Abstract The Neo-Tethys Ocean was an eastward-ga** triangular oceanic embayment
between Laurasia to the north and Gondwana to the south. The Neo-Tethys Ocean was …

Short-and long-term processes at or close to the subduction plate interface (eg, mineral
transformations, fluid release, seismicity and more generally deformation) might be more …

This paper presents a synthetic view of the geodynamic evolution of the Zagros orogen
within the frame of the Arabia–Eurasia collision. The Zagros orogen and the Iranian plateau …

The Zagros Mountains are the result of the Arabia/Eurasia collision initiated at~ 35Ma as the
rifted Arabian lithosphere was underthrusted beneath the Iranian plate due to its negative …

This paper reviews the tectonic, magmatic, and metallogenic history of the Tethyan orogen
from the Carpathians to Indochina. Focus is placed on the formation of porphyry Cu±Mo±Au …

The temporal and geochemical evolution of arc magmatism that culminated in porphyry
Cu±Mo±Au deposit formation has been studied in three separate Neo-Tethyan arc systems …

This study reports zircon LA-ICPMS U–Pb ages of 50 igneous rock samples from the
Urumieh–Dokhtar magmatic arc (UDMA) and Sanandaj–Sirjan structural zone (SSZ) in Iran …

Abstract The Sanandaj‐Sirjan zone of Iran is a northwest trending orogenic belt immediately
north of the Zagros suture, which represents the former position of the Neotethys Ocean. The …

Abstract The Arabia-Eurasia collision has been linked to global cooling, the slowing of
Africa, Mediterranean extension, the rifting of the Red Sea, an increase in exhumation and …

Arc volcanism across Iran is dominated by a Paleogene pulse, despite protracted and
presumably continuous subduction along the northern margin of the Neotethyan ocean for …