polar Research
- M - Miscellanea
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Online First
Browse - Volume list
Results of Geomagnetic Observations, Belsk Geophysical Observatory 2004
Author(s): Marianiuk J., Neska M., Reda J.
Volume: 379
Series: C-92
Volume: 379
Series: C-92
This publication contains results of geomagnetic observations performed in 2004; it is a consecutive, thirty-ninth issue in the series of yearbooks listing observations of the natural magnetic field of the Earth at the Central Geophysical Observatory at Belsk.
Water Domain Structure and Effects of Water Content on Electric Properties of Rocks Studied in a Wide Frequency Range
Author(s): Rusiniak L.
Volume: 378
Series: A-28
Volume: 378
Series: A-28
Water is one of the most common substances, widespread on the Earth in different states of matter. It has an essential influence on many climatic and atmospheric phenomena. In the Earth's crust, water influences mechanical and electrical behaviour of various structures. The electric properties of moist porous rocks are very important in many branches of geophysics. The moist porous rock material is very interesting from physical point of view, as it is a solid dielectric with a liquid dipole dielectric in the pores, cracks and other structural defects. There are good prospects of practical use of the results of measurements of electric properties of such rocks in non-destructive testing and in the study of water inside various products and materials.
Potential Climate Changes and Sustainable Water Management
Editor(s): Liszewska M.
Volume: 377
Series: E-4
Volume: 377
Series: E-4
In recent years it has become obvious that operational use of natural resources assuming their stationarity represents too narrow view of this complex issue. A change of paradigm seems to be developing, the two main principles of which are: the increased role of geo-sciences in assessing non-stationarity of resources potential, and postulate for their sustainable exploitation in the face of global change. Sustainability criteria provide a framework for prioritising competing interests and for making decision about safe and stable use of resources.
Local Earthquakes Recorded by Polish Seismological Stations 2003
Author(s): Zuchniak M., Niewiadomski J., Guterch B.
Volume: 376
Series: B-37
Volume: 376
Series: B-37
The majority of seismic events recorded in Poland are caused by mining activity in the Upper Silesian Coal Basin and Lubin Copper Basin. Induced seismicity is observed less frequently in the Rybnik Coal District and Bełchatów Open-Pit Mining Area. In 2003, a few local tectonic earthquakes occurred in the Western Carpathians at distances up to about 30 km from station Niedzica.
Seismological Bulletin 2002. Local Earthquakes Recorded by Polish Seismological Stations
Author(s): Draber D., Niewiadomski J., Zuchniak M.
Volume: 375
Series: B-36
Volume: 375
Series: B-36
The majority of seismic events recorded in Poland are caused by mining activity in the Upper Silesian Coal Basin and Lubin Copper Basin. Induced seismicity is observed less frequently in the Rybnik Coal District and Belchatów Open-Pit Mining area. In 2002, a few local tectonic earthquakes occurred in the Western Carparhians at distances up to about 30 km from station Niedzica.