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Pseudotachylite and Migmatite


Migmatite and Pseudotachylite


Definition

Definition
Very fine grained fault rock which is composed of glassy matrix that often contains inclusions of wall-rock fragments.  
Migmatite is typically a granitic rock within a metamorphic host rock which is composed of two intermingled but distinguishable components  

History
  
  

Origin
USA  
Southern Alps, France  

Discoverer
Unknown  
Jakob Sederholm  

Etymology
From pseudo- +‎ tachylite, a glassy rock generated by frictional heat within faults.  
From the Greek word migma which means a mixture  

Class
Metamorphic Rocks  
Metamorphic Rocks  

Sub-Class
Durable Rock, Hard Rock  
Durable Rock, Medium Hardness Rock  

Family
  
  

Group
-  
-  

Other Categories
Fine Grained Rock, Opaque Rock  
Coarse Grained Rock, Fine Grained Rock, Medium Grained Rock, Opaque Rock  

Texture

Texture
Quench  
Foliated  

Color
Black, Brown, Green, Grey, Pink, White  
Black, Bluish - Grey, Brown, Brown- Black, Dark Greenish - Grey, Dark Grey to Black  

Maintenance
Less  
More  

Durability
Durable  
Durable  

Water Resistant
Yes  
Yes  

Scratch Resistant
Yes  
Yes  

Stain Resistant
No  
No  

Wind Resistant
Yes  
No  

Acid Resistant
Yes  
No  

Appearance
Dull and Soft  
Dull, Banded and Foilated  

Uses

Architecture
  
  

Interior Uses
Decorative Aggregates, Entryways, Interior Decoration  
Countertops, Flooring, Kitchens  

Exterior Uses
As Building Stone, As Facing Stone, Garden Decoration  
As Building Stone, As Facing Stone  

Other Architectural Uses
Curbing  
Curbing  

Industry
  
  

Construction Industry
As Dimension Stone, Cement Manufacture, for Road Aggregate, Making natural cement  
As Dimension Stone, Cement Manufacture, for Road Aggregate, Making natural cement  

Medical Industry
-  
-  

Antiquity Uses
Artifacts, Monuments  
Artifacts  

Other Uses
  
  

Commercial Uses
Creating Artwork, Gemstone  
Cemetery Markers, Jewelry, Tombstones, Used to manufracture paperweights and bookends  

Types

Types
Cataclastic rock  
Diatexites and Metatexites  

Features
Host Rock for Lead  
Generally rough to touch, Is one of the oldest rock  

Archaeological Significance
  
  

Monuments
-  
-  

Famous Monuments
-  
-  

Sculpture
-  
-  

Famous Sculptures
-  
-  

Pictographs
-  
-  

Petroglyphs
-  
-  

Figurines
-  
-  

Fossils
Absent  
Absent  

Formation

Formation
Due to change in environmental conditions, rocks are heated and pressurized deep inside the Earth's surface. Pseudotachylite is formed from the extreme heat caused by magma or by the intense collisions and friction of tectonic plates.  
Migmatites form by high temperature regional and thermal metamorphism of protolith rocks where rocks melt partially due to high temperature.   

Composition
  
  

Mineral Content
Iron Oxides, Pyroxene, Quartz, Stishovite, Sulfides  
Biotite, Chlorite, Feldspar, Garnet, Graphite, Hornblade, Micas, Muscovite or Illite, Quartz, Quartzite, Silica, Zircon  

Compound Content
Carbon Dioxide, Silicon Dioxide, Sulfur Dioxide, Sulphur  
Aluminium Oxide, NaCl, CaO, Carbon Dioxide, Iron(III) Oxide, FeO, Potassium Oxide, Magnesium Carbonate, MgO, MnO, Phosphorus Pentoxide, Silicon Dioxide, Titanium Dioxide  

Transformation
  
  

Metamorphism
Yes  
Yes  

Types of Metamorphism
Burial Metamorphism, Cataclastic Metamorphism, Contact Metamorphism  
Burial Metamorphism, Cataclastic Metamorphism, Regional Metamorphism  

Weathering
No  
Yes  

Types of Weathering
-  
Biological Weathering, Chemical Weathering, Mechanical Weathering  

Erosion
No  
Yes  

Types of Erosion
-  
Chemical Erosion, Glacier Erosion, Water Erosion, Wind Erosion  

Properties

Physical Properties
  
  

Hardness
7  
5.5-6.5  

Grain Size
Very fine-grained  
Medium to Fine Coarse Grained  

Fracture
Uneven  
Irregular  

Streak
Light to dark brown  
White  

Porosity
Less Porous  
Very Less Porous  

Luster
Vitreous  
Dull to Pearly to Subvitreous  

Compressive Strength
60.00 N/mm2  
37
120.00 N/mm2  
26

Cleavage
-  
-  

Toughness
-  
1.2  

Specific Gravity
2.46-2.86  
2.65-2.75  

Transparency
Transparent to Translucent  
Opaque  

Density
2.7-2.9 g/cm3  
-9999 g/cm3  

Thermal Properties
  
  

Specific Heat Capacity
0.92 kJ/Kg K  
10
0.79 kJ/Kg K  
17

Resistance
Heat Resistant  
Heat Resistant, Pressure Resistant  

Reserves

Deposits in Eastern Continents
  
  

Asia
South Korea  
China, India, Iran, Iraq, Kazakhstan, Kyrgyzstan, Mongolia, Russia  

Africa
Western Africa  
Cameroon, Ethiopia, Ghana, Kenya, Madagascar, Morocco, Mozambique, Namibia, Nigeria, Tanzania, Togo  

Europe
Great Britain, Switzerland  
Albania, Austria, Bosnia and Herzegovina, Finland, France, Georgia, Germany, Hungary, Italy, Kosovo, Monaco, Norway, Poland, Romania, Serbia, Slovakia, Slovenia, Sweden, Switzerland, Ukraine, United Kingdom  

Others
-  
-  

Deposits in Western Continents
  
  

North America
-  
Canada, Costa Rica, Cuba, Mexico, Panama, USA  

South America
-  
Argentina, Bolivia, Brazil, Chile, Colombia, Ecuador, Peru, Venezuela  

Deposits in Oceania Continent
  
  

Australia
Central Australia, Western Australia  
New South Wales, New Zealand, Queensland, Victoria  

Summary >>
<< Reserves

All about Pseudotachylite and Migmatite Properties

Know all about Pseudotachylite and Migmatite properties here. All properties of rocks are important as they define the type of rock and its application. Pseudotachylite and Migmatite belong to Metamorphic Rocks.Texture of Pseudotachylite is Quench whereas that of Migmatite is Foliated. Pseudotachylite appears Dull and Soft and Migmatite appears Dull, Banded and Foilated. The luster of Pseudotachylite is vitreous while that of Migmatite is dull to pearly to subvitreous. Pseudotachylite is available in black, brown, green, grey, pink, white colors whereas Migmatite is available in black, bluish - grey, brown, brown- black, dark greenish - grey, dark grey to black colors. The commercial uses of Pseudotachylite are creating artwork, gemstone and that of Migmatite are cemetery markers, jewelry, tombstones, used to manufracture paperweights and bookends.

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