Sill (D)
the country rock
A Sill is formed when a fluid rock (usually magma but it can be mud or salt) is squeezed in between the layers (usually horizontal) of older rocks before it solidifies in place. A Dike or Dyke is the opposite, here the fluid rock penetrates across the layering of the older rocks. Logically to get the material to form a Sill there must be an accompanying feeder Dyke.
sill
the type of thin pluton thats cuts across preexisting layers of rocks is Dike.
Hornfels
Sill (D)
Sill (D)
sill
sill
the country rock
yes sill is one of a sedimentary rocks
A Sill is formed when a fluid rock (usually magma but it can be mud or salt) is squeezed in between the layers (usually horizontal) of older rocks before it solidifies in place. A Dike or Dyke is the opposite, here the fluid rock penetrates across the layering of the older rocks. Logically to get the material to form a Sill there must be an accompanying feeder Dyke.
its acutally a dike trust me
sill
A magma sill is a planar sheet of magma which is parallel to the surrounding rock.
An vertical intrusion of magma in a pre-existing rock formation is known as a dike.