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-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
Wybrane Zagadnienia Geofizycznych Badań w Kopalniach, Radków, 5-10 czerwca 1989 r. / Some Geophysical Problems in Mines, Radków, 5-10 June 1989
Author(s):
Volume: 235
Series: M-15
Volume: 235
Series: M-15
W pracy przedstawiono wyniki badań mikrograwimetrycznych mających na celu wykrycie efektów procesu sufozji, rozwijającego się w podłożu budowlanym dużego zakładu przemysłowego, usytuowanego na polu górniczym kopalni węgla kamiennego "Sosnowiec". Przyczyną sufozji było w tym przypadku natrafienie na nieznany uskok podczas prac górniczych prowadzonych na głębokości około 100 m pod powierzchnią terenu. Uskok ten spowodował wzmożony wypływ wody, powodujący powstanie niecki osiadania powierzchni terenu i w następstwie powstania zapadliska w jej centrum. Pojawiły się szkody w budynkach przemysłowych i torowiskach wewnętrznych linii kolejowych.
Bibliography 1979-1988 and Activity Report for the 35-year Anniversary
Author(s):
Volume: 232
Series: M-14
Volume: 232
Series: M-14
The third volume of bibliography covers publications written by staff of the Institute of Geophysics in the years 1979-1988. It is also a jubilee issue as it commemorates the 35-year period of the publishing activity of the Institute.
Mechanizm Ognisk Wstrząsów Górniczych / The Mechanism of Seismic Events Induced by Mining
Author(s): Gibowicz S.
Volume: 221
Series: M-13
Volume: 221
Series: M-13
This is a Polish translation of the review prepared as an invited paper to lead Session 1 of the Second International Symposium on Rockbursts and Seismicity in Mines, held from June 8 to June 10, 1988, at the University of Minnesota, Minneapolis, USA. An English version is being published in USA in the Symposium Proceedings. The review attempts to synthesize methods and results of recent studies on the source mechanism of seismic events induced by mining and relevant microearthquakes of volcanic and tectonic origin.
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.