That is a difficult question. It is unlikely there is much textural difference. It might be necessary to study chemical zoning. One possibility is that garnets in an igneous rock might be xenocrysts.
The most important difference between metamorphic and igneous garnets lies in their formation processes and resulting characteristics:
Formation Process:Metamorphic Garnets: These garnets form under high pressure and temperature conditions during the metamorphism of pre-existing rocks. They are commonly found in schists, gneisses, and other metamorphic rocks1. Igneous Garnets: These garnets crystallize directly from magma. They are typically found in igneous rocks such as granites, pegmatites, and some ultramafic rocks1.
Chemical Composition:Metamorphic Garnets: Often show compositional zoning due to changes in pressure and temperature during their growth. This zoning can provide valuable information about the metamorphic history of the host rock2. Igneous Garnets: Generally have a more uniform composition, reflecting the relatively stable conditions of crystallization from a cooling magma
Formation Environment is the key difference between metamorphic & Igneous Garnets.
Metamorphic Garnets form under intense heat and pressure deep within the Earth's crust.They are commonly found in metamorphic rocks like gneiss, schist, and granulite.
Igneous Garnets form from the solidification of molten rock (magma or lava) found in igneous rocks like granites, pegmatites, and peridotites.
Metamorphic garnets often contain inclusions of other minerals,But igneous garnets may have a more homogenous composition.