Article ID Journal Published Year Pages File Type
4675203 Procedia Earth and Planetary Science 2013 4 Pages PDF
Abstract

The Mecsekalja Zone crystalline metamorphic rocks are crosscut by a crack-seal texture vein generation. Crack-seal textures are indicative of intermittent hydraulic behavior of a fluid-rock system and of fluid pressure fluctuations. Here we present microthermometric and δD composition data from primary fluid inclusions of the crack-seal veins that are presented together with earlier published stable isotope compositions of the vein calcite. Taken together, this reveals some features of the hydraulic behavior of the fluid-rock system during the crack-seal process.

Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Atmospheric Science