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4 Results Found

  • Article
  • Open Access
1,007 Views
14 Pages

Overprinted Metamorphic Assemblages in High-Alumina Metapelitic Rocks in Contact with Varnous Pluton (NNW Greece)

  • Foteini Aravani,
  • Lambrini Papadopoulou,
  • Antonios Koroneos,
  • Alexandros Chatzipetros,
  • Stefanos Karampelas and
  • Kyriaki Pipera

1 August 2025

The Varnous Mt. area in the northern Pelagonian Nappe is characterized by the intrusion of an Early Permian pluton, with its tectonic setting and igneous petrology well constrained in earlier studies. The metamorphic basement rocks warrant further de...

(This article belongs to the Section Mineral Geochemistry and Geochronology)
  • Article
  • Open Access
4 Citations
2,464 Views
26 Pages

This paper focuses on the structural and finite strain analysis of the Pelagonian nappe, the HP/LT Ampelakia unit, and the Olympos-Ossa unit in the Olympos-Ossa mountainous area in order to better understand the exhumation history of the Ampelakia un...

  • Review
  • Open Access
15 Citations
8,041 Views
72 Pages

In this paper, the Hellenic orogenic belt’s main geological structure and architecture of deformation are presented in an attempt to achive a better interpretation of its geotectonic evolution during Alpine orogeny. This study was based not onl...

(This article belongs to the Special Issue Advanced Studies in Structural Geology: The Role of Tectonics on Applied Geology Αspects)
  • Article
  • Open Access
1,281 Views
23 Pages

Magmatic to Subsolidus Evolution of the Variscan Kastoria Pluton (NW Greece): Constraints from Mineral Chemistry and Textures

  • Ioanna Gerontidou,
  • Antonios Koroneos,
  • Lambrini Papadopoulou,
  • Alexandros Chatzipetros,
  • Matteo Masotta and
  • Stefanos Karampelas

15 January 2026

This study focuses on the mineralogy and mineral chemistry of the accessory minerals occurring in the Kastoria pluton situated in NW Greece, which intrudes the Pelagonian nappe having crystallized during the Late Paleozoic (~300 Ma). The pluton consi...

(This article belongs to the Section Mineral Geochemistry and Geochronology)