Textbook
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
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- No. Panggil
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PMB 539.6 ITA v . II
- Penerbit
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Switzerland :
Springer Mineralogy.,
2020
- Deskripsi Fisik
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xi, 1351p. : ill, ; 18 cm
- Bahasa
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English
- ISBN/ISSN
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978-3-030-26805-3
- Klasifikasi
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539.6 ITA v . II
- Tipe Isi
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- Tipe Media
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- Tipe Pembawa
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- Edisi
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1st vol
- Subjek
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- Info Detail Spesifik
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- Pernyataan Tanggungjawab
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Nikita V. Chukanov : Penulis
Versi lain/terkait
Tidak tersedia versi lain
Lampiran Berkas
Tidak Ada Data