BROWSE - VOLUME LIST
- A - Physics of the Earth's Interior
- B - Seismology
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C - Geomagnetism
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-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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Browse - Volume list
Wybrane Zagadnienia Geofizycznych Badań w Kopalniach, Lubiatów, 13-18 maja 1991 r. / Selected Geophysical Problems in Mines, Lubiatów, 13-18 May 1991
Author(s):
Volume: 245
Series: M-16
Volume: 245
Series: M-16
Na podstawie analizy sygnałów sejsmicznych 79 wstrząsów górniczych określono współzależność wartości dwóch parametrów ognisk wstrząsów: spadku naprężenia i momentu sejsmicznego, w czterech oddziałach wydobywczych kopalni "Rudna" w Polkowicach. Stwierdzono, że dla wstrząsów usytuowanych w unikalnej dla całego obszaru kopalni "Rudna" synklinie dolomitowej, zależność spadku naprężenia od momentu sejsmicznego okazała się istotnie odmienna niż dla wstrząsów usytuowanych w pozostałych rejonach kopalni. Stwierdzono również, że pomimo znacznego zróżnicowania wartości spadków naprężeń wstrząsów o porównywalnej energii, uśrednione przebiegi spadków naprężeń w funkcji momentu sejsmicznego nazwane tu funkcjami skalowania były w czterech oddziałach wydobywczych kopalni bardzo zbliżone.
Results of Geomagnetic Observations, Arctowski Antarctic Station 1988-1989
Author(s):
Volume: 244
Series: C-44
Volume: 244
Series: C-44
This volume contains the results of observations of the Earth magnetic field for the years 1990 and 1991 carried out at the Polish Antarctic Station Arctowski situated in King George Island (South Shetland Archipelago), In 1986 and 1987 the Arctowski Magnetic Station has been continuing its activity began in 1978.
Results of Geomagnetic Observations, Polish Polar Station, Hornsund, Spitsbergen, 1984-1985
Author(s):
Volume: 243
Series: C-43
Volume: 243
Series: C-43
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 1984 and 1985.
Results of Geomagnetic Observations, Hel Geophysical Observatory 1990
Author(s):
Volume: 242
Series: C-42
Volume: 242
Series: C-42
This volume contains the results of the observations of the Earth magnetic field for the year 1990, carried out at the Geophysical Observatory at Hel near Gdańsk. It is a consecutive 13-th report of similar results published since 1966. A detailed description of the observatory and its history may be found in the Publications of the Institute of Geophysics, Polish Academy of Sciences, C-5 (127).
Results of geomagnetic observations, Hel Geophysical Observatory 1958-1965
Author(s):
Volume: 241
Series: C-41
Volume: 241
Series: C-41
This report is one of a series presenting results of magnetic observations carried out at the Geophysical Observatory at Hel near Gdańsk fot the years 1958-1965. It is a consecutive, 13-th report of the results published since 1966, but its from is different. The tables list the monthly and hourly means and the mean diurnal variation of magnetic elements for each month. The means are given for all days and for international quiet and disturbed days for each month.