Auflistung 11. Symposium "Tektonik, Struktur- und Kristallingeologie" , 2006-03 nach Schlagwort "Geodynamik der Lithosphäre {Geologie}"
Anzeige der Dokumente 1-6 von 6
-
Asymmetrical deformation of the Piton de la Fournaise (Réunion Island) summit cone
(11. Symposium "Tektonik, Struktur- und Kristallingeologie", 2006-03)Piton de la Fournaise (Réunion Island) is an active basaltic shield volcano in the south-western part of the Indian Ocean. The activity consists essentially of lava being issued from two rift zones close to the summit cone. ... -
Evolution of the Tamtsag Basin / NE-Mongolia — part I: basin fill
(11. Symposium "Tektonik, Struktur- und Kristallingeologie", 2006-03)The Tamtsag Basin in NE Mongolia is part of a widespread basin system which formed during Late Jurassic and Cretaceous times (Graham et al. 2001, Qing-Ren et al. 2003). It is filled with continental sediments and volcanics ... -
How stress transfer between volcanic and seismic zones affects volcanic and earthquake
(11. Symposium "Tektonik, Struktur- und Kristallingeologie", 2006-03)Oceanic transform faults and ridge segments form a network where mechanical interaction is to be expected. In particular, dike emplacement in ridge segments is likely to affect earthquake activity in the adjacent transform ... -
Kinematic 3D Retro-Deformation of Fault Blocks Picked from 3D Seismics
; Lohr, Tina; ; ; Endres, Heike; Samiee, Ramin; Trappe, Henning; (11. Symposium "Tektonik, Struktur- und Kristallingeologie", 2006-03)
Movement on fault planes causes a large amount of smaller-scale deformation, ductile or brittle, in the area surrounding the fault. Much of this deformation is below the resolution of reflection seismics (i.e. sub-seismic, ... -
Microstructural analysis of the RWTH-1 cores in thinsections
Scholz, Katerina;; Trautwein, Ute; (11. Symposium "Tektonik, Struktur- und Kristallingeologie", 2006-03)
The Aachen RWTH-1 well was drilled to 2544mTVD for geothermal purposes and gives substance to extensive geoscientific research. It is located in a hydrothermally and seismically active area of the Aachen Anticline, 500m ... -
Origin of Central Andean collapse calderas
(11. Symposium "Tektonik, Struktur- und Kristallingeologie", 2006-03)
Regional strains in tectonically active volcanic provinces may have a profound influence on the mode of collapse caldera formation. Conversely, the deformation pattern, more specifically, the symmetry of plan-view strain ...
