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Pegmatite and Marl


Marl and Pegmatite


Definition

Definition
Pegmatite rock is a holocrystalline, intrusive igneous rock which is composed of interlocking phaneritic crystals  
Marl is an unconsolidated sedimentary rock consisting of clay and lime  

History
  
  

Origin
-  
-  

Discoverer
R. J. Hauy  
William Smith  

Etymology
From Greek pegma, pegmat which means- thing joined together + -ite  
From Old French marle, from Late Latin marglia  

Class
Igneous Rocks  
Sedimentary Rocks  

Sub-Class
Durable Rock, Hard Rock  
Durable Rock, Soft Rock  

Family
  
  

Group
Plutonic  
-  

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

Texture

Texture
Pegmatitic  
Earthy  

Color
Black, Brown, Cream, Green, Grey, Pink, Red, Rust, Silver, White, Yellow  
Beige, Brown, Green, Grey, White  

Maintenance
Less  
Less  

Durability
Durable  
Durable  

Water Resistant
Yes  
Yes  

Scratch Resistant
Yes  
No  

Stain Resistant
Yes  
No  

Wind Resistant
No  
No  

Acid Resistant
No  
No  

Appearance
Layered, Banded, Veined and Shiny  
Rough and Dull  

Uses

Architecture
  
  

Interior Uses
Decorative Aggregates, Flooring, Interior Decoration  
Decorative Aggregates, Floor Tiles  

Exterior Uses
As Building Stone, As Facing Stone, Paving Stone  
As Building Stone, Roof Tiles  

Other Architectural Uses
Curbing  
Curbing  

Industry
  
  

Construction Industry
As Dimension Stone, Building houses or walls, Construction Aggregate, for Road Aggregate, Landscaping  
Cement Manufacture, Construction Aggregate, for Road Aggregate, Making natural cement, Raw material for the manufacture of mortar  

Medical Industry
-  
-  

Antiquity Uses
Artifacts, Sculpture, Small Figurines  
Artifacts, Jewellery, Sculpture, Small Figurines  

Other Uses
  
  

Commercial Uses
Creating Artwork, Jewelry, Source of corundum, tourmalines, beryls and topaz  
Creating Artwork, Soil Conditioner  

Types

Types
Granite Pegmatite, Gabbro Pegmatite and Diorite Pegmatite  
Clay Marl ,Blue Marl, Red Marl, High Bank Marl, Shell Layer Marl, Under Shell Layer Marl, Sand Marl, Green Marl, Grey Marl and Clayey Marl  

Features
Generally rough to touch, Is one of the oldest rock, Source of corundum, tourmalines, beryls and topaz  
Generally rough to touch, Is one of the oldest rock, Splintery, Very fine grained rock  

Archaeological Significance
  
  

Monuments
-  
-  

Famous Monuments
-  
-  

Sculpture
-  
-  

Famous Sculptures
-  
-  

Pictographs
-  
-  

Petroglyphs
-  
-  

Figurines
-  
-  

Fossils
Absent  
Present  

Formation

Formation
Pegmatite rock is holocrystalline, intrusive igneous rock which is formed by partial melting and dewatering during the process of metamorphism.  
Marl forms when very fine-grained clay particles are deposited in water which settles at the bottom of water bodies and are compacted by overlying sediment; the water squeezes out and hence forming Marl rock.  

Composition
  
  

Mineral Content
Apatite, Beryl, Feldspar, Fluorite, Garnet, Lepidolite, Quartz, Silica, Spodumene, Topaz  
Calcite, Clay, Dolomite, Gypsum, Micas, Pyrite, Quartz  

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

Transformation
  
  

Metamorphism
Yes  
No  

Types of Metamorphism
Burial Metamorphism, Cataclastic Metamorphism, Contact Metamorphism, Hydrothermal Metamorphism, Impact Metamorphism, Regional Metamorphism  
-  

Weathering
Yes  
Yes  

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

Erosion
Yes  
Yes  

Types of Erosion
Chemical Erosion, Coastal Erosion, Glacier Erosion, Sea Erosion, Water Erosion, Wind Erosion  
Chemical Erosion, Coastal Erosion, Water Erosion, Wind Erosion  

Properties

Physical Properties
  
  

Hardness
7  
2-3  

Grain Size
Medium to Coarse Grained  
Very fine-grained  

Fracture
Conchoidal  
Conchoidal  

Streak
White  
White  

Porosity
Less Porous  
Highly Porous  

Luster
Grainy, Pearly and Vitreous  
Dull  

Compressive Strength
178.54 N/mm2  
19
30.00 N/mm2  
99+

Cleavage
Perfect  
-  

Toughness
2.1  
2.6  

Specific Gravity
2.6-2.63  
2.2-2.8  

Transparency
Translucent to Opaque  
Opaque  

Density
2.6-2.65 g/cm3  
2.4-2.8 g/cm3  

Thermal Properties
  
  

Specific Heat Capacity
0.79 kJ/Kg K  
17
0.80 kJ/Kg K  
16

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

Reserves

Deposits in Eastern Continents
  
  

Asia
China, India, Iran, Japan, Nepal, North Korea, Russia, Saudi Arabia, South Korea  
India, Pakistan, Russia  

Africa
South Africa  
Ethiopia, Kenya, Morocco, South Africa  

Europe
Austria, France, Greece, Ireland, Italy, Netherlands, Slovakia, Spain, Turkey, Ukraine  
Austria, France, Germany, Greece, Italy, Romania, Scotland, Spain, Switzerland  

Others
-  
-  

Deposits in Western Continents
  
  

North America
Canada  
USA  

South America
Brazil  
Colombia, Ecuador, Peru  

Deposits in Oceania Continent
  
  

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

Summary >>
<< Reserves

All about Pegmatite and Marl Properties

Know all about Pegmatite and Marl properties here. All properties of rocks are important as they define the type of rock and its application. Pegmatite belongs to Igneous Rocks while Marl belongs to Sedimentary Rocks.Texture of Pegmatite is Pegmatitic whereas that of Marl is Earthy. Pegmatite appears Layered, Banded, Veined and Shiny and Marl appears Rough and Dull. The luster of Pegmatite is grainy, pearly and vitreous while that of Marl is dull. Pegmatite is available in black, brown, cream, green, grey, pink, red, rust, silver, white, yellow colors whereas Marl is available in beige, brown, green, grey, white colors. The commercial uses of Pegmatite are creating artwork, jewelry, source of corundum, tourmalines, beryls and topaz and that of Marl are creating artwork, soil conditioner.

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