Purbeck–Isle of Wight Fault Zone

E930713

The Purbeck–Isle of Wight Fault Zone is a prominent structural fault system in southern England that strongly influenced the geological evolution and deformation of the Wessex region.

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Statements (38)

Predicate Object
instanceOf geological fault zone
structural lineament
affectedBy Alpine orogeny NERFINISHED
associatedWith monoclinal structures on the Isle of Purbeck
monoclinal structures on the Isle of Wight
controls basin architecture of the Wessex Basin
distribution of Mesozoic sediments in southern England
country United Kingdom
deformationStyle fault-related folding
tilting of fault blocks
extendsFrom Isle of Purbeck NERFINISHED
extendsTo Isle of Wight NERFINISHED
geologicalPeriodActivity Cretaceous NERFINISHED
Jurassic
influencedRegion Wessex region NERFINISHED
influences present-day topography of the Isle of Purbeck
present-day topography of the Isle of Wight
structural evolution of the Isle of Purbeck
structural evolution of the Isle of Wight
laterReactivationStyle inversion
lithologyInfluence controls thickness variations in Mesozoic sedimentary sequences
locatedIn Wessex Basin NERFINISHED
southern England
movementType normal faulting during basin development
reverse or thrust reactivation during inversion
orientation approximately east–west striking
partOf onshore continuation of structural trends in the English Channel
reactivatedIn Cenozoic
relatedTo Portland–Wight structural trend
Weymouth Anticline NERFINISHED
researchField basin analysis
structural geology
tectonics
significance key structure in the tectonic evolution of the Wessex Basin
major control on regional deformation in southern England
tectonicRole boundary between different structural domains in the Wessex Basin
tectonicSetting Mesozoic extensional basin margin
trend east–west

Referenced by (1)

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

Wessex Basin majorFaultSystem Purbeck–Isle of Wight Fault Zone