Feldspar Group
Of Minerals
Presented By,
Meenakshi A
MSc Geology
Introduction
Feldspars are the most common rock forming mineral.
 Feldspars make up more than half of Earth’s crust.
Word feldspar is derived from German words :
FELD + SPAR
Feld : field and Spar : light colored minerals that break
with a smooth surface.
Common rock forming mineral in igneous and
metamorphic and sedimentary rocks.
• The silicate structure is Frame Work or Tecto-silicate structure also known as 3-D structure.
• Feldspars are Aluminosilicate minerals with the general formula : XAl Si O .
where X can be Na/K/Ca.
Structure of Feldspars
1-2 3-2 8
• The structure contains SiO4 and AlO4
tetrahedrons
• Each tetrahedron consists of a central
Silicon/Aluminum atom bonded to four
oxygen atoms.
• Si and Al tetrahedrons are arranged to
form 4 membered rings.
Structure of Feldspars
• These 4 membered rings are joined together to form Crankshaft Structure.
Structure of Feldspars
Structure of Feldspars
• The crankshaft structure created Voids.
• The positively charged cations: Na/K/Ca that occupy relatively large Voids/Intersticies in the frame
work structure.
Structure of Feldspars
Structure of Feldspars
COMPOSITION
• Feldspars include 3 principal end members:
1) Albite
2) Anorthite
3) K-feldspar
• Compositional range between albite and
anorthite is : Plagioclase feldspar AND
Between K-feldspar and Albite is Alkali
feldspar.
: NaAlSi3O8
: CaAl2Si2O8
: KAlSi3O8
Ternary Diagram Showing Compositional Range Of Feldspars
Alkali feldspars
Feldspars with composition ranging from:
KAlSi3O8 – NaAlSi3O8
Members include : Microcline
Sanidine
Anorthoclase
Orthoclase
Adularia
Alkali feldspars
Formation of different alkali feldspars based on cooling rate.
PHYSICAL
PROPERTIES
• Form/Habit : Usually prismatic, also tabular and elongated.
Colour : Flesh red, pink, light pink or red.
• Streak : White
• Lustre : Vitreous
• Cleavage : Perfect two directional
• Fracture : Uneven.
• Hardness : 6
• Specific Gravity : 2.57
Alkali feldspars
PHYSICAL
PROPERTIES
Crystallographic
system :
Alkali feldspars
Plagioclase feldspars
Feldspars with composition ranging from:
NaAlSi3O8 – CaAl2Si2O8
Members include :
Albite (Ca%0-10 – Na%100-90)
Oligoclase (Ca%10-30 – Na%90-70)
Andesine (Ca%30-50 – Na%70-50)
Labradorite (Ca%50-70 – Na%50-30)
Bytownite (Ca%70-90 – Na%30-10)
Anorthite (Ca%90-100 – Na%10-0)
PHYSICAL
PROPERTIES
Form/Habit : Usually prismatic, also tabular
Colour : Variable, usually white or light coloured, also grey and colourless
Streak : White
Lustre : Vitreous, semi-vitreous to pearly
Cleavage : Two directional
Fracture : Uneven and splintery
Hardness : 6.0 - 6.5
Specific Gravity : 2.55 - 2.76
Uses Of
Feldspars
• Feldspars are used widely in the glass
and ceramics industries.
• In addition, several feldspars are used
as gemstones. For example, moonstone.
• Amazonite, a green variety of
microcline, is used as an ornamental
material.
• Used in paint, fabrics etc.
References
Earth Materials 2nd Edition
Nesse
Rutley’s Elements of Mineralogy
Wikipedia
Study.com
Thank You All
Presented by,
Meenakshi A
MSc Geology
Year One
Email
meenakshi55ashok@email.com

Feldspar Group Of Minerals in geology.pptx

  • 1.
    Feldspar Group Of Minerals PresentedBy, Meenakshi A MSc Geology
  • 2.
    Introduction Feldspars are themost common rock forming mineral.  Feldspars make up more than half of Earth’s crust. Word feldspar is derived from German words : FELD + SPAR Feld : field and Spar : light colored minerals that break with a smooth surface. Common rock forming mineral in igneous and metamorphic and sedimentary rocks.
  • 3.
    • The silicatestructure is Frame Work or Tecto-silicate structure also known as 3-D structure. • Feldspars are Aluminosilicate minerals with the general formula : XAl Si O . where X can be Na/K/Ca. Structure of Feldspars 1-2 3-2 8 • The structure contains SiO4 and AlO4 tetrahedrons • Each tetrahedron consists of a central Silicon/Aluminum atom bonded to four oxygen atoms. • Si and Al tetrahedrons are arranged to form 4 membered rings.
  • 4.
  • 5.
    • These 4membered rings are joined together to form Crankshaft Structure. Structure of Feldspars
  • 6.
  • 7.
    • The crankshaftstructure created Voids. • The positively charged cations: Na/K/Ca that occupy relatively large Voids/Intersticies in the frame work structure. Structure of Feldspars
  • 8.
  • 9.
    COMPOSITION • Feldspars include3 principal end members: 1) Albite 2) Anorthite 3) K-feldspar • Compositional range between albite and anorthite is : Plagioclase feldspar AND Between K-feldspar and Albite is Alkali feldspar. : NaAlSi3O8 : CaAl2Si2O8 : KAlSi3O8
  • 10.
    Ternary Diagram ShowingCompositional Range Of Feldspars
  • 11.
    Alkali feldspars Feldspars withcomposition ranging from: KAlSi3O8 – NaAlSi3O8 Members include : Microcline Sanidine Anorthoclase Orthoclase Adularia
  • 12.
    Alkali feldspars Formation ofdifferent alkali feldspars based on cooling rate.
  • 13.
    PHYSICAL PROPERTIES • Form/Habit :Usually prismatic, also tabular and elongated. Colour : Flesh red, pink, light pink or red. • Streak : White • Lustre : Vitreous • Cleavage : Perfect two directional • Fracture : Uneven. • Hardness : 6 • Specific Gravity : 2.57 Alkali feldspars
  • 14.
  • 15.
    Plagioclase feldspars Feldspars withcomposition ranging from: NaAlSi3O8 – CaAl2Si2O8 Members include : Albite (Ca%0-10 – Na%100-90) Oligoclase (Ca%10-30 – Na%90-70) Andesine (Ca%30-50 – Na%70-50) Labradorite (Ca%50-70 – Na%50-30) Bytownite (Ca%70-90 – Na%30-10) Anorthite (Ca%90-100 – Na%10-0)
  • 16.
    PHYSICAL PROPERTIES Form/Habit : Usuallyprismatic, also tabular Colour : Variable, usually white or light coloured, also grey and colourless Streak : White Lustre : Vitreous, semi-vitreous to pearly Cleavage : Two directional Fracture : Uneven and splintery Hardness : 6.0 - 6.5 Specific Gravity : 2.55 - 2.76
  • 17.
    Uses Of Feldspars • Feldsparsare used widely in the glass and ceramics industries. • In addition, several feldspars are used as gemstones. For example, moonstone. • Amazonite, a green variety of microcline, is used as an ornamental material. • Used in paint, fabrics etc.
  • 18.
    References Earth Materials 2ndEdition Nesse Rutley’s Elements of Mineralogy Wikipedia Study.com
  • 19.
    Thank You All Presentedby, Meenakshi A MSc Geology Year One Email [email protected]