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Abstract Trace element partitioning in clinopyroxene and amphibole governs the geochemical evolution of alkaline magmas, directly impacting liquid lines of descent reconstruction, volcanic hazard assessment and magmatic ore exploration in these volcanic settings.
The physical characterization of carbonate–bearing normal faults is fundamental for resource development and seismic hazard. Here we report laboratory measurements of density, porosity, Vp, Vs, elastic moduli and permeability for a range of effective confining pressures (0.1-100 MPa), conducted on samples representing different structural domains of a carbonate-bearing fault.
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