Abstract
A calcium-rich stilbite occurs in the amygdaloidal cavity of the Upper Miocene dacite dyke at Bomeki, Miyagi Town, Miyagi Prefecture. Chemical analysis gave SiO2 56.38, Al2O3 15.89, CaO 7.94, Na2O 1.08, K2O.10, H2O+16.23 and H2O- 1.93wt%. Fe, Mn, Mg and P were not detected. This corresponds to Na1.00K.06Ca4.07Al8.96Si26.98O72•28.98H2O.
Cell-parameters calculated from x-ray powder data are a0=13.43, b0=18.21, c0=11.21Å and β=128.9° closing to those of stilbite. The Bomeki stilbite is nearly colorless to faintly white in color and the cleavage is perfect on (010). Mohs hardness=3-4, sp. gr.=2.22 and refractive indices α=1.492, β=1.500, γ=1.502 (γ-α=0.010), all±0.002.
The amount of exchangeable cations and cations-exchangeable capacity are only 37% of the theoretical value calculated from the chemical composition.