Barrovian metamorphism

E744754

Barrovian metamorphism is a classic regional metamorphic sequence characterized by systematically increasing metamorphic grade and index minerals with depth, first documented in the Scottish Highlands.

All labels observed (1)

Label Occurrences
Barrovian metamorphism canonical 1

How this entity was disambiguated

Statements (47)

Predicate Object
instanceOf geological process ⓘ
metamorphic facies series ⓘ
regional metamorphism ⓘ
associatedWith crustal thickening ⓘ
fold and thrust belts ⓘ
medium pressure metamorphism ⓘ
moderate geothermal gradient ⓘ
characterizedBy progressive development of index minerals ⓘ
systematic increase in metamorphic grade with depth ⓘ
contrastedWith Buchan metamorphism ⓘ
high-pressure metamorphism ⓘ
controlledBy pressure-temperature-time paths ⓘ
developsIn regional crustal scale ⓘ
documentedBy George Barrow ⓘ
educationalUse type example of regional metamorphism ⓘ
firstDocumentedIn Scottish Highlands ⓘ
forms metamorphic zones named after index minerals ⓘ
hasKeyConcept index mineral zones ⓘ
isograds ⓘ
historicalSignificance first systematic mapping of metamorphic zones ⓘ
indexMineralSequenceIncludes biotite ⓘ
chlorite ⓘ
garnet ⓘ
kyanite ⓘ
sillimanite ⓘ
staurolite ⓘ
linkedTo deformation during orogeny ⓘ
regional heat flow increase ⓘ
metamorphicGradeProgression low grade to high grade ⓘ
namedAfter George Barrow ⓘ
occursIn metamorphic terranes worldwide ⓘ
pressureTemperatureCharacteristic intermediate pressure ⓘ
intermediate temperature ⓘ
relatedConcept metamorphic facies ⓘ
metamorphic grade ⓘ
orogenic metamorphism ⓘ
requires burial to mid-crustal depths ⓘ
spatialPattern roughly parallel isograds across a region ⓘ
timeOfRecognition early 20th century ⓘ
typicalMineralAssemblage quartz-plagioclase-biotite-garnet in pelites ⓘ
typicalProtolith mudstones ⓘ
pelitic sedimentary rocks ⓘ
shales ⓘ
typicalTectonicSetting continental collision zone ⓘ
orogenic belt ⓘ
usedFor interpreting tectonometamorphic evolution ⓘ
mapping metamorphic zones ⓘ

How these facts were elicited

Referenced by (1)

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

George Barrow → notableConcept → Barrovian metamorphism ⓘ