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Banded iron formation and Cataclasite


Cataclasite and Banded iron formation


Definition

Definition
Banded iron formation are distinctive units of sedimentary rock that are almost always of Precambrian age   
Cataclasite is a type of cataclastic rock that is formed by fracturing and comminution during faulting. It is normally cohesive and non-foliated, consisting of angular clasts in a finer-grained matrix   

History
  
  

Origin
Western Australia, Minnesota   
Swiss Alps, Europe   

Discoverer
Unknown   
Michael Tellinger   

Etymology
From its formation process   
From the Italian word cataclasi   

Class
Sedimentary Rocks   
Metamorphic Rocks   

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

Family
  
  

Group
Not Applicable   
Not Applicable   

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

Texture

Texture
Banded, Trellis   
Clastic   

Color
Red, Reddish Brown   
Brown, Green, White, Yellow   

Maintenance
Less   
Less   

Durability
Durable   
Durable   

Water Resistant
No   
Yes   

Scratch Resistant
Yes   
No   

Stain Resistant
Yes   
No   

Wind Resistant
No   
No   

Acid Resistant
No   
No   

Appearance
Layered, Banded, Veined and Shiny   
Dull and Banded   

Uses

Architecture
  
  

Interior Uses
Decorative Aggregates, Homes   
Decorative Aggregates, Homes   

Exterior Uses
Paving Stone, Office Buildings   
As Building Stone, As Facing Stone, Paving Stone   

Other Architectural Uses
Curbing, Whetstones   
Curbing   

Industry
  
  

Construction Industry
As Dimension Stone, Used for flooring, stair treads, borders and window sills.   
As Dimension Stone, Building houses or walls, Cement Manufacture, Construction Aggregate, for Road Aggregate   

Medical Industry
Not Yet Used   
Not Yet Used   

Antiquity Uses
Artifacts   
Artifacts   

Other Uses
  
  

Commercial Uses
As a touchstone, Cemetery Markers, Creating Artwork   
Commemorative Tablets, Creating Artwork   

Types

Types
Algoma-type , Lake Superior-type, Superior-type and Taconite   
Protocataclasite, Mesocataclasite, Ultracataclasite and Foliated cataclasite   

Features
Is one of the oldest rock   
Easily splits into thin plates, Is one of the oldest rock   

Archaeological Significance
  
  

Monuments
Not Yet Used   
Not Yet Used   

Famous Monuments
Not Applicable   
Not Applicable   

Sculpture
Not Yet Used   
Not Yet Used   

Famous Sculptures
Not Applicable   
Not Applicable   

Pictographs
Not Used   
Used   

Petroglyphs
Not Used   
Used   

Figurines
Not Yet Used   
Not Yet Used   

Fossils
Present   
Absent   

Formation

Formation
The banded iron layers are formed in sea water when oxygen is released by photosynthetic cyano-bacteria. The oxygen then combines with dissolved iron in ocean to form insoluble iron oxides, which precipitated out, forming a thin layer of banded iron formation on ocean floor.   
Cataclasiste rocks mainly form by pressure deep under the Earth's surface, from the extreme heat caused by magma or by the intense collisions and friction of tectonic plates.   

Composition
  
  

Mineral Content
Hematite, Magnetite, Quartz   
Albite, Apatite, Augite, Biotite, Calcite, Enstatite, Epidote, Feldspar, Micas, Muscovite or Illite, Pyroxene, Quartz   

Compound Content
Fe, Iron(III) Oxide, Silicon Dioxide   
Silicon Dioxide   

Transformation
  
  

Metamorphism
No   
No   

Types of Metamorphism
Not Applicable   
Not Applicable   

Weathering
Yes   
Yes   

Types of Weathering
Chemical Weathering   
Mechanical Weathering   

Erosion
Yes   
Yes   

Types of Erosion
Coastal Erosion, Wind Erosion   
Coastal Erosion, Wind Erosion   

Properties

Physical Properties
  
  

Hardness
5.5-6   
3-4   

Grain Size
Large and Coarse Grained   
Fine Grained   

Fracture
Uneven, Splintery or Conchoidal   
NA   

Streak
White   
Black   

Porosity
Highly Porous   
Less Porous   

Luster
Earthy   
Vitreous   

Cleavage
Imperfect   
Not Available   

Toughness
1.5   
Not Available   

Specific Gravity
5.0-5.3   
2.1   

Transparency
Translucent to Opaque   
Translucent to Opaque   

Density
Not Available   
2.9-3.1 g/cm3   

Thermal Properties
  
  

Specific Heat Capacity
3.20 kJ/Kg K   
1
Not Available   

Resistance
Heat Resistant, Impact Resistant, Pressure Resistant, Wear Resistant   
Heat Resistant, Impact Resistant, Pressure Resistant   

Reserves

Deposits in Eastern Continents
  
  

Asia
China, India, Iran, Iraq, Oman, Russia, Saudi Arabia, Taiwan, Thailand, Vietnam   
China, India, Russia, Saudi Arabia, South Korea   

Africa
Kenya, Morocco, South Africa, Tanzania   
Egypt, Ethiopia, Kenya, Madagascar, Morocco, South Africa   

Europe
Austria, France, Greece, Italy, Malta, Poland, Portugal, Serbia, Spain, Sweden, United Kingdom   
England, Finland, France, Spain, United Kingdom   

Others
Greenland, Mid-Atlantic Ridge   
Not Yet Found   

Deposits in Western Continents
  
  

North America
Canada, Mexico, USA   
Canada, USA   

South America
Bolivia, Brazil   
Argentina, Colombia   

Deposits in Oceania Continent
  
  

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

Summary >>
<< Reserves

All about Banded iron formation and Cataclasite Properties

Know all about Banded iron formation and Cataclasite properties here. All properties of rocks are important as they define the type of rock and its application. Banded iron formation belongs to Sedimentary Rocks while Cataclasite belongs to Metamorphic Rocks.Texture of Banded iron formation is Banded, Trellis whereas that of Cataclasite is Clastic. Banded iron formation appears Layered, Banded, Veined and Shiny and Cataclasite appears Dull and Banded. The luster of Banded iron formation is earthy while that of Cataclasite is vitreous. Banded iron formation is available in red, reddish brown colors whereas Cataclasite is available in brown, green, white, yellow colors. The commercial uses of Banded iron formation are as a touchstone, cemetery markers, creating artwork and that of Cataclasite are commemorative tablets, creating artwork.

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