Deutsche Vulkanologische Gesellschaft e.V., Mendig

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Prof. Dr. Christoph Breitkreuz


Institut für Geologie
Professur für Allgemeine und Historische Geologie
TU Bergakadamie Freiberg
Bernhard-von-Cotta Str. 2
09599 Freiberg/Germany


cbreit@geo.tu-freiberg.de

 

Here you can find more information about these scientific projects:

 

last update 16.07.2009
Forth conference on laccolith and sills:



Physical geology of subvolcanic systems: laccoliths, sills, and dykes


Moab and Mount Hillers - Utah - USA,  20-23 September 2010
 

 

http://lasi.lmtg.obs-mip.fr/LASI4/home.html


 

Centre for Volcanic Textures - with biennal Short course

 

next: Oct. 8th - 12th, 2009

 

The concept of the CVT:

Volcanic textures observable in outcrop, rock slab and thin sections are the result of complex processes during magma ascent, fragmentation during eruption, emplacement, cooling, diagenesis/hydrothermal overprint and deformation. Analysis of volcanic textures provides a powerful tool for the reconstruction of these processes both in young volcanic fields and in ancient volcanic successions. The distinction between SiO2-rich lavas, ignimbrites and subvolcanic intrusions, for example, is not trivial, and it bears important implications for the geotectonic setting and basin development. Apart from basic scientific projects, volcanic texture analysis is significant in mineral deposit and hydrocarbon exploration, and in assessment of volcanic hazards.

 

http://www.geo.tu-freiberg.de/dynamo/CVT.htm

 

VENTS = Polish-Czech-German project on Late Paleozoic magmatism

 

Project outline

During the Late Carboniferous - Early Permian, the northern margin of the Bohemian Massif was characterized by the formation of tectonically controlled basins and by strong volcanic activity. Volcanic and subvolcanic products of the predominantly calc-alkaline magmatism are intercalated within intermontane basins, like the Intra-Sudetic Basin, the North- Sudetic Basin, the Karkonosze-Piedmont Basin and the Döhlen Basin, in southern Poland, northern Czech Republic and eastern Saxony, respectively. In addition, important information on the magmatic evolution of these systems can be achieved by investigation of subvolcanic bodies cropping out in adjacent basement blocks like the Lusitanian Block in eastern Saxony and the Karkonosze Block in Poland and the Czech Republic.

The VENTS program which will have a duration of 6 years involves project leaders from three Polish universities ( Wrocław, Poznań, Warszawa), one German university (Freiberg ) and the Saxonian Geological Survey, and the Charles University and the Geological Survey of the Czech Republic .

 

www.geo.tu-freiberg.de/dynamo/VENTS.htm