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The 36 pages that link to Metamorphic rock, each with the reason it gives.

• LimestoneNarrower topic: Heat and pressure can transform limestone into marble.

• Sedimentary rockCompared with: It changes in the solid state, whereas sedimentary rock forms through deposition or precipitation.

• GraphiteNarrower topic: Many natural graphite deposits form when carbon-rich rocks undergo metamorphism.

• Igneous rockCompared with: Metamorphism alters solid rock, whereas igneous formation involves molten material.

• Canadian ShieldRelated: Many Shield rocks record intense heat and pressure deep within ancient crust.

• MarbleNarrower topic: Marble is the carbonate-rich product of metamorphic change.

• Metamorphic gradeNarrower topic: Metamorphic rocks preserve the mineral and textural evidence used to estimate grade.

• Rock cycleRelated: Burial and tectonic forces transform existing rocks into metamorphic rock.

• CorundumNarrower topic: Corundum commonly forms when aluminum-rich rocks undergo metamorphism.

• LithologyBroader topic: Its foliation, mineral assemblages, and grain textures define distinctive lithologies.

• PetrographyNarrower topic: Its mineral assemblages and fabrics record metamorphic conditions and history.

• FoliationNarrower topic: Foliation is a fabric found chiefly in metamorphic rocks.

• InosilicateNarrower topic: Metamorphism can create or modify amphibole-bearing inosilicate assemblages.

• ProtolithCompared with: A protolith is the precursor; metamorphic rock is the transformed product.

• Rubidium–strontium datingRelated: Mineral isochrons can date metamorphism or later isotopic equilibration.

• SchistNarrower topic: Schist forms through metamorphism rather than direct cooling from a melt.

• Volcanic rockCompared with: It changes from preexisting rock rather than forming directly from erupted melt.

• Lapis lazuliNarrower topic: Lapis lazuli is classified by the geological alteration that formed it.

• RutileNarrower topic: Rutile commonly crystallizes or recrystallizes during metamorphism.

• DiopsideNarrower topic: Diopside develops in metamorphic settings where suitable calcium-, magnesium-, and silica-bearing minerals react.

• FluorapatiteNarrower topic: Fluorapatite can persist or recrystallize during metamorphism.

• HornblendeNarrower topic: Hornblende occurs in metamorphic rocks such as amphibolite.

• MigmatiteNarrower topic: Migmatite retains metamorphic rock alongside material crystallized from melt.

• MyloniteNarrower topic: Mylonite is a metamorphic rock whose distinctive fabric reflects intense deformation.

• PorphyroblastNarrower topic: Porphyroblasts form as part of mineral changes within metamorphic rocks.

• BiotiteRelated: Biotite is common in metamorphic rocks and can indicate conditions of formation.

• HornfelsNarrower topic: Hornfels is one dense, fine-grained member of this broad rock family.

• RecrystallizationRelated: Its mineral grains commonly record recrystallization during metamorphism.

• BrookiteRelated: Brookite occurs in some metamorphic rocks and mineral veins.

• CobaltiteNarrower topic: Cobaltite also occurs in deposits shaped by metamorphism and fluid movement.

• Extrusive rockCompared with: It forms by solid-state change rather than lava cooling at the surface.

• PhylliteNarrower topic: Phyllite is a foliated metamorphic rock produced from an earlier fine-grained rock.

• StauroliteNarrower topic: Staurolite typically crystallizes during metamorphism rather than in ordinary igneous settings.

• BoudinageNarrower topic: Many classic boudinage structures occur in metamorphic rocks deformed at depth.

• LoellingiteNarrower topic: Metamorphic deposits provide another setting for loellingite occurrence.

• Clastic rockCompared with: Clastic rocks can supply the parent material later transformed into metamorphic rock.