Table T13. Photoelectric effect of igneous and alteration minerals associated with lower crustal and upper mantle environments.
Mineral
Composition
Pe
Clay Kaolinite Al4[Si4O10](OH)8 1.49

Illite KAl4[Si7AlO20](OH)4 2.05

Chlorite Mg12[(Si, Al)8O20](OH)16 1.40

Quartz SiO2 1.81

Chlorite Mg12[(Si, Al)8O20](OH)16 1.40

Spinel MgAl2O4 1.49

Serpentine Mg3[Si2O5](OH)4 1.40

Biotite K2Mg6[Si6Al2O20](OH)4 2.30

Calcite CaCO3 5.08
Amphibole Pargasite NaCa2Mg4Al3Si6O22(OH)2 2.55

Tremolite Ca2Mg5Si8O22(OH)2 2.62

Hornblende Ca2Fe+35[Si6Al2O22](OH)2 10.49
Fe-Ti oxide Ilmenite Fe+2Ti+4O3 16.63

Hematite Fe2O3 21.48

Magnetite Fe+2Fe+32O4 22.24
Olivine Forsterite Mg2SiO4 1.54

Fayalite Fe2SiO4 17.17
Pyroxene Orthopyroxene MgSiO3 1.84

Clinopyroxene CaMgSi2O6 3.53

Augite Mg2(SiAl)2O6 4.69

Orthoferrosilite FeSiO3 13.57
Feldspar Albite NaAlSi3O8 1.68

Anorthite CaAl2Si2O8 3.13
Pe = (Ze/10)3.6
Pe = ( AiZiPi)/( AiZi)

Notes: Ai = number of each atom in the molecule. Zi = atomic number for each element. Pe = photoelectric cross-section index.