Implications of salt diapirism in syn-depositional architecture of a carbonate margin-to-Edge transition: an example from Plataria Syncline, Ionian Zone, NW Greece

I Vakalas, S Kokkalas, P Konstantopoulos, C Tzimeas… - Applied Sciences, 2023 - mdpi.com
The present study examines the imprint of salt tectonics on carbonate depositional patterns
of the Ionian zone platform edge to slope transition. The study area is part of an overturned …

Petrographic characteristics of sandstones as a basis to evaluate their suitability in construction and energy storage applications. a case study from klepa nafpaktias …

P Petrounias, PP Giannakopoulou, A Rogkala… - Energies, 2020 - mdpi.com
This study investigates how the petrographic features of Klepa Nafpaktias sandstones affect
their behavior in construction applications such as concrete, in environmental applications …

Controls on sedimentation in a deep‐water foredeep: Central Pindos foreland basin, western Greece

C Botziolis, AG Maravelis, O Catuneanu, A Zelilidis - Basin Research, 2024 - earthdoc.org
This study provides a sedimentological, stratigraphic and palaeocurrent investigation of
Upper Eocene to Lower Oligocene deep‐sea fan deposits found in the central part of the …

Sedimentary Characteristics and Basin Evolution of a Compartmentalized Foreland Basin—Internal Ionian Zone, Western Greece

I Vakalas, E Tripsanas, C Tzimeas, P Konstantopoulos - Energies, 2024 - mdpi.com
This study is based on the detailed sedimentological analysis of eleven sections and one
well through the late Eocene–Oligocene flysch formation of the Internal Ionian Zone (IIZ) in …

Statistical analysis of turbidite bed thickness patterns from the Alpine fold and thrust belt of western and southeastern Greece

G Pantopoulos, I Vakalas, A Maravelis, A Zelilidis - Sedimentary Geology, 2013 - Elsevier
A statistical evaluation of turbidite bed thickness was performed for 11 turbidite successions
which constitute part of foreland basins formed along the Alpine fold and thrust belt of …

Sedimentation of submarine fan deposits in the Pindos foreland basin, from late Eocene to early Oligocene, west Peloponnesus peninsula, SW Greece

PA Konstantopoulos, A Zelilidis - Geological Journal, 2013 - Wiley Online Library
Turbidite facies distribution and palaeocurrent analysis of submarine fan evolution in the
Pindos foreland basin of west Peloponnesus peninsula (SW Greece) indicate that this part of …

[HTML][HTML] Provenance analysis of Eocene–Oligocene turbidite deposits in Pindos Foreland Basin, fold and thrust belt of SW Greece: constraints from framework …

PA Konstantopoulos, A Zelilidis - Arabian Journal of Geosciences, 2013 - Springer
Abstract The provenance of Eocene–Oligocene turbidites from the Pindos Foreland Basin,
SW Greece, has been constrained using petrographical and geochemical techniques …

[PDF][PDF] The geodynamic evolution of Pindos foreland basin in SW Greece

P Konstantopoulos, A Zelilidis - Episodes Journal of International …, 2012 - episodes.org
Abstract The distribution of Eocene-Oligocene turbidite facies in the Pindos foreland and the
paleocurrent directions of submarine fan deposits, of the Peloponnesus area, document the …

Provenance of flysch sediments and the palaeogene-Early Miocene Geodynamic evolution of the Hellenides: a contribution from heavy mineral investigations

P Faupl, A Pavlopoulos, G Migiros - Developments in Sedimentology, 2007 - Elsevier
Abstract The Palaeogene-Early Miocene geodynamic evolution of the Hellenides is
characterised by widespread flysch deposition. In the Pelagonian, Parnassos-Ghiona and …

[PDF][PDF] Preliminary data about sporadic permafrost on Peristeri and Tzoumerka massifs

G PALMENTOLA… - Revista de geomorfologie …, 2006 - geomorfologie.ro
Inactive Rock Glaciers have been recognized and mapped on the Peristeri and Tzoumerka
massifs, northern Pindos chain, Northwestern Greece, at around 2.000 m in altitude …