Partially open grain and phase boundaries as fluid pathways in metamorphic and magmatic rocks

نویسندگان

چکیده

Transmission electron microscopy and 3D focused ion beam/scanning microscope nanotomography are applied to grain phase boundaries between quartz, plagioclase, K-feldspar, clinopyroxene, amphibole, calcite. The samples come from metamorphic, plutonic volcanic rocks, hydrothermal experienced cooling decompression after highly variable P–T peak conditions. Most of the partially open in range up several hundred nanometres partly totally filled with secondary minerals, such as actinolite, biotite, chlorite, sheet silicates, well amorphous matter. Cracking opening suggested be related anisotropic thermoelastic response crystals cooling. It starts below brittle–ductile transition involved minerals. boundaries, together dissolution-generated cavities, can form porosity more than 2 vol.% permeability under conditions at least lowermost greenschist facies. Such networks or refilled potentially affect properties crystalline rocks processes upper crust, metasomatism, weathering, migration radionuclides through bedrock geological repositories nuclear waste, deformation nature experiment.

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ژورنال

عنوان ژورنال: Journal of Metamorphic Geology

سال: 2021

ISSN: ['0263-4929', '1525-1314']

DOI: https://doi.org/10.1111/jmg.12610