Evidence for exhumation of a granite intrusion in a regional extensional stress regime based on coupled microstructural and fluid inclusion plane studies – An example from the Velence Mts., Hungary
Zsolt Benkó(University of Debrecen), Tamás Váczi(Eötvös Loránd University), Marc Lespinasse(Université de Lorraine), Ferenc Molnár(Geological Survey of Finland)
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