[HTML][HTML] Orogenic architecture of the Mediterranean region and kinematic reconstruction of its tectonic evolution since the Triassic
The basins and orogens of the Mediterranean region ultimately result from the opening of
oceans during the early break-up of Pangea since the Triassic, and their subsequent …
oceans during the early break-up of Pangea since the Triassic, and their subsequent …
Caucasus collisional history: Review of data from East Anatolia to West Iran
Y Rolland - Gondwana Research, 2017 - Elsevier
This article summarizes the geodynamic evolution of the Caucasus mountain belt from the
Paleozoic to Present based on a review of works from Eastern Anatolia, Greater and Lesser …
Paleozoic to Present based on a review of works from Eastern Anatolia, Greater and Lesser …
Long-lived, stationary magmatism and pulsed porphyry systems during Tethyan subduction to post-collision evolution in the southernmost Lesser Caucasus, Armenia …
Abstract The composite Meghri–Ordubad and Bargushat plutons of the Zangezur–Ordubad
region in the southernmost Lesser Caucasus consist of successive Eocene to Pliocene …
region in the southernmost Lesser Caucasus consist of successive Eocene to Pliocene …
Geodynamics, seismicity, and seismic hazards of the Caucasus
A Ismail-Zadeh, S Adamia, A Chabukiani… - Earth-Science …, 2020 - Elsevier
Being a part of ongoing continental collision between the Arabian and Eurasian plates, the
Caucasus region is a remarkable site of moderate to strong seismicity, where devastating …
Caucasus region is a remarkable site of moderate to strong seismicity, where devastating …
[HTML][HTML] The eastern Black Sea-Caucasus region during the Cretaceous: New evidence to constrain its tectonic evolution
We report new observations in the eastern Black Sea-Caucasus region that allow
reconstructing the evolution of the Neotethys in the Cretaceous. At that time, the Neotethys …
reconstructing the evolution of the Neotethys in the Cretaceous. At that time, the Neotethys …
The North Sistan orogen (Eastern Iran): Tectono-metamorphic evolution and significance within the Tethyan realm
Abstract The Sistan orogen (Eastern Iran) separates the Afghan and Lut continental blocks
and stretches along∼ 700 km from north to south, at a high angle with respect to other …
and stretches along∼ 700 km from north to south, at a high angle with respect to other …
The East Anatolia–Lesser Caucasus ophiolite: An exceptional case of large-scale obduction, synthesis of data and numerical modelling
We present new, geological, metamorphic, geochemical and geochronological data on the
East Anatolian–Lesser Caucasus ophiolites. These data are used in combination with a …
East Anatolian–Lesser Caucasus ophiolites. These data are used in combination with a …
Long-lived, Eocene-Miocene stationary magmatism in NW Iran along a transform plate boundary
Abstract The Eocene-Miocene Mianeh-Hashtroud igneous district in NW Iran is part of the
Turkish–Caucasus–Iranian collision zone, a key region to decipher the assembly and …
Turkish–Caucasus–Iranian collision zone, a key region to decipher the assembly and …
Postcollisional transition from subduction-to intraplate-type magmatism in the eastern Sakarya zone, Turkey: Indicators of northern Neotethyan slab breakoff
Postcollisional magmatism in the eastern Sakarya zone was recorded by voluminous basic
volcanism and repeated plutonism during the early Cenozoic. The temporal and …
volcanism and repeated plutonism during the early Cenozoic. The temporal and …
30 Myr of Cenozoic magmatism along the Tethyan margin during Arabia–Eurasia accretionary orogenesis (Meghri–Ordubad pluton, southernmost Lesser Caucasus)
Three magmatic series of substantially different ages and compositions were successively
emplaced to form the composite Meghri–Ordubab pluton (MOP) in the southernmost Lesser …
emplaced to form the composite Meghri–Ordubab pluton (MOP) in the southernmost Lesser …