BROWSE - VOLUME LIST
- A - Physics of the Earth's Interior
- B - Seismology
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C - Geomagnetism
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-34, 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-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-36, D-35, D-34, D-33, D-32, D-31, D-30, D-29, 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
M - Miscellanea
Naprężenia we Wnętrzu Ziemi. Stresses in the Earth s Interior
Author(s): Teisseyre R.
Volume: 216
Series: M-12
Volume: 216
Series: M-12
Stresses in the Earth's interior are a direct cause for all dynamic processes within the Earth. In this monographic paper, they are analyzed in terms of their relation to motoric forces mechanisms on the one hand, and various geophysical fields and field anomalies on the other. Some regional or even local relationships have been examined too.
Wykorzystanie Efektu Emisji Sejsmoakustycznej w Geotechnice. Geotechnical Applications of Seismoacoustic Emission
Author(s): Zuberek W.
Volume: 214
Series: M-11
Volume: 214
Series: M-11
Seismoacoustic (called also acoustic or geoacoustic) emission is generated in rocks as a result of various dynamic processes of deformation and fracturing. These processes are accompanied by sudden elastic energy release, and elastic waves are emitted from the source. The main purpose of this work was to explain the seismoacoustic phenomena from physical point of view, basing on the synthesis of observations which have been made until now.
Wybrane Zagadnienia Geofizycznych Badań w Kopalniach, Lubiatów, 18-22.05.1987 r. *** Some Geophysical Problems in Mines
Author(s):
Volume: 213
Series: M-10
Volume: 213
Series: M-10
A consecutive volume of publications related t mining geophysics, mainly to method of mine tremors studies, contains papers presented during the XVII Polish-Czechoslovakian Symposium at Lubiatów. Additionally a few papers are included, which have not been presented during the Symposium but are closely related to the topics of interest.
Teoria Dużych Dynamicznych Odkształceń Górotworu
Author(s): Majewski E.
Volume: 201
Series: M-9
Volume: 201
Series: M-9
The paper deals with an application of nonlinear theory of a elasto-viscoplastic deformations to describing deformation processes occurring in a rock body at the presence of dynamic loadings.
Wybrane Zagadnienia Geofizycznych Badań w Kopalniach, Jastarnia, 6-10 V 1985 *** Some Geophysical Problems in Mines
Author(s):
Volume: 191
Series: M-8
Volume: 191
Series: M-8
It is found that, according to theoretical analysis supported by laboratory tests and by field observations in mine regions, the complex model of mine tremors and rockbursts shall be introduced. There are numerous observations of rockbursts of evident implosive character, in such a way that shear movement and implosion are related each to other. However, a part of shear movements may be slow, precursor to the implosive events.