, 2020 International audienceThe Neotethys ocean is transiently involved in two subduction zones during the Late Cretaceous. While the Northern Neotethys subduction zone (below Eurasia) was active from the early Mesozoic until the Eocene, the intra-oceanic ...
Fournier, Marc +6 more
core +1 more source
Frontiers in Earth Science, 2020 Zircon U-Pb age, mineral compositional, elemental and Sr-Nd isotopic data are documented for intermediate to felsic rocks in the Takht batholith, a Late Oligocene igneous complex in the southeastern segment of the Urumieh-Dokhtar belt, Iran, to ...
Kwan-Nang Pang +6 more
doaj +1 more source
Investigation of the evolution of arc: Azadegan magmatic rocks, north of Shahrekord, Sanandaj-Sirjan zone [PDF]
پترولوژی, 2021 The magmatic complex of Azadegan, composed of basalt, andesitic basalt, andesite, gabbro and diorite, located 45 km northwest of Shahrekord and in the middle part of the Sanandaj-Sirjan zone..
Maryam Ahankoub +2 more
doaj +1 more source
Clumped isotope data for Early Triassic brachiopods and whole rock carbonates from Oman (NeoTethys)
, 2023 This repository contains the research data associated with the research paper titled: "Carbonate Clumped Isotope Constraints on Early Triassic NeoTethyan Seawater Oxygen Isotope Compositions and Temperatures".The dataset includes results from ...
EDWARD, O (via Mendeley Data)
core +2 more sources
Cretaceous Volcanic Rock Geosites of the Papuk UNESCO Global Geopark (Croatia): Scientific Aspect of Geoheritage in Geoeducation, Geotourism and Geoconservation [PDF]
Geoconservation Research, 2023 Research over decades confirms the geological values of the Papuk UNESCO Global Geopark (Croatia) as a unique place in the regional frame where several orogenic events left their traces through the formation of diverse lithologies.
Dražen Balen +4 more
doaj +1 more source
PETROGENESIS AND ORIGIN OF THE CHENAR GRANITOID STOCK, NW OF KERMAN, IRAN: EVIDENCE OF NEOTETHYS SUBDUCTION RELATED ARC MAGMATISM [PDF]
Journal of Sciences, Islamic Republic of Iran, 2003 The lower to middle Miocene Chenar granitoid stock, a part of Central Iranian volcanic belt, is intruded into Eocene volcano-sedimentary complex in northwestern Kerman in south Central Iran.
M. Arvin
doaj
Middle and Late Jurassic radiolarians from the Neotethys suture in the Eastern Alps [PDF]
Journal of Paleontology, 2016 AbstractCherty limestones, marls and radiolarites are widespread in the Hallstatt Mélange of the Northern Calcareous Alps. The mélange was formed during the Neotethyan orogeny in a series of deep-water basins that progressively developed in front of the advancing nappe front.
O’Dogherty Luy, Luis Carlos +2 more
openaire +2 more sources
, 2019 Stable isotopic record of the late Eocene-early Oligocene interval, southwestern Neotethys margin (northeastern ...
Messaoud, Jihede Haj +1 more
core +1 more source
, 2020 In Anatolia, the northern branch of Neotethys is represented by Izmir-Ankara-Erzincan (IAE) Ocean, whose fragments and associated continental entities are preserved in the IAE Suture.
Bedi, Yavuz +9 more
core +1 more source
Bio- and isotope stratigraphy of the Cenomanian-Turonian transition and the variations related to OAE2 in the Holul section, west of Kermanshah [PDF]
Journal of Stratigraphy and Sedimentology Researches, 2017 Micropalaeontological study based on planktonic foraminifera in the Cenomanian - Turonian succession of the Holul section, located in the Lurestan geological province (west of the Kermanshah City), resulted in distinction of Rotalipora cushmani ...
Mehdi Sarfi +3 more
doaj +1 more source