The Smithian/Spathian boundary (late Early Triassic): A review of ammonoid, conodont, and carbon-isotopic criteria
The transition from the Smithian substage to the Spathian substage of the Olenekian stage
of the late Early Triassic was a critical time marked by a series of biological and …
of the late Early Triassic was a critical time marked by a series of biological and …
The drift history of Iran from the Ordovician to the Triassic
Abstract New Late Ordovician and Triassic palaeomagnetic data from Iran are presented.
These data, in conjunction with data from the literature, provide insights on the drift history of …
These data, in conjunction with data from the literature, provide insights on the drift history of …
The record of the Late Palaeozoic active margin of the Palaeotethys in NE Iran: constraints on the Cimmerian orogeny
The Cimmerian orogen resulted from the collision and accretion of several Perigondwanan
blocks to the southern margin of Eurasia between the Late Triassic and Early Jurassic …
blocks to the southern margin of Eurasia between the Late Triassic and Early Jurassic …
The Cimmerian evolution of the Nakhlak–Anarak area, Central Iran, and its bearing for the reconstruction of the history of the Eurasian margin
New structural, sedimentological, petrological and palaeomagnetic data collected in the
region of Nakhlak–Anarak provide important constraints on the Cimmerian evolution of …
region of Nakhlak–Anarak provide important constraints on the Cimmerian evolution of …
Oblique convergence during the Cimmerian collision: evidence from the Triassic Aghdarband Basin, NE Iran
Abstract The Lower-Middle Triassic Aghdarband Basin, NE Iran, consists of a strongly
deformed arc-related marine succession deposited along the southern margin of Eurasia in …
deformed arc-related marine succession deposited along the southern margin of Eurasia in …
Paleozoic to Triassic ocean opening and closure preserved in Central Iran: constraints from the geochemistry of meta-igneous rocks of the Anarak area
The Anarak area belongs to an ophiolitic belt along the northern border of the Central-East
Iranian Microcontinent, and is thought to contain fragments of the former Paleotethys and …
Iranian Microcontinent, and is thought to contain fragments of the former Paleotethys and …
Biostratigraphy of Triassic ammonoids
The Triassic is a turning point in the evolutionary history of ammonoids, characterized by the
flourishing Ceratitida and the appearance of the first heteromorphs. Following the end …
flourishing Ceratitida and the appearance of the first heteromorphs. Following the end …
Nakhlak carbonate-hosted Pb (Ag) deposit, Isfahan province, Iran: a geological, mineralogical, geochemical, fluid inclusion, and sulfur isotope study
MA Jazi, MH Karimpour, AM Shafaroudi - Ore Geology Reviews, 2017 - Elsevier
Abstract The Upper Cretaceous Nakhlak epigenetic vein-type Pbsingle bond (Ag) deposit is
located 55 km northeast of the town of Anarak in Isfahan Province, Iran. The deposit contains …
located 55 km northeast of the town of Anarak in Isfahan Province, Iran. The deposit contains …
The Cimmerian accretionary wedge of Anarak, Central Iran
The occurrence in Iran of several ophiolite belts dating between Late Palaeozoic to Triassic
poses several questions on the possible existence of various sutures marking the closure of …
poses several questions on the possible existence of various sutures marking the closure of …
Cimmerian metamorphism and post Mid-Cimmerian exhumation in Central Iran: Insights from in-situ Rb/Sr and U/Pb dating
The pre-Alpine evolution of the Tethyan domains between Gondwana and Laurasia, and in
particular that of the Cimmerian continental blocks, remains poorly constrained. Central Iran …
particular that of the Cimmerian continental blocks, remains poorly constrained. Central Iran …