Crack-seal microstructure evolution in bi-mineralic quartz–chlorite veins in shales and siltstones from the RWTH-1 well, Aachen, Germany

Author:

Becker Stephan,Hilgers Christoph,Kukla Peter A.,Urai Janos L.

Publisher

Elsevier BV

Subject

Geology

Reference73 articles.

1. Becker, S., 2008. The Aachen fold and thrust belt: an integration of surface geology, reflection seismics and new subsurface data of the well RWTH-1. Diploma Thesis, RWTH Aachen University.

2. Fluid inclusion characteristics of the Variscan and post-Variscan mineralizing fluids in the Federal Republic of Germany;Behr;Chemical Geology,1987

3. A Continent Revealed: The European Geotraverse;Blundell,1992

4. Experimental simulation of the formation of fibrous veins by localised dissolution-precipitation creep;Bons;Mineralogical Magazine,1997

5. The formation of veins and their microstructures;Bons;Journal of Virtual Explorer,2000

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