Poly-elemental geochemical microfields of carbonyl type | Characteristic micro- and nanominerals and chemical compounds appeared from the decay of the carbonyls and their derivatives as a result of dynamometamorphism |
Pb-Zn-Mn-Ru-Pd-Pt-Au-Ag-C-Cl-F | Native Fe, Pb, Zn, Al, silicide FeSi, moissanite, graphite, iocite, hematite, goethite, manganosite, zincite, plattnerite, massicot, ferrihydrite, portlandite, calicinite, nahcolite, losiite, carobiite, williamite, silica gel SiO₂∙nH₂O, gelgraphite C∙nH₂O, oxides C2O3, C2O |
Pb-Fe-Ru-S-F | |
Pb-Pd-Pt-O-C | |
Zn-Ru-Au-Ag-S-Cl | |
Pb-Cu-Ni-Au-Pt-S |