Batholith
That depends! If the fault line cross cuts the igneous intrusion causing the intrusion to be displaced on either side of the fault and forming a broken mass of rock within the intrusion known as a fault breccia then the fault is younger than the intrusions, as the intrusion must have already existed for the fault to cause it's displacement. If on the other hand the igneous intrusion cross cuts the fault and is un-deformed then it is probable that it is younger than the fault.
a dome mountain is formed
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The intrusion is younger than the overlying sedimentary rock.
Batholith is the name for a huge igneous intrusion.
"layering" As in "layered" igneous intrusion.
If it is above it, the rock layer came after the intrusion. if the intrusion went through the rock layer is older because they layer had to be there in order for the intrusion to go through.
igneous rock
Batholith
The minerals had longer to form from the hot magma than did the minerals in the small intrusion, which would have cooled much faster.
That depends! If the fault line cross cuts the igneous intrusion causing the intrusion to be displaced on either side of the fault and forming a broken mass of rock within the intrusion known as a fault breccia then the fault is younger than the intrusions, as the intrusion must have already existed for the fault to cause it's displacement. If on the other hand the igneous intrusion cross cuts the fault and is un-deformed then it is probable that it is younger than the fault.
An igneous intrusion is younger than the rock into which it intruded.
In dikes and sills.
The largest type of intrusion is the pluton.
The antonym for batholith is small igneous intrusion or dyke.
A laccolith is an igneous formation between two sedimentary layers