Triassic-cretaceous sedimentary and magmatic development of the classic SW outcrop of the Antalya Complex, S Türkiye as a developing rift and passive margin bordering the Southern Neotethys [PDF]
The SW segment of the Antalya Complex (Antalya nappes) documents sedimentation, magmatism and tectonics related to Permian-Triassic continental rifting, Jurassic-Cretaceous passive margin subsidence, Late Cretaceous ophiolite genesis, and latest ...
Parlak, Osman +3 more
core +1 more source
Petrogenesis of low Silica Adakitic domes of Sahl (South of Shahrood, southeast of Semnan Province) [PDF]
پترولوژی, 2016 Sahl area, in the south of Shahrood, is a part of the northern portion of the Central Iran Structural Zone. The area is dominated by a thick sequence of the Paleocene to the middle Eocene volcanic and volcano-sedimentary rocks.
Fazilat Yousefi +4 more
doaj
, 2017 The Mersin Melange is a tectonostratigraphic unit within the allochthonous Mersin Ophiolitic Complex in the Taurides, southern Turkey. This chaotic structure consists of blocks and tectonic slices of diverse origins and ages set in a clastic matrix of ...
Bedi, Yavuz +7 more
core +1 more source
Carnets de Géologie, 2009 The Miscellaneidae are divided into two groups of species: forms with a single intercameral foramen and forms with two or a row of multiple foramina. Ten taxa ascribed to this family are revised, amply illustrated and discussed considering both micro ...
Hottinger Lukas
doaj
GeosciencesSeveral short sections from Istria (northern Adriatic Sea) were studied to determine the impact of short-term climate variability on pelagic assemblages from the northern mid-latitudes during a critical period of evolution in the mid-Eocene greenhouse ...
Ines Galović +6 more
doaj +1 more source
The closure of the Vardar Ocean (the western domain of the northern Neotethys) from the early Middle Jurassic to the Paleocene time, based on the surface geology of eastern Pelagonia and the Vardar zone, biostratigraphy, and seismic-tomographic images of the mantle below the Central Hellenides. [PDF]
UCL Open Environ, 2021 Scherreiks R, BouDagher-Fadel M.
europepmc +1 more source
Three independent single-grain geochronometers applied to detrital minerals from Central Dinaride sediments constrain the timing of felsic magmatism that associated the Jurassic evolution of the Neotethys.
Mikes, Tamás +6 more
core
Eocene contractional deformation in the NW corner of the Arabian plate and its relation to Arabia-Eurasia collision in SE Türkiye [PDF]
Field evidence indicates c. 40 Ma (Early-Middle Eocene) contractional deformation in the S Amanos Mountains. Following latest Cretaceous southward ophiolite emplacement, an intra-platform basin infilled with shallow to deeper marine, dominantly carbonate
Parlak, Osman, Robertson, Alastair H. F.
core +1 more source
Metamorphism at convergent plate margins: Preface. [PDF]
Geosci Front, 2022 Palin RM, Roberts NMW.
europepmc +1 more source
, 2016 Evidence of the subduction–collision history of the S Neotethys is well exposed in the frontal part of the SE Anatolian thrust belt and the adjacent Arabian continental margin. The foreland succession in the study area begins with Eocene shelf carbonates,
Ünlügenç U.C. +2 more
core +1 more source