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 NAME-BIRENDRA KUMAR
 ROLL NO-14121072
 BRANCH-MINING 3rdsem.
 SUBJECT- PROPERTIES OF ROCKS.
9/30/2015 1
 color
 Texture
 Structure
 Mineral composition
 origin
9/30/2015 2
a. Leucocrative; this type of rocks have light
color .
b. Mesocrative; this type of rocks occur in
medium dark colur.
c. Melamocrative; this type of rocks ocour in dark
colour.
9/30/2015 3
1.Degree of crystallization
a.Holocrystalline ; when a rock is made of
entirely of crystals.
9/30/2015 4
Fig;1 Fig;2
9/30/2015 5
9/30/2015 6
The size of grains in an igneous rock varies
considerable. The slow cooling gives crystals
time to grow to size greater than 5mm.In
rapid cooling, the mineral grains crystallize
quickly as a mass of tiny crystals which are
generally less than 1mm in size. In some
laves, the is so rapid that they fail to
crystallize and “glassy texture”results.
9/30/2015 7
3. Shap of the crystal; the grains of an
igneous rock are called “euhedral” if
they show developed crystal faces,
and if the crystal faces are partly
developed, they are described as
“subhedral”.
9/30/2015 8
4. Mutual relations of grains ;
They are following types;
A. Equigranular
a.panidiomorphic texture; when most
of the grains are euhedra.ex-
lamprophyres.
b.Hypidiomorphic texture; hen most of
the crystals are subhedral.ex-granite
and syenites.
9/30/2015 9
e. Orthophyric texture; some highly
rocks such as orthophyres and
plagiophyers.
f. felsitic texture; An igneous rocks
containing a uniform mass of
cryptocrystalline matter. 9/30/2015 10
9/30/2015 11
d. Intergranular and instersertal texture ;in
many basalts plagioclase laths occur in such
away that they form a network with triangular
or polygonal interspaces.
9/30/2015 12
9/30/2015 13
9/30/2015 14
9/30/2015 15
 Flow structure;  Xenolith structure
9/30/2015 16
9/30/2015 17
9/30/2015 18
 Extrusive; extrusive
igneous rock
bodies are formed
from magma
poured out at the
surface. ex-
lavaflows
 Instrusive; these
types of bodies are
formed by the
consolidation of
magma at some
depth below the
earth surface. Ex-
batholith
9/30/2015 19
Batholit lopolith
9/30/2015 20
9/30/2015 21
9/30/2015 22
9/30/2015 23
 Nature
 Texture
a. Grain size
b. Roundness
c. Sorting
d. Packing
 structures
9/30/2015 24
 Clastic sediments; clastic rocks are formed by
the mechanical accumulation of grains of
clastic sediments.
Depending upon the size of constituent
grains they are following types-
 Rudaceous rocks; these rocks are formed by
accumulation of bigger rocks fragments such
as gravels, pebbles and boulders.
 Arenaceous rocks ; these rocks are composed
almost entirely of and grains . Ex -sandstone
 Argillaceous rocks; these rocks are made up
of very fine grained sediments. Ex-shale
9/30/2015 25
Sand stone shale
Conglomerate
9/30/2015 26
1.Carbonate rocks, limestone 2.Salt rocks, gypsum
9/30/2015 27
4. Siliceous rocks, jaspar flint
3.Ferruginous rocks, siderite
9/30/2015 28
2.Biochemical rcks,shell -
limestone
1.Organic rocks, coal
9/30/2015 29
 Grain size
Grade Grain size (mm) Rock type
Pebble grave 10 and above
2-10
conglomerate
sand 0.1-2 sandstone
silt 0.01-0.1 siltstone
clay Less than 0.01 shale
9/30/2015 30
It is related to grain size.
9/30/2015 31
 Stratification ; all the sedimentary rocks are,
in general, characterized by “stratification”.
deposition of sediments into layers or beds is
called stratification.
 Lamination ;the bedding, less than one
centimeter in thickness, are called
“lamination”.
9/30/2015 32
9/30/2015 33
9/30/2015 34
 Colour
 Texture
 Structure
9/30/2015 35
a. Leucocrative; this type of rocks have light
colour .
b. Mesocrative; this type of rocks occur in
medium dark colour.
c. Melamocrative; this type of rocks occour in
dark colour.
9/30/2015 36
 Crystalloblastic texture; the holocrystalline
texture of metamorphic rocks is called the
“crysalloblastic texture” .this type of of
texture develop s due to recrystallisation of
minerals grains in the solid medium.the
crystals showing perfect crystal outline, are
called the “idioblastic” while those which do
not have any definite shape, are described as
“xenoblastic”.
9/30/2015 37
 Granoblastic texture; in a metamorphic rock if
the major constituents are granular or
equidimensional, the texture is called
“granoblastic”.
 Palimpest texture; the remnant texture of the
parents rock found preserved in the metamorphic
rock, is called “palimpest texture”.
9/30/2015 38
Porphyroblastic texture
granoblastic
9/30/2015 39
 Cataclastic structure;
These rocks are formed mainly under the
influence of shearing stresses in the upper
zones of the earth’s crust.
 Maculose structure; when argillaceous
rocks are subjected to contact
metamorphism, a spotted rock is formed in
areas where incomplete recrystalization
takes place.
9/30/2015 40
 Schistose structure ; the foliation of schists is
called “schistosity”.
 Gneissoses structure; such a coarse grained
metamorphic rocks showing baned or
streaked appearance, is called “gneiss”and its
structure is called the “gneissose structure”.
9/30/2015 41
 Hornfelsic structure; this type of rocks is
formed due to the predominance of
equidimentional minerals such as felspar,
andalusite, cordierite, and quartz.
9/30/2015 42
THANKS,
9/30/2015 43

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Presentation1

  • 1.  NAME-BIRENDRA KUMAR  ROLL NO-14121072  BRANCH-MINING 3rdsem.  SUBJECT- PROPERTIES OF ROCKS. 9/30/2015 1
  • 2.  color  Texture  Structure  Mineral composition  origin 9/30/2015 2
  • 3. a. Leucocrative; this type of rocks have light color . b. Mesocrative; this type of rocks occur in medium dark colur. c. Melamocrative; this type of rocks ocour in dark colour. 9/30/2015 3
  • 4. 1.Degree of crystallization a.Holocrystalline ; when a rock is made of entirely of crystals. 9/30/2015 4
  • 7. The size of grains in an igneous rock varies considerable. The slow cooling gives crystals time to grow to size greater than 5mm.In rapid cooling, the mineral grains crystallize quickly as a mass of tiny crystals which are generally less than 1mm in size. In some laves, the is so rapid that they fail to crystallize and “glassy texture”results. 9/30/2015 7
  • 8. 3. Shap of the crystal; the grains of an igneous rock are called “euhedral” if they show developed crystal faces, and if the crystal faces are partly developed, they are described as “subhedral”. 9/30/2015 8
  • 9. 4. Mutual relations of grains ; They are following types; A. Equigranular a.panidiomorphic texture; when most of the grains are euhedra.ex- lamprophyres. b.Hypidiomorphic texture; hen most of the crystals are subhedral.ex-granite and syenites. 9/30/2015 9
  • 10. e. Orthophyric texture; some highly rocks such as orthophyres and plagiophyers. f. felsitic texture; An igneous rocks containing a uniform mass of cryptocrystalline matter. 9/30/2015 10
  • 12. d. Intergranular and instersertal texture ;in many basalts plagioclase laths occur in such away that they form a network with triangular or polygonal interspaces. 9/30/2015 12
  • 16.  Flow structure;  Xenolith structure 9/30/2015 16
  • 19.  Extrusive; extrusive igneous rock bodies are formed from magma poured out at the surface. ex- lavaflows  Instrusive; these types of bodies are formed by the consolidation of magma at some depth below the earth surface. Ex- batholith 9/30/2015 19
  • 24.  Nature  Texture a. Grain size b. Roundness c. Sorting d. Packing  structures 9/30/2015 24
  • 25.  Clastic sediments; clastic rocks are formed by the mechanical accumulation of grains of clastic sediments. Depending upon the size of constituent grains they are following types-  Rudaceous rocks; these rocks are formed by accumulation of bigger rocks fragments such as gravels, pebbles and boulders.  Arenaceous rocks ; these rocks are composed almost entirely of and grains . Ex -sandstone  Argillaceous rocks; these rocks are made up of very fine grained sediments. Ex-shale 9/30/2015 25
  • 27. 1.Carbonate rocks, limestone 2.Salt rocks, gypsum 9/30/2015 27
  • 28. 4. Siliceous rocks, jaspar flint 3.Ferruginous rocks, siderite 9/30/2015 28
  • 30.  Grain size Grade Grain size (mm) Rock type Pebble grave 10 and above 2-10 conglomerate sand 0.1-2 sandstone silt 0.01-0.1 siltstone clay Less than 0.01 shale 9/30/2015 30
  • 31. It is related to grain size. 9/30/2015 31
  • 32.  Stratification ; all the sedimentary rocks are, in general, characterized by “stratification”. deposition of sediments into layers or beds is called stratification.  Lamination ;the bedding, less than one centimeter in thickness, are called “lamination”. 9/30/2015 32
  • 35.  Colour  Texture  Structure 9/30/2015 35
  • 36. a. Leucocrative; this type of rocks have light colour . b. Mesocrative; this type of rocks occur in medium dark colour. c. Melamocrative; this type of rocks occour in dark colour. 9/30/2015 36
  • 37.  Crystalloblastic texture; the holocrystalline texture of metamorphic rocks is called the “crysalloblastic texture” .this type of of texture develop s due to recrystallisation of minerals grains in the solid medium.the crystals showing perfect crystal outline, are called the “idioblastic” while those which do not have any definite shape, are described as “xenoblastic”. 9/30/2015 37
  • 38.  Granoblastic texture; in a metamorphic rock if the major constituents are granular or equidimensional, the texture is called “granoblastic”.  Palimpest texture; the remnant texture of the parents rock found preserved in the metamorphic rock, is called “palimpest texture”. 9/30/2015 38
  • 40.  Cataclastic structure; These rocks are formed mainly under the influence of shearing stresses in the upper zones of the earth’s crust.  Maculose structure; when argillaceous rocks are subjected to contact metamorphism, a spotted rock is formed in areas where incomplete recrystalization takes place. 9/30/2015 40
  • 41.  Schistose structure ; the foliation of schists is called “schistosity”.  Gneissoses structure; such a coarse grained metamorphic rocks showing baned or streaked appearance, is called “gneiss”and its structure is called the “gneissose structure”. 9/30/2015 41
  • 42.  Hornfelsic structure; this type of rocks is formed due to the predominance of equidimentional minerals such as felspar, andalusite, cordierite, and quartz. 9/30/2015 42