BROWSE - VOLUME LIST
- A - Physics of the Earth's Interior
- B - Seismology
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C - Geomagnetism
C-119, 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
Results of Geomagnetic Observations, Arctowski Antarctic Station 1990-1991
Author(s): Glegolski W., Gnoiński A.
Volume: 276
Series: C-54
Volume: 276
Series: C-54
This volume contains the results of observations of the Earth's magnetic field for the years 1990 and 1991 carried out at the Polish Antarctic Station Arctowski situated in King George Island, South Shetland Archipelago, and processed at the Institute of Geophysics. The station is currently managed by the Department of Antarctic Biology.
Thermodynamic Model of the Core-mantle Boundary
Author(s): Majewski E.
Volume: 275
Series: A-25
Volume: 275
Series: A-25
High pressure atomic diffusion of Fe0.94O from the mantle to the liquid outer core, solution of Fe0.94O in the liquid outer core, melting of FeS-troilite at the core-mantle boundary in the Earth, and diffusion of liquid iron from the outer core to D'' layer, are modelled. The core-mantle boundary is treated as a phase boundary and a surface of solution. The liquid outer core is modelled as a solution layer. Some interactions between the core-mantle boundary and the inner core boundary are considered. It is assumed the Fe0.94O soluted and FeS-troilite melted at the core-mantle boundary are transported in the process of thermal convection in the outer core to the inner core boundary. Next, Fe0.94O precipitates and FeS-troilite crystallizes at the inner core boundary. Local equations for the diffusion-controlled and interface-reaction-controlled rates of mass transfer across the core-mantle boundary are derived.
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.