Yes, thermal metamorphism would be occurring here. This develops adjacently from the point where the rock wall and intrusion meet.
Since heat always moves from hotter to colder materials, it flows from the magma into the wall rock. As a result, the wall rock heats up while the magma cools and solidifies. Additionally, both the intrusion and the wall rock are permeable to hydrothermal fluids. Contact When a hot magma intrusion heats up rock, metamorphism occurs.
Mudstone, carbonate, clastic, and igneous rocks are the primary types of original rock that undergo thermal contact metamorphism and can produce a variety of thermal contact metamorphic rock types.
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