BROWSE - VOLUME LIST
- A - Physics of the Earth's Interior
- B - Seismology
C - Geomagnetism
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
D - Physics of the Atmosphere
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
A - Physics of the Earth's Interior
Fault Zone Dynamics Evolution Patterns
Author(s): Senatorski P.
A model of fault zone dynamics is proposed. Slips along complex fault system, long-range interactions, any distribution of barriers and asperities (modelled by cohesive forces with breakdown strengths and non-zero breakdown slips), a velocity-dependent friction, healing and reactivation of cohesive forces, a circular causality between earthquakes and tectonic stresses are taken into account.
Europrobe Symposium, Jabłonna 1991
This paper summarizes results of recent heat flow analysis and litospheric thermal modelling in the Baltic Shield and the southwest shield margin. Special emphasis is given to the Danish and adjacent areas (Fig. 1) which contain the tectonic transition from areas of exposed Precambrian shield rocks to unexposed Precambrian and Caledonian structures, buried beneath sedimentary units of greatly variable thickness.
Symposium on Geodynamics. Jabłonna, May 15-17, 1989
Between the Veriscan orogen and the edge of the East European Platform there runs a strip of the North German-Polish Caledonides. They are an orogen which formed as a result of a sinistral strike slip in the Silurian period. Because of the strike slip movement, the litosphere was broken up, divided into blocks, and then the blocks were shuffled, docked and concentrated at the cut-off edge of the East European Platform.
A Parabolic Relation between the Surface Heat Flow and Radiogenic Heat Production for Heat Flow Provinces
Author(s): Maj S.
A nonlinear (parabolic) relation between the surface heat flow J and radiogenic heat generation Q in crystalline ground for the heat flow provinces is derived.
Wyniki Sejsmicznych Badań Głębokiej Struktury Skorupy Ziemskiej Obszaru Polski 1969-1985 *** Results of Seismic Crustal Studies in Poland
Author(s): Guterch A., Grad M., Materzok R., Toporkiewicz S., Perchuć E.
One of the major tectonic problems in Europe is determination of the south-west margin of the East European Platform in the region of the so-called Polish-Danish trough. In general, this margin is assumed to be the Tornquist-Teisseyre Line running approximately from NW to SE in this part of Europe. Determination of deep crustal structure of the contact zone between the Precambrian Platform and the Palaeozoic Platform was main aim of the deep seismic sounding program in Poland in 1969-1982 years.