A monotypic stand of Neocalamites iranensis n. sp. from the Carnian Pluvial Episode (Late Triassic) of the Aghdarband area, NE Iran (Turan Plate)

Autor: Mazaheri-Johari M.[1], Kustatscher E.[2, Roghi G.[4], Ghasemi-Nejad E.[5], Gianolla P.[1]

Publikováno v: Rivista italiana di paleontologia e stratigrafia (Online) 127 (2021): 189–209. doi:10.13130/2039-4942/15646
info:cnr-pdr/source/autori:Mazaheri-Johari M.[1], Kustatscher E.[2,3], Roghi G.[4], Ghasemi-Nejad E.[5], Gianolla P.[1]/titolo:A monotypic stand of Neocalamites iranensis n. sp. from the Carnian Pluvial Episode (Late Triassic) of the Aghdarband area, NE Iran (Turan Plate)/doi:10.13130%2F2039-4942%2F15646/rivista:Rivista italiana di paleontologia e stratigrafia (Online)/anno:2021/pagina_da:189/pagina_a:209/intervallo_pagine:189–209/volume:127
RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA ; Vol. 127 No. 2 (2021)
Rivista italiana di Paleontologia e Stratigrafia; V. 127 N. 2 (2021)
Rivista Italiana di Paleontologia e Stratigrafia, Vol 127, Iss 2 (2021)

The Aghdarband Basin in the Kopeh-Dagh Range (NE Iran) is one of the most important areas for unraveling the evolution of the Turan plate (southern margin of Eurasia) during the last phase of the closure of the Paleotethys and to reconstruct the hist

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