Rift basins in mountain belts shed light on the palaeogeography and tectonic development
of adjacent sutured ocean basins, as for the Antalya Complex in the S Neotethys region …

Valid palaeotectonic and palaeogeographical reconstructions of the easternmost
Mediterranean and adjacent region involve a long-lived Tethys (Rheic, Palaeotethyan and …

Une comparaison précise du changement dans les faunes radiolaires à 3, 5 m au-dessus
d'un tuf daté à 199, 6±0, 3 Ma, par U Pb sur un zircon, et coïncidant approximativement à …

The main goal of this catalogue is to present a set of uniformly and precisely defined
radiolarian species that will serve as a coherent taxonomic base to establish a global …

Volcanic activity in the Central Atlantic magmatic province, resulting in an increased flux of
CO2, SO2, and CH4 into the oceans and atmosphere, has been proposed as one of the …

Evidence of rifting and continental break-up to form the S Neotethys is found within the
volcanic-sedimentary Koçali Complex. This is a folded, thrust-imbricated succession that …

The Kocali Complex in SE Turkey includes pelagic sediments (pelagic limestones, cherts,
etc.), basic volcanic rocks of oceanic crust origin together with platform-derived sediments …

The Triassic–Jurassic boundary (T–J boundary) interval is one of the most important but
poorly understood intervals in the Phanerozoic. Here we fully document the ammonite and …

Abstract In the Argolis, the Basal Sequence, constituting the eastern Pelagonian margin
which bordered the Maliac-Vardar oceanic domain, includes shallow-water carbonates of …

This paper is a presentation of three sources of artifact‐quality chert in C entral A natolia. A
previous dearth of research focused on locating and characterizing such raw material …