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INTRUSIVE IGNEOUS
ROCKS
-Forms when megma intrudes in to bedrock
and slowly cools
DYKES- These cut the
bedding of rocks vertically,
hence discordant in nature
SILLS- These Spreads
parallel to the bedding
planes of the rocks ,
concordant in nature.
LACCOLITHS: It is a
concordant body, with flat
bottom and convex upward.
It is dome shaped
LOPOLITHS : These are
basin or saucer-shaped
concordant bodies with top
nearly flat and convex
bottom
LOPOLITHS
LACCOLITHS
PATHOLITHS- These are
concordant bodies that
occurs along the crests and
troughs of the folded
sedimentary strata.
BATHOLITHS: These are
the largest kind of plutons,
irregular in shape and
occupies large area.
NECK- It is cylindrical
conduit that fed magma
upward to a volcanic vent or it
is a conduit of the ancient
volcano.
BYSAMILITHS- these are
more or less vertical
cylindrical bodies that
crosscut (discordant) adjacent
sediments and are bounded by
steep faults.
THANK YOU

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Types and Structures of Intrusive Igneous Rocks

  • 1. INTRUSIVE IGNEOUS ROCKS -Forms when megma intrudes in to bedrock and slowly cools
  • 2. DYKES- These cut the bedding of rocks vertically, hence discordant in nature SILLS- These Spreads parallel to the bedding planes of the rocks , concordant in nature.
  • 3. LACCOLITHS: It is a concordant body, with flat bottom and convex upward. It is dome shaped LOPOLITHS : These are basin or saucer-shaped concordant bodies with top nearly flat and convex bottom LOPOLITHS LACCOLITHS
  • 4. PATHOLITHS- These are concordant bodies that occurs along the crests and troughs of the folded sedimentary strata. BATHOLITHS: These are the largest kind of plutons, irregular in shape and occupies large area.
  • 5. NECK- It is cylindrical conduit that fed magma upward to a volcanic vent or it is a conduit of the ancient volcano. BYSAMILITHS- these are more or less vertical cylindrical bodies that crosscut (discordant) adjacent sediments and are bounded by steep faults.