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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Online First
A - Physics of the Earth's Interior
Shear Cracks in an External Stress Field
Author(s): Niewiadomski J.
Volume: 150
Series: A-12
Volume: 150
Series: A-12
Deformations of the Earth's crust, which often manifest themself in the form of earthquakes, are a result of complex physical and chemical processes taking place within the Earth. They probably also depend on thermodynamically conditions and subsequent changes in physical and chemical properties of the material: modului of elasticity, heat conductivity, magnetic properties, or hydro-gaso-dynamic components (Savarensky et. al., 1972).
Determination of Source Parameters from Seismograms of Mining Tremors and the Inverse Problem for a Seismic Source
Author(s): Cichowicz A.
Volume: 147
Series: A-11
Volume: 147
Series: A-11
Problem of seismic source modelling are considered. Changes in a theoretical pulse shape depending upon the adopted model of slip velocity on the fault plane are analyzed in details. The influence of the medium and of the recording instrument upon the pulse form is taken into account. Additionally, ground motions were determined from deconvolution of real records. A simple method of determining the source parameters directly from seismograms is described.
Symposium of the European Seismological Commission. Physics of Earthquake Source and Earthquake Prediction Problems, Mogilany, 1-6 June 1979
Author(s):
Volume: 142
Series: A-10
Volume: 142
Series: A-10
This volume contains the papers from Symposium of the European Seismological Commission "Physics of Earthquake Source and Earthquake Prediction Problems", Mogilany, 1-6 June 1979.
Proceedings of the XVI General Assembly of the European Seismological Commission, Strasbourg, August 29 - September 5, 1978. Symposia of Subcommissions
Editor(s): Teisseyre R.
Volume: 135
Series: A-9
Volume: 135
Series: A-9
Proceedings of the 16th General Assembly of the European Seismological Commission, Strasbourg, August 29 - September 5, 1978 contains the papers (or their abstracts only) which were presented at the meetings of subcommissions and working groups. The present volume also contains some papers which for technical reasons were not submitted on time for the preceding volumes of papers from Strasbourg. A few papers which were presented during the symposia in Strasbourg but were not mentioned in the announcement for the ESC meeting are also included.
Symposium on Geodynamics. Jabłonna, 30 June - 2 July 1977
Author(s):
Volume: 130
Series: A-8
Volume: 130
Series: A-8
This volume contains the papers from Symposium on Geodynamics. Jabłonna, 30 June - 2 July 1977.