The intrusion is younger than the overlying sedimentary rock.
No, igneous rocks can be used in this way based on the fact that an igneous intrusion will be younger than the material through which it passes. This is part of the principle of cross cutting relationships.
Increase the pressure and temperature by burying them; or heat them with an igneous intrusion.
Intrusive igneous bodies that cut across existing sedimentary beds are said to be discordant. An example of a discordant intrusion is a batholith.
Basically, igneous intrusion involves the solidifying of magma when it cools in the crust of the Earth. When magma rises through the crust, it intrudes into the existing sedimentary rock layers and forms a hill. The surounding rock may be more prone to erosion and wear away leaving the intrusion jutting above the (eroded) surroundings.
its igneous and sedimentary and metamorphic
A laccolith is an igneous formation between two sedimentary layers
In dikes and sills.
No, igneous rocks can be used in this way based on the fact that an igneous intrusion will be younger than the material through which it passes. This is part of the principle of cross cutting relationships.
Increase the pressure and temperature by burying them; or heat them with an igneous intrusion.
It is younger than them.
It is younger.
It is younger.
the rock layers were eroded at the interface between the igneous intrusion and the sedimentary rocks.
Intrusive igneous bodies that cut across existing sedimentary beds are said to be discordant. An example of a discordant intrusion is a batholith.
law of crosscutting relationships.
In simple terms...undergoing additional heat and pressure from a more recent igneous intrusion which change the structure and minerology.
In simple terms...undergoing additional heat and pressure from a more recent igneous intrusion which change the structure and minerology.