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, Polish Polar Station, Hornsund, Spitsbergen, 1992-1993
Author(s): Glegolski W., Gnoiński A.
Volume: 286
Series: C-57
Volume: 286
Series: C-57
This volume contains the results of observations of the Earth's magnetic field carried out at the Polish Polar Station Hornsund in Spitsbergen in the years 1992 and 1993.
Effective Properties of Geomaterials: Rocks and Porous Media
Author(s): Bielski W., Telega J.
Volume: 285
Series: A-26
Volume: 285
Series: A-26
This comprehensive survey consists of two parts. In Part I we present the available results concerning the effective properties of cracked materials, mainly rocks. The second part of the paper deals with the transport and effective properties of porous materials in the case of a rigid and deformable skeleton. The whole paper is oriented towards applications in geophysics and geomechanics. Thus, much attention has been devoted to two-phased media, which model the upper crust of the Earth. Such media may be either isotropic or anisotropic cracked elastic bodies, though their behaviour can also exhibit inelastic features. Porous media may be dry, saturated or partially saturated. One-phase and multi-phase flows through porous media have been considered.
Earthquakes in the Hornsund Region, Spitsbergen 1994-2000 and Seismological Bulletin, Arctowski Antarctic Station 1992-1995
Author(s): Górski M.
Volume: 284
Series: B-18
Volume: 284
Series: B-18
The data of earthquakes in the Hornsund region, recorded at the Hornsund station from January 1994 until April 2000, have been analysed. Scaling relations (seismic moment vs. source radius and energy vs. seismic moment) are presented. The results were compared with analogous relations for other series of seismic events, in particular those in coal and copper mines. A comparison of scaling relations for three earthquake series singled out in the Hornsund region has been made.
Seismological Bulletin 1989-1990. Local Earthquakes Recorded by Polish Seismological Stations
Author(s):
Volume: 283
Series: B-17
Volume: 283
Series: B-17
This bulletin contains a list of mining-induced quakes recorded in 1989-1990 by the Polish seismological network. From the following regions: Upper Silesian Coal Basin and Rybnik Coal District as well as Lubin Copper Basin.
Seismological Bulletin 1987/1988. Local Earthquakes Recorded by Polish Seismological Stations
Author(s):
Volume: 282
Series: B-16
Volume: 282
Series: B-16
This bulletin contains a list of local earthquakes recorded in 1987-1988 by the Polish seismological network. The bulletin consists of two parts. The first part contains major events from the Upper Silesian Coal Basin and the Rybnik Coal District and the second part contains seismic events from the Lubin Copper Basin.