Barrovian metamorphic zones

E744753

Barrovian metamorphic zones are a classic sequence of regional metamorphic grade zones in pelitic rocks, widely used as a model for understanding progressive metamorphism in orogenic belts.

All labels observed (1)

Label Occurrences
Barrovian metamorphic zones canonical 1

How this entity was disambiguated

Statements (46)

Predicate Object
instanceOf metamorphic zonation model ⓘ
regional metamorphism concept ⓘ
appliesTo orogenic belts ⓘ
pelitic rocks ⓘ
associatedWith medium pressure metamorphism ⓘ
medium temperature metamorphism ⓘ
assumes compositionally similar pelitic protoliths ⓘ
equilibrium mineral assemblages ⓘ
basedOn index minerals ⓘ
canonicalExample classic Scottish Barrovian sequence ⓘ
characterizes progressive regional metamorphism ⓘ
contrastedWith Buchan metamorphic zones ⓘ
contrastsWith high-pressure blueschist facies metamorphism ⓘ
low-pressure Buchan-type metamorphism ⓘ
developedFrom field mapping of index minerals ⓘ
developedIn Scottish Highlands ⓘ
documentedIn metamorphic petrology textbooks ⓘ
field geology ⓘ
metamorphic petrology ⓘ
formsPartOf classical metamorphic zonation schemes ⓘ
hasZone biotite zone ⓘ
chlorite zone ⓘ
garnet zone ⓘ
kyanite zone ⓘ
sillimanite zone ⓘ
staurolite zone ⓘ
helpsConstrain depth of metamorphism ⓘ
thermal structure of orogenic belts ⓘ
timing of metamorphic events ⓘ
indexMineralSequence chlorite to biotite to garnet to staurolite to kyanite to sillimanite ⓘ
influenced classification of regional metamorphism ⓘ
namedAfter George Barrow ⓘ
relatedConcept metamorphic facies ⓘ
metamorphic isograds ⓘ
pressure–temperature paths ⓘ
represents increasing metamorphic grade sequence ⓘ
requires mineralogical mapping across regional transects ⓘ
timePeriod early 20th century ⓘ
typicalRockType metapelite ⓘ
typicalTectonicSetting collisional orogen ⓘ
usedBy metamorphic petrologists ⓘ
structural geologists ⓘ
usedFor interpreting pressure–temperature conditions ⓘ
mapping metamorphic grade ⓘ
reconstructing metamorphic field gradients ⓘ
teaching progressive metamorphism ⓘ

How these facts were elicited

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

George Barrow → knownFor → Barrovian metamorphic zones ⓘ