Supplementary data
Table S1. (part 1) Detailed list of 62 minerals used in research. C refers to Class (Table 1). Bold font in names refers to the short names used in figures.
Mineral name C Empirical formula Mineral name C Empirical formula algodonite 2 Cu6As azurite 5 Cu3(CO3)2(OH)2 antimonpearceite 2 Ag12Cu4Sb1.5As0.5S11 malachite 5 Cu2(CO3)(OH)2 bornite 2 Cu5Fe2+S4 brochantite 7 Cu4(SO4)(OH)6 bournonite 2 PbCuSbS3 copiapite 7 Fe2+Fe3+4(SO4)6(OH)2•20(H2O) chalcopyrite 2 CuFe2+S2 devilline 7 CaCu4(OH)6(SO4)2•3(H2O) colusite 2 Cu12.5V5+As1.5Sb0.9Sn0.6Ge0.3S16 fornacite 7 Pb2Cu(AsO4)(CrO4)(OH) covellite 2 CuS langite 7 Cu4(SO4)(OH)6•2(H2O) digenite 2 Cu9S5 nakauriite 7 Mn2+4Ni3Cu(SO4)4(CO3)(OH)6•48(H2O) enargite 2 Cu3AsS4 natrochalcite 7 NaCu2(SO4)2(OH)•(H2O) freibergite 2 Ag7.2Cu3.6Fe2+1.2Sb3AsS13 osarizawaite 7 PbCuAl2(SO4)2(OH)6 germanite 2 Cu26Fe2+4Ge4S32 posnjakite 7 Cu4(SO4)(OH)6•(H2O) gladite 2 PbCuBi5S9 vauquelinite 7 Pb2Cu(CrO4)(PO4)(OH) idaite 2 Cu5Fe2+S6 arthurite 8 CuFe3+22(AsO4)0.72(PO4)0.22(SO4)0.1O1.5(OH)0.5•4(H2O) jaskolskiite 2 Pb2.2Cu0.2Sb1.2Bi0.6S5 chenevixite 8 Cu2Fe3+2(AsO4)2(OH)4•(H2O) krupkaite 2 PbCuBi3S6 clinoclase 8 Cu3(AsO4)(OH)3 seligmannite 2 PbCuAsS3 conichalcite 8 CaCu(AsO4)(OH) stannite 2 Cu2Fe2+SnS4 cornetite (co0) 8 Cu3(PO4)(OH)3 stromeyerite 2 CuAgS cornubite 8 Cu5(AsO4)2(OH)4•(H2O) 2+ tetrahedrite 2 Cu9Fe 3Sb4S13 descloizite 8 PbZn(VO4)(OH) umangite 2 Cu3Se2 duftite 8 PbCu(AsO4)(OH) boleite 3 KAg9Cu24Pb26Cl62(OH)48 libethenite 8 Cu2(PO4)(OH) kinoite 3 Ca2Cu2Si3O10•2(H2O) mottramite 8 PbCu(VO4)(OH) cuprite 4 Cu2O olivenite 8 Cu2(AsO4)(OH) delafossite 4 CuFe3+O2 parnauite 8 Cu9(AsO4)2(SO4)(OH)10•7(H2O) tenorite 4 CuO pseudomalachite 8 Cu5(PO4)2(OH) delafossite 4 CuFe3+O2 turquoise 8 CuAl6(PO4)4(OH)8•4(H2O) Table S1. (part 2) Detailed list of 62 minerals used in research. C refers to Class (Table 1). Bold font in names refers to the short names used in figures.
Mineral name C Empirical formula Mineral name C Empirical formula richelsdorfite 8 Ca2Cu5Sb(AsO4)4Cl(OH)6•6(H2O) creaseyite 9 Pb2Cu2Fe3+1.75Al0.25Si5O17•6(H2O) tsumebite 8 Pb2Cu(PO4)(SO4)(OH) dioptase 9 CuSiO2(OH)2 tyrolite 8 CaCu5(AsO4)2(CO3)(OH)4•6(H2O) halloysite 9 Al2Si2O5(OH)4 ajoite 9 K2.25Na1.75Cu20Al3Si29O76(OH)16•8(H2O) plancheite 9 Cu8Si8O22(OH)4•(H2O) allophane 9 (Al2O3)(SiO2)1.3•2.5(H2O) vesuvianite 9 Ca10Mg2Al4(Si2O7)2(SiO4)5(OH)4 chrysocolla 9 Cu1.75Al0.25H1.75(Si2O5)(OH)4•0.25(H2O)
Figure S1. The number of measurement points (MPs) taken per mineral together with their partitions into possible reference and validation only ones.
Figure S2. The number of different (exclusive) rock samples on which MPs were taken – listed per mineral.
Figure S3. Heatmap representing elements composition among all 62 minerals in accordance to mineral’s empirical formula [24]. The sorting from left to right was done based on the shortest N‐dimensional distance between each pair of minerals where the first pla‐9 is the closest to the origin of PCA space.
Figure S4. NTF model: a nonnegative 3‐way tensor Y is represented by a tensor‐matrix product of the latent component matrices 𝑈 , 𝑈 , 𝑈 with an identity tensor I or equivalently by a sum of J rank‐1 tensors obtained by an outer product of the latent components.
J = 2 J = 3 J = 4
Mineral U Mineral U Mineral U
1 1 1
0.8 0.8 0.8
0.6 0.6 0.6 0.9 0.4 0.85 0.4 0.4 0.8 CONTRIBUTION CONTRIBUTION CONTRIBUTION 0.2 0.2 0.2 0.15 0.16 0 0 0.06 0.04 0 0.03 0.01 12 123 1234 LATENT SPECTRA INDEX LATENT SPECTRA INDEX LATENT SPECTRA INDEX
(a) (b) (c)