Moine Thrust Belt

E161857

The Moine Thrust Belt is a major geological structure in northwest Scotland where ancient rocks were pushed westward over younger rocks, forming one of the world’s classic examples of a thrust fault zone.

All labels observed (4)

Label Occurrences
Moine Thrust Belt canonical 2
Dalradian Basin 1
Lewisian Gneiss Complex by the Moine Thrust 1

How this entity was disambiguated

Statements (49)

Predicate Object
instanceOf geological structure
tectonic feature
thrust belt
ageRange Paleozoic
country Scotland
United Kingdom
deformationFeatures fault gouge
fold–thrust relationships
mylonites
deformationType compressional tectonics
displacementStyle thin-skinned thrusting
exposedAt Assynt
Durness area
Knockan Crag
Loch Eriboll
extendsFrom Loch Eriboll
extendsTo Loch Carron area
Skye
hasFeature Ben More Thrust
Moine Thrust Belt self-linksurface differs
surface form: Moine Thrust

Sgurr Beag Thrust
hasStatus internationally important geological site
lithologyInvolved limestones
metamorphic rocks
sandstones
shales
locatedIn Scottish Highlands
northwest Scotland
mainDeformationAge Silurian
mappingPeriod late 19th century
maximumHorizontalDisplacement tens of kilometres
movementDirection westward
olderRockUnit Moine Supergroup
orogeny Caledonian orogeny
partOf British Caledonides
surface form: Caledonian orogenic belt
significance classic example of a thrust fault zone
key area in the development of modern structural geology
structuralStyle duplex structures
stack of imbricate thrust sheets
studiedBy Ben Peach
British Geological Survey
surface form: Geological Survey of Great Britain

John Horne
tectonicSetting convergent plate margin
usedFor field training for geologists
teaching structural geology
youngerRocksOverriddenBy older rocks
youngerRockUnit Cambrian sedimentary rocks
Lewisian Gneiss Complex basement overlain by sediments
Ordovician sedimentary rocks

How these facts were elicited

Referenced by (5)

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

Caledonian fault system hasPart Moine Thrust Belt
Moine Supergroup separatedFrom Moine Thrust Belt
this entity surface form: Lewisian Gneiss Complex by the Moine Thrust
Moine Supergroup boundedByStructure Moine Thrust Belt
Appin Group tectonicSetting Moine Thrust Belt
this entity surface form: Dalradian Basin
Moine Thrust Belt hasFeature Moine Thrust Belt self-linksurface differs
this entity surface form: Moine Thrust