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 exhibitsrubelit, jeden kus /11x7cm/ g8629muskovit, jeden kus /11x9cm/ g8630 dialag, jeden kus /10x6cm/ g8631 verdelit /turmalín/, jeden kus /8x7cm/ g8632 turmalín, jeden kus /12x7cm/ g8633 lepidolit, jeden kus /10x7cm/ g8634 muskovit, záhněda, jeden kus /9x7cm/ g8636 skapolit, jeden kus /7x6cm/ g8638 skapolit s aktinolitem, jeden kus /10x6cm/ g8639 albit, křemen, jeden kus /6x6cm/ g8640 granát, jeden kus /11x8cm/ g8642 hessonit /granát/, jeden kus /17x7cm/ g8643 turmalín, jeden kus /10x7cm/ g8602 granát, jeden kus /9x8cm/ g8644 granát, jeden kus /11x8cm/ g8645 epidot, dva kusy /12x8cm, 11x8cm/ g8646 hessonit /granát/, jeden kus /12x10cm/ g8647 hessonit, jeden kus /9x6cm/ g8648 vesuvian, jeden kus /7x7cm/ g8649 vesuvian, jeden kus /12x7cm/ g8650 |