Tectonics of the Strandja Massif, NW Turkey: history of a long-lived arc at the northern margin of Palaeo-Tethys

B NATALIN, G SUNAL, M Satir… - Turkish Journal of Earth …, 2012 - journals.tubitak.gov.tr
Abstract The Strandja Massif, Thrace Peninsula, NW Turkey, forms an important link
between the Balkan Zone of Bulgaria, which is usually correlated with Variscan orogen in …

Geology and zircon U-Pb geochronology of the Mtkvari pyroclastic flow and evaluation of destructive processes affecting Vardzia rock-cut city, Georgia

A Okrostsvaridze, SL Chung, YC Lin… - Quaternary International, 2020 - Elsevier
Late Cenozoic subaerial volcanic highland crop out in Eastern Anatolia and the western part
of the Lesser Caucasus, part of which, located in Georgia, is known as Samtskhe-Javakheti …

Late Cenozoic volcanic activity in Western Georgia: Evidence from new isotope geochronological data

VA Lebedev, VG Sakhno, AI Yakushev - Doklady Earth Sciences, 2009 - Springer
The products of volcanic activity from the Kutaisi area and Guria (western Georgia) were
studied in terms of isotope geochronology to determine the age of rocks and to confirm their …

Geological structure of Georgia

I Gamkrelidze, A Okrostsvaridze, K Koiava… - Geotourism Potential of …, 2021 - Springer
This chapter provides a brief description of the geological structure of Georgia and
geodynamic evolution of the Caucasus. The territory of Georgia is a component of the …

NEW DATA ON PETROGEOCHEMICAL RESEARCH OF PRE-ALPINE QUARTZ DIORITES AND GRANITOIDS OF THE LOKI CRYSTALLINE MASSIF (LESSER …

T Tsutsunava, G Beridze… - … Janelidze Institute of …, 2024 - journals.4science.ge
The issues of geochemistry and genesis of the Upper Devonian quartz diorites and Late
Variscan granitoids of the pre-Alpine basement of the Loki crystalline massif are discussed …

Late Triassic age of moshevani suite of the Loki massif (Georgia, the Caucasus)

K Koiava, T Gavtadze, V Glonti, L Kvaliashvili… - Geofizicheskiy …, 2018 - journals.uran.ua
The Loki massif is located near the southern border of Georgia and is represented by large
anticline structure of EW oriented extension. The most ancient formations of the massif are …