Midland Valley terrane (locally, structurally)

E225486

The Midland Valley terrane is a major geological block in central Scotland characterized by complex structural deformation and a history of volcanic and sedimentary basin development between the Highlands and the Southern Uplands.

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All labels observed (2)

Statements (47)

Predicate Object
instanceOf geological terrane
structural block
boundedBy Highland Boundary Fault
Southern Uplands Fault
surface form: Southern Upland Fault
contains Ayrshire Basin
Carboniferous lavas
Clyde basin
surface form: Clyde Basin

Coal Measures
Forth Basin
Old Red Sandstone
Permian basins
sedimentary basins
volcanic centers
country Scotland
developedDuring Carboniferous
Devonian
formsPhysiographicRegion Central Lowlands of Scotland
surface form: Midland Valley of Scotland
geologicalAge Paleozoic
hasCharacteristic complex structural deformation
folding
normal faulting
strike-slip faulting
hasDeformationPhase Variscan-related deformation
post-Variscan reactivation
hasEconomicResource building stone
coal
hydrocarbons
hasResearchField basin analysis
petroleum geology
structural geology
hasSedimentation deltaic deposits
fluvio-lacustrine deposits
marine incursions
hasStructuralStyle fault-bounded half-grabens
tilted fault blocks
hasVolcanism Carboniferous volcanism
Permian volcanism
locatedIn central Scotland
overlies British Caledonides
surface form: Caledonian orogenic belt
partOf British Caledonides
surface form: Scottish Caledonides
separates Highlands
Southern Uplands
structurallyBetween Grampian Terrane
surface form: Grampian terrane

Southern Uplands terrane
tectonicEvolution post-orogenic extension
strike-slip basin development
tectonicSetting post-Caledonian

Referenced by (2)

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

Southern Uplands terrane overlies Midland Valley terrane (locally, structurally)
Avalonia contains Midland Valley terrane (locally, structurally)
this entity surface form: Midlands Microcraton-related terranes