Moine Supergroup
E154085
The Moine Supergroup is a sequence of Neoproterozoic metamorphic rocks in the Scottish Highlands, notable for recording early tectonic events prior to the Caledonian orogeny.
All labels observed (2)
| Label | Occurrences |
|---|---|
| Moine Supergroup canonical | 3 |
| Moine Thrust Belt | 1 |
How this entity was disambiguated
This entity first appeared as the object of triple T1343596 — 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: Moine Supergroup Context triple: [Dalradian Supergroup, overlies, Moine Supergroup]
-
A.
Dalradian Supergroup
The Dalradian Supergroup is a thick sequence of late Precambrian to early Paleozoic metamorphic sedimentary and volcanic rocks extensively exposed in the Scottish Highlands and parts of Ireland.
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B.
Grampian Terrane
The Grampian Terrane is a major geological block in Scotland characterized by ancient metamorphic and igneous rocks that form much of the Grampian Highlands.
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C.
Coast Plutonic Complex
The Coast Plutonic Complex is a vast belt of granitic and related intrusive rocks forming the core of the Coast Mountains along the Pacific margin of western North America.
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D.
Siccar Point unconformity
The Siccar Point unconformity is a famous geological site in Scotland where dramatically tilted older rocks are overlain by younger strata, providing key evidence for deep geological time and helping to establish modern geology.
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E.
Old Red Sandstone
Old Red Sandstone is a thick sequence of Devonian-age sedimentary rocks, notable for its red coloration and widespread occurrence across parts of Scotland and other regions of the North Atlantic.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
Target entity: Moine Supergroup Target entity description: The Moine Supergroup is a sequence of Neoproterozoic metamorphic rocks in the Scottish Highlands, notable for recording early tectonic events prior to the Caledonian orogeny.
-
A.
Dalradian Supergroup
The Dalradian Supergroup is a thick sequence of late Precambrian to early Paleozoic metamorphic sedimentary and volcanic rocks extensively exposed in the Scottish Highlands and parts of Ireland.
-
B.
Grampian Terrane
The Grampian Terrane is a major geological block in Scotland characterized by ancient metamorphic and igneous rocks that form much of the Grampian Highlands.
-
C.
Coast Plutonic Complex
The Coast Plutonic Complex is a vast belt of granitic and related intrusive rocks forming the core of the Coast Mountains along the Pacific margin of western North America.
-
D.
Siccar Point unconformity
The Siccar Point unconformity is a famous geological site in Scotland where dramatically tilted older rocks are overlain by younger strata, providing key evidence for deep geological time and helping to establish modern geology.
-
E.
Old Red Sandstone
Old Red Sandstone is a thick sequence of Devonian-age sedimentary rocks, notable for its red coloration and widespread occurrence across parts of Scotland and other regions of the North Atlantic.
- F. None of above. chosen
Statements (44)
| Predicate | Object |
|---|---|
| instanceOf |
geologic unit
ⓘ
metamorphic rock sequence ⓘ supergroup ⓘ |
| ageRange | approximately 1000–800 Ma (depositional age, inferred) ⓘ |
| boundedByStructure | Moine Thrust Belt ⓘ |
| containsSubdivision |
Glenfinnan Group
ⓘ
Loch Eil Group ⓘ Morar Group ⓘ |
| country | Scotland ⓘ |
| deformationEvents |
Caledonian deformation phases
ⓘ
multiple Precambrian deformation phases ⓘ |
| exposedIn |
Northern Highlands
ⓘ
Northwest Highlands ⓘ |
| geologicAge | Neoproterozoic ⓘ |
| lithology |
gneisses
ⓘ
metasedimentary rocks ⓘ pelites ⓘ psammites ⓘ quartzites ⓘ schists ⓘ |
| locatedIn | Scottish Highlands ⓘ |
| metamorphicGrade | greenschist to amphibolite facies ⓘ |
| metamorphism | polyphase metamorphism ⓘ |
| namedAfter |
Sutherland (Scottish Highlands)
ⓘ
surface form:
A’ Mhòine (Moine) in Sutherland
|
| orogenyRecorded |
Caledonian orogeny
ⓘ
surface form:
Knoydartian orogeny
|
| overlies |
Lewisian complex basement
ⓘ
surface form:
Lewisian Gneiss Complex
|
| partOf |
British Caledonides
ⓘ
surface form:
Caledonian orogenic belt
|
| region |
northern Scotland
ⓘ
surface form:
Northern Scotland
|
| researchUse | key reference for Neoproterozoic tectonics of the North Atlantic region ⓘ |
| separatedFrom |
Moine Thrust Belt
ⓘ
surface form:
Lewisian Gneiss Complex by the Moine Thrust
|
| stratigraphicRelationship | unconformable on Lewisian basement (locally inferred) ⓘ |
| structuralStyle |
intensely folded
ⓘ
thrust imbricated ⓘ |
| studyDiscipline |
metamorphic petrology
ⓘ
stratigraphy ⓘ structural geology ⓘ tectonics ⓘ |
| tectonicSettingInferred |
Neoproterozoic sedimentary basin
ⓘ
possible rift or passive margin setting ⓘ |
| tectonicSignificance |
deformed during Caledonian orogeny
ⓘ
records pre-Caledonian tectonic events ⓘ |
| typicalMineralogy |
feldspar
ⓘ
mica ⓘ quartz ⓘ |
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: Moine Supergroup Description of subject: The Moine Supergroup is a sequence of Neoproterozoic metamorphic rocks in the Scottish Highlands, notable for recording early tectonic events prior to the Caledonian orogeny.
Referenced by (4)
Full triples — surface form annotated when it differs from this entity's canonical label.