![Nesosilicates [SiO4]⁴-
• In the structure of nesosilicates, SiO4 tetrahedra are not directly connected with
mutual oxygen ion, only by interstitial cations. The simplest structure in nesosilicates
have mineral forsterite Mg2[SiO4]. The most important minerals from the
nesosilicates are shown in Table below. Olivine with little iron is closer to forsterite
with greenish color. The same with more iron is closer to fayalite with dark green
color. Olivine crystallizes in orthorhombic system and hardness of 7-6.5 (depending
on the isomorphous replacement of Mg with Fe). It forms by crystallization of
magma at high temperatures (pyrogen minerals). In normal atmospheric conditions,
it has low resistance to weathering and easily subjected to metamorphism in the
mineral serpentine (olivine serpentinization), talc or actinolite.](https://image.slidesharecdn.com/15002-250702122409-0470d604/85/Silicate-minerals-with-groups-in-categories-pdf-7-320.jpg)
![• Cyclosilicates, or ring silicates, have linked
tetrahedra with (SixO3x)2x or a ratio of 1:3.
These groups of minerals exist as three-
member [Si3O9)6-]. four-member (Si4O12)8-
and six member [Si6O18)12-]. rings.
• 1. Three-member ring Benitoite - BaTi(SiO3)3
• 2. Four-member ring Axinite
{(Ca,Fe,Mn)3Al2(BO3)(Si4O12)(OH)}
• 3. Six-member ring Beryl/Emerald
{Be3Al2(SiO3)6 Cordierite
{(Mg,Fe)2Al3(Si5AlO18)}](https://image.slidesharecdn.com/15002-250702122409-0470d604/85/Silicate-minerals-with-groups-in-categories-pdf-10-320.jpg)
Silicate minerals with groups in categories.pdf
- 1. University of Anbar Collage of Science Department of Geology Minerals / 1st stage. Silicate mineral group Assistant lecturer Nazar Zaidan Khalaf
- 2. Silicate mineral group lecture eaght Lectures eight, nine and ten Assistant lecturer Nazar Zaidan Al-Salmani
- 3. • Silicates mineral group • Silicates are the most common and most important petrogenic minerals, particularly feldspars, amphiboles, pyroxenes, olivine, micas and clay minerals. -Their main characteristics are: • difficult to melt and often have very complex chemical composition because of isomorphic replacement. Most silicate minerals are formed by crystallization of magma at high temperatures, and in metamorphic processes at high temperature and high pressure. • Silicate minerals are classified according to the structure with main feature of strong relationship between major oxygen ions, and minor silicon ions.
- 4. Silicates mineral group • Four oxygen ions are arranged in close form of the tetrahedron with a small silicon ion in the center. Therefore, the basic structural unit of silicate minerals is SiO4 tetrahedra.
- 5. • Structure • The basic structural unit of all silicate minerals is the silicon tetrahedron in which one silicon atom is surrounded by and bonded to (i.e., coordinated with) four oxygen atoms, each at the corner of a regular tetrahedron. These SiO4 tetrahedral units can share oxygen atoms and be linked in a variety of ways, which results in different structures • The topology of these structures forms the basis for silicate classification. For example, • nesosilicates are minerals whose structure are made up of independent silicate tetrahedrons. • Sorosilicates are silicate minerals consisting of double tetrahedral groups in which one oxygen atom is shared by two tetrahedrons. • Cyclosilicates, in contrast, are arranged in rings made up of three, four, or six tetrahedral units. • Inosilicates show a single-chain structure wherein each tetrahedron shares two oxygen atoms. • Phyllosilicates have a sheet structure in which each tetrahedron shares one oxygen atom with each of three other tetrahedrons. • Tectosilicates show a three-dimensional network of tetrahedrons, with each tetrahedral unit sharing all of its oxygen atoms. Silicates miner
- 6. • Silicate minerals are put together by binding siliconeoxygen tetrahedra to each other and to other ions in a fairly small number of ways. Even this number represents only variations on the theme of combining ionic and covalent bonds. The ionic bonding of tetrahedra involves another atom, a cation which usually carries a +2charge. This ion is situated between the corners of two tetrahedra where it can receive one electron from the nearest oxygen in each. The covalent bonding of tetrahedra involves actually sharing one oxygen atom between two adjacent tetrahedra. One of the extra electrons of the shared oxygen is used by one silicon, and the other electron is used by the other. Between these two extreme cases, there are a number of different cases of bonding two, three, four, six or more of the SiO4 tetrahedra, • so that there are seven different major structural types of silicate minerals. These are the following: Silicates mineral group
- 7. Nesosilicates [SiO4]⁴- • In the structure of nesosilicates, SiO4 tetrahedra are not directly connected with mutual oxygen ion, only by interstitial cations. The simplest structure in nesosilicates have mineral forsterite Mg2[SiO4]. The most important minerals from the nesosilicates are shown in Table below. Olivine with little iron is closer to forsterite with greenish color. The same with more iron is closer to fayalite with dark green color. Olivine crystallizes in orthorhombic system and hardness of 7-6.5 (depending on the isomorphous replacement of Mg with Fe). It forms by crystallization of magma at high temperatures (pyrogen minerals). In normal atmospheric conditions, it has low resistance to weathering and easily subjected to metamorphism in the mineral serpentine (olivine serpentinization), talc or actinolite.
- 8. The Most Important Petrogenic Minerals from Nesosilicates Group
- 9. • Sorosilicates have isolated double tetrahedra groups with (Si2O7)6- or a ratio of 2:7. There are no significant petrogenic minerals among sorosilicates, except epidote, zoisite and vesuvianite
- 10. • Cyclosilicates, or ring silicates, have linked tetrahedra with (SixO3x)2x or a ratio of 1:3. These groups of minerals exist as three- member [Si3O9)6-]. four-member (Si4O12)8- and six member [Si6O18)12-]. rings. • 1. Three-member ring Benitoite - BaTi(SiO3)3 • 2. Four-member ring Axinite {(Ca,Fe,Mn)3Al2(BO3)(Si4O12)(OH)} • 3. Six-member ring Beryl/Emerald {Be3Al2(SiO3)6 Cordierite {(Mg,Fe)2Al3(Si5AlO18)}
- 11. •The Most Important Petrogenic Cyclosilicates
- 12. Inosilicates • Inosilicates, or chain silicates, have interlocking chains of silicate tetrahedra with either SiO3, 1:3 ratio, for single chains or Si4O11, 4:11 ratio, for double chains. • SINGLE CHAIN- INOSILICATES,PYROXENE GROUP • The pyroxenes are important rock-forming inosilicate minerals and often exist in many igneous and metamorphic rocks. They share a common structure of single chains of silica tetrahedra . The group of minerals crystallizes in the monoclinic and orthorhombic systems. Inosilicates with a single-chain SiO4 tetrahedron of the pyroxene group are very important and widespread petrogenic minerals . Pyroxenes constitute a related group of silicate minerals with similar crystallographic, physical and chemical properties. The most important of them are given in Table below.
- 13. • The Most Important Petrogenic Minerals from Pyroxene Group
- 14. • The most petrogenic important minerals among the group are the following: • 1. Diopside-hedenbergite series • 2. Augite group • 3. Pyroxenes (aegirine-augite and jadeite-augite) • 4. Pigeonite
- 15. DOUBLE-CHAIN INOSILICATE/ AMPHIBOLE GROUP • Amphibole is an important group of generally dark-colored inosilicate minerals. It is composed of double-chain SiO4 tetrahedra, linked at the vertices and generally containing ions of iron and/or magnesium in their structures. Amphiboles crystallize in monoclinic and orthorhombic system. In chemical composition, amphiboles are similar to the pyroxenes. The differences from pyroxenes are that amphiboles contain essential hydroxyl (OH) or halogen (F, Cl) and the basic structure is a double chain of tetrahedra. Amphiboles are the primary constituent of amphibolites. Amphiboles along with pyroxenes and feldspars are the most abundant rock-forming minerals (Table below).
- 16. The Most Important Petrogenic Minerals of Amphibole Group
- 17. The basic structure of the phyllosilicates is based on interconnected six-member rings of tetrahedra that extend outward in infinite sheets. Three out of the four oxygens from each tetrahedron are shared with other tetrahedral as shown. The most important petrogenic minerals among phyllosilicates are group talc- pyrophyllite, mica, chlorite, vermiculite, smectite and kaolinitee serpentine (Table below).
- 18. The Most Important Petrogenic Minerals from the Group Phyllosilicates
- 20. References - S. K. HALDAR &JOSIP TISLJAR 2013, INTRODUCTION TO MINERALOGY AND PETROLOGY Elsevier 225 Wyman Street, Waltham, MA 02451, USA Publishers . 341 p. Blackburn, W.H. and Dennen, W.H., 1988, Principles of Mineralogy: Iowa, WCB Publishers . 413 p. ابراهيم مضوي بابكر . 2004 . المعادن علم , النيلين جامعة , كتاب منشور . 232 ص