Pelagonian Zone

E679499

The Pelagonian Zone is a major geological unit in the central Balkans characterized by ancient metamorphic and sedimentary rocks that form part of the internal Hellenide mountain belt.

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Statements (45)

Predicate Object
instanceOf geological terrane
geological zone
tectonostratigraphic unit
boundedBy Pindos Zone NERFINISHED
Vardar Zone NERFINISHED
composedOf metamorphic rocks
sedimentary rocks
contains dolomite
gneiss
limestone
marble
schist
extendsInto Albania NERFINISHED
formedDuring closure of the Tethys Ocean
geologicalAge Mesozoic
Paleozoic
hasDeformationPhase multiple Alpine deformation phases
hasEconomicGeology industrial minerals
marble resources
hasFossils Mesozoic marine fossils
hasMetamorphicGrade low- to medium-grade metamorphism
hasRockType metasedimentary rocks
metavolcanic rocks
hasStratigraphy Paleozoic basement with Mesozoic cover
hasStructuralStyle nappe structures
thrust tectonics
isKeyFor reconstruction of Tethyan paleogeography
understanding Hellenide tectonic evolution
isPartOf Alpine–Himalayan orogenic belt NERFINISHED
liesBetween External Hellenides and Vardar Zone NERFINISHED
locatedIn Greece
North Macedonia NERFINISHED
central Balkans
namedAfter Pelagonia NERFINISHED
orogeny Alpine orogeny NERFINISHED
overlies basement rocks
paleogeographicOrigin Cimmerian continent fragment
partOf Hellenides NERFINISHED
internal Hellenides
researchField geology
stratigraphy
tectonics
structuralPosition internal zone of the Hellenide orogen
tectonicSetting continental fragment
microcontinental block

Referenced by (1)

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

Hellenides contains Pelagonian Zone