Download presentation
Presentation is loading. Please wait.
Published byAdele Phillips Modified over 9 years ago
1
Mineralogy Minerals and crystals
2
World’s largest crystals: A cave in the Naica Lead Zinc mine, Mexico
3
Miners in Cueva de los Crystals: the mineral gypsum Crystals of a variety of gypsum (CaSO 4.2H 2 O) precipitated from hot water at 60 degrees celsius in a limestone cave in the Naica mine
4
Minerals Tourmaline on Feldspar Emerald Beryl (Be 3 Al 2 (SiO 3 ) 6
5
Crystal Shapes Halite (NaCl) Diamond (C) Quartz (SiO 2 ) Garnet (Fe 3 Al 2 Si 3 O 12 ) Stibnite (Sb 2 S 3 ) Calcite (CaCO 3 )
6
Pyrite (FeS 2 ) crystals
7
Feldspars – two of the most important rock-forming minerals Plagioclase Albite – NaAlSi 3 O 8 Anorthite CaAl 2 Si 2 O 8 K-feldspar KAlSi 3 O 8 Microcline Orthoclase Sanidine
8
Colours and forms of quartz Milky quartz Rose quartz Amethyst Citrine
9
Quartz crystals displaying prism and pyramid faces
10
Faces display consistent angular relationships Quartz Crystal Angles measured with a goniometer Prism Pyramid
11
Crystals have ordered arrangements of atoms Order Disorder
12
X-ray beam splits into numerous smaller beams. Interference of waves of different beams produces a diffraction pattern on a screen or film. The pattern indicates the spacing and arrangement of atoms. X-ray diffraction
13
Surface of galena (PbS) imaged With an atomic force microscope Atomic structure of galena (PbS) Sulphur Lead
14
The atomic structure of halite (NaCl) Ionic bonding
15
Ionic bonding – transfer of electrons Cation + Anion -
16
Relative sizes of ions Ion co-ordination
17
The atomic structure of diamond Covalent bonding
18
The source of Diamonds Kimberlite containing diamond The ‘Big Hole’ at Kimberly, South Africa
19
Cutting diamonds
20
Covalent bonding – sharing of electrons
21
Atomic structure of graphite Covalent bonding within sheet Van der Waal’s bonding between sheets
22
Ice Crystals Hydrogen bonding
23
The silicon tetrahedron
24
Silicate Structures Inosilicate (Single chain) Sheet silicate Nesosilicate (Double chain) Framework silicate SiO 4 4 - SiO 3 2- Si 4 O 10 4 - SiO 2 Si 4 O 11 6 -
25
(Fe,Mg) 2 SiO 4 Nesosilicate Olivine
26
Diopside CaMgSi 2 O 6 Hypersthene (Fe,Mg)SiO 3 Inosilicate (Single Chain) Pyroxene
27
Inosilicate (Double Chain) Amphibole Tremolite Ca 2 Mg 5 Si 8 O 22 (OH) 2 Riebeckite Na 2 Fe 5 Si 8 O 22( OH) 2 Tigers Eye
28
Sheet Silicate Biotite KAl(Fe,Mg) 3 Si 3 O 10 (OH) 2 Muscovite KAl 3 Si 3 O 10 (OH) 2
29
Asbestos Uses and risks (Insulation, heat, fire resistance) Serpentine (Mg 3 Si 2 O 5 (OH) 4 Chrysotile (Mg 3 Si 2 O 5 (OH) 4
30
Framework Silicate Quartz SiO 2 Plagioclase Albite NaAlSi 3 O 8 Anorthite CaAl 2 Si 2 O 8 K-feldspar KAlSi 3 O 8 Amethyst SiO 2
31
Relationship of Quartz structure to Feldspar Structure Imagine four SiO 2 molecules 4 x SiO 2 = Si 4 O 8 Substitute Al 3+ for Si 4+ in one of these molecules SiO 2 +AlO 2 +SiO 2 +SiO 2 = AlSi 3 O 8 - Add Na + or K + to supply missing charge = NaAlSi 3 O 8 or KAlSi 3 O 8 SiO 2 +AlO 2 + SiO 2 = Al 2 Si 2 O 8 2- Add Ca 2+ to supply missing charge = CaAl 2 Si 2 O 8 Albite K-Feldspar Anorthite
Similar presentations
© 2024 SlidePlayer.com. Inc.
All rights reserved.