Southern Pyrenees axial zone

E951955

The Southern Pyrenees axial zone is the central, geologically oldest core of the Pyrenees mountain range, composed mainly of heavily deformed and metamorphosed rocks that form its highest and most rugged peaks.

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Observed surface forms (1)

Surface form Occurrences
central Pyrenees 1

Statements (40)

Predicate Object
instanceOf geological region
structural zone
boundedBy North Pyrenean Zone NERFINISHED
South Pyrenean Zone NERFINISHED
characterizedBy metamorphism
oldest rocks of the Pyrenees
rugged topography
strong deformation
composedMostlyOf igneous rocks
metamorphic rocks
contains gneiss complexes
granite plutons
highest peaks of the Pyrenees
schist sequences
exposes deep crustal levels
extendsAlong east–west axis of the Pyrenees
formedBy convergence of Iberian and Eurasian plates
formedDuring Pyrenean orogeny NERFINISHED
forms backbone of the Pyrenees
central core of the Pyrenees
geologicalAge Paleozoic basement
hasMetamorphicGrade medium- to high-grade metamorphism
hasStructuralStyle intense folding
thrust faulting
importantFor study of Alpine orogeny
study of Variscan basement
isSubjectOf metamorphic petrology studies
structural geology studies
tectonic evolution studies
locatedIn Andorra NERFINISHED
France
Southern Pyrenees NERFINISHED
Spain
orogenType collisional mountain belt core
overlainBy Mesozoic cover units at margins
partOf Pyrenees NERFINISHED
relatedTo Eurasian plate NERFINISHED
Iberian plate NERFINISHED
separates northern foreland from southern foreland of the Pyrenees
tectonicRole axial core of Pyrenean orogen

Referenced by (2)

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

Maladeta massif partOf Southern Pyrenees axial zone
Montes Malditos (massif high point context) locatedIn Southern Pyrenees axial zone
subject surface form: Montes Malditos
this entity surface form: central Pyrenees