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Silicates

      9th class - Silicates This group of minerals is extremely large. The fundamental building block of silicates is the SiO4 tetrahedron, and silicate structures are classified according to the degree of polymerization by corner-sharing of the tetrahedra:
Nesosilicates - have insular SiO4 tetrahedra.
Sorosilicates - have cluster structures with two, or rarely more, corner- sharing tetrahedra.
Cyclosilicates - have tetrahedra connected into rings.
Inosilicates - have tetrahedra in chains of infinite length.
Phyllosilicates - have rings of tetrahedra linked into continuous sheets.
Tektosilicates - have tetrahedra linked into a 3-dimensional framework.


List of exhibits

pyrop, jeden kus /12x8cm/ g8614
epidot, jeden kus /8x5cm/ g8664
vesuvian, jeden kus /8x7cm/ g8665
hessonit, jeden kus /10x6cm/ g8666
hessonit, jeden kus g8668
hessonit, jeden kus /7x7cm/ g8669
epidot, jeden kus /10x7cm/ g8670
epidot, jeden kus /10x7cm/ g8671
vesuvian, jeden kus /9x7cm/ g8672
vesuvian, jeden kus /7x7cm/ g8673
karfolit, jeden kus /10x9cm/ g8740
karfolit, jeden kus /11x6cm/ g8744
karfolit, dva kusy /9x6, 4x3cm/ g8745
karfolit, jeden kus /7x6cm/ g8750
epidot, jeden kus /8x5cm/ g8904
saponit, jeden kus /8x5cm/ g8905
prehnit, jeden kus /9x4cm/ g8908
datolit, jeden kus /12x8cm/ g8909
klinizoisit, jeden kus /10x7cm/ g8910
analcim, jeden kus /11x7cm/ g8911


Virtual museum of the Czech Geological Survey, www.geology.cz, (C) Czech Geological Survey, 2011, v.0.99 [13.12.2011]