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
This entity first appeared as the object of triple T8598399 — resolving that mention is where its identity was fixed. The disambiguator weighed these candidate entities and picked the highlighted one (or “None”, minting a new entity). This is how homonymy is resolved: the same surface form can point to different entities.
Target entity: Barrovian metamorphic zones Context triple: [George Barrow, knownFor, Barrovian metamorphic zones]
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A.
Bowen’s reaction series
Bowen’s reaction series is a conceptual model in geology that explains the sequence and conditions under which minerals crystallize from cooling magma.
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B.
Metamorphism
Metamorphism is a seminal geological text that systematically explains the processes and conditions under which rocks undergo mineralogical and structural changes within the Earth's crust.
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C.
Atlas of Microstructures in Metamorphic Rocks
Atlas of Microstructures in Metamorphic Rocks is a specialized geological reference book that illustrates and explains the microscopic textures and structures found in metamorphic rocks for research and educational use.
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D.
Peninsular Gneiss
Peninsular Gneiss is an ancient, highly metamorphosed rock formation that forms part of the geological foundation of southern India and is prominently exposed at sites like Lalbagh’s famous rock outcrop in Bengaluru.
-
E.
Damara orogeny
The Damara orogeny was a major Neoproterozoic–early Paleozoic mountain-building event in present-day Namibia associated with the assembly of the Gondwana supercontinent.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
Target entity: Barrovian metamorphic zones Target entity description: 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.
-
A.
Bowen’s reaction series
Bowen’s reaction series is a conceptual model in geology that explains the sequence and conditions under which minerals crystallize from cooling magma.
-
B.
Metamorphism
Metamorphism is a seminal geological text that systematically explains the processes and conditions under which rocks undergo mineralogical and structural changes within the Earth's crust.
-
C.
Atlas of Microstructures in Metamorphic Rocks
Atlas of Microstructures in Metamorphic Rocks is a specialized geological reference book that illustrates and explains the microscopic textures and structures found in metamorphic rocks for research and educational use.
-
D.
Peninsular Gneiss
Peninsular Gneiss is an ancient, highly metamorphosed rock formation that forms part of the geological foundation of southern India and is prominently exposed at sites like Lalbagh’s famous rock outcrop in Bengaluru.
-
E.
Damara orogeny
The Damara orogeny was a major Neoproterozoic–early Paleozoic mountain-building event in present-day Namibia associated with the assembly of the Gondwana supercontinent.
- F. None of above. chosen
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 NERFINISHED ⓘ |
| contrastsWith |
high-pressure blueschist facies metamorphism
ⓘ
low-pressure Buchan-type metamorphism ⓘ |
| developedFrom | field mapping of index minerals ⓘ |
| developedIn | Scottish Highlands NERFINISHED ⓘ |
| 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 NERFINISHED ⓘ |
| 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 GENERATED ⓘ |
| 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
The pipeline generated the facts above by prompting gpt-5.1 with this entity's name + description and the instruction below.
You are a knowledge base construction expert. Given a subject entity and a description of it, return factual statements that you know for the subject as a JSON list of dictionaries(triples), where keys must be "subject", "predicate" and "object". The number of facts may be very high, between 25 to 50 or more, for very popular subjects. For less popular subjects, the number of facts can be very low, like 5 or 10. # Requirements - If you don't know the subject at all, return an empty list. - If the subject is not a named entity, return an empty list. - Include at least one triple where predicate is "instanceOf". - Do not get too wordy. - Separate several objects into multiple triples with one object.
Subject: Barrovian metamorphic zones Description of subject: 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.
Referenced by (1)
Full triples — surface form annotated when it differs from this entity's canonical label.