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Vibrational (infrared and raman) spectra of minerals and related compounds (volume 1)

Vesuvianite-group minerals (VGM) are wide• spread and occur in different geological formations including regional metamorphic rocks, skams, rodingites, etc. Specific crystal-chemical features of these minerals reflect conditions of their crystallization. As a rule, high-temperature VGM have high-symmetry structures (space group P4/ nnc), whereas low-temperature samples are characterized by the symmetry P4/n or P4nc (Allen and Burnham 1992). The simplified crystal-chemical formula of VGM is X18(X'Yl) Y24Y3sT 0-s(Si04)1o(Si201)401_2 W9 where X, X' = Ca, Na, K, Fe2+, and REE (cations with coordinationnumbers from 7 to 9); Yl-Y3 = Al, Mg, Fe2+, Fe3+, Mn2+, Mn3+, Ti, Cr, Cu, Zn; T = B, Al, D; W = OH, F, 0. The Yl cations have tetragonal-pyramidal coordination, whereas the Y2 and Y3 cations occur in octahedra

Ketersediaan
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Pusat Sumber Daya Mineral, Batubara dan Panas Bumi - Jln. Soekarno Hatta No. 444, Bandung, Jawa Barat PMB 539.6 ITA v . II
PMB 539.6 ITA v . II
Tersedia
Informasi Detail
Judul Seri
-
No. Panggil
PMB 539.6 ITA v . II
Penerbit
Switzerland : Springer Mineralogy.,
Deskripsi Fisik
xi, 1351p. : ill, ; 18 cm
Bahasa
English
ISBN/ISSN
978-3-030-26805-3
Klasifikasi
539.6 ITA v . II
Tipe Isi
-
Tipe Media
-
Tipe Pembawa
-
Edisi
1st vol
Subjek
Minerals
Infrared and Raman
Vibrational Spectra
Info Detail Spesifik
-
Pernyataan Tanggungjawab
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Tidak tersedia versi lain

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