BROWSE - VOLUME LIST
- A - Physics of the Earth's Interior
- B - Seismology
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C - Geomagnetism
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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Browse - Volume list
Modelling of Crack Induced Resistivity Changes - Applications to Earthquake Studies
Author(s): Teisseyre K.
Volume: 274
Series: A-24
Volume: 274
Series: A-24
An anisotropic resistivity model of rocks that contain spatially oriented crack systems is presented. Each system consists of open cracks filled in with material of different resistivity than that of the rock frame; the cracks in the system have the same orientation and shape. Generally speaking, the resistivity change caused by inclusions (cracks) is intermediate between two extreme cases: inclusion effect expressed by connection in series, and inclusion effect expressed by parallel connection. Resistivity changes in three directions are attributed to geometry of the cracks, so the resistivity tensor is calculated for a specified crack geometry, by adding serial and parallel part of the change.
The Hundredth Anniversary of the First Chair of Geophysics. In Memory of Maurycy Pius Rudzki, Professor of the Jagiellonian University *** Stulecie Pierwszej Katedry Geofizyki
Author(s):
Volume: 273
Series: M-18
Volume: 273
Series: M-18
Our Earth has been the object of interest throughout the whole history of science. Searching for the beginnings of modern Earth's science, we should mention Newton, who established the physical background to it, and formulated the theory of gravitational attraction. The first gravity field theory together with earlier discoveries on the Earth's rotation constitute the fundamentals of this branch of science - and essential part of classical physics. Many basic problems related to our Globe, as for instance the theory of equilibrium figure, have been successfully approached by the most renown founders of mathematics and physics.
Results of Geomagnetic Observations, Polish Polar Station, Hornsund, Spitsbergen, 1990-1991
Author(s):
Volume: 272
Series: C-53
Volume: 272
Series: C-53
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 1990 and 1991.
Électricité Atmosphérique et Météorologie Observatoire Géophysique de S. Kalinowski à Świder 1993
Author(s): Warzecha S., Kubicki M.
Volume: 271
Series: D-43
Volume: 271
Series: D-43
The present issue contains the results of recordings of some elements of atmospheric electricity and daily observations of major meteorological factors noted at the S. Kalinowski Geophysical Observatory of the Polish Academy of Sciences at Świder in 1993.
Atmospheric Ozone, Solar Radiation, 1993
Author(s):
Volume: 269
Series: D-42
Volume: 269
Series: D-42
Ozone observations have been made by means of Dobson spectrophotometer No. 84 in the Geophysical Observatory at Belsk since March 1963. This publication presents all total ozone values and vertical distribution of ozone over Belsk in 1993 obtained from the conventional Umkehr observations.