The origin and pre-Cenozoic evolution of the Tibetan Plateau
Different hypotheses have been proposed for the origin and pre-Cenozoic evolution of the
Tibetan Plateau as a result of several collision events between a series of Gondwana …
Tibetan Plateau as a result of several collision events between a series of Gondwana …
[HTML][HTML] Tectonic, magmatic, and metallogenic evolution of the Tethyan orogen: From subduction to collision
JP Richards - Ore Geology Reviews, 2015 - Elsevier
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 …
from the Carpathians to Indochina. Focus is placed on the formation of porphyry Cu±Mo±Au …
Continental arc volcanism as the principal driver of icehouse-greenhouse variability
Variations in continental volcanic arc emissions have the potential to control atmospheric
carbon dioxide (CO2) levels and climate change on multimillion-year time scales. Here we …
carbon dioxide (CO2) levels and climate change on multimillion-year time scales. Here we …
Building the Zagros collisional orogen: timing, strain distribution and the dynamics of Arabia/Eurasia plate convergence
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 …
rifted Arabian lithosphere was underthrusted beneath the Iranian plate due to its negative …
High Sr/Y magmas reflect arc maturity, high magmatic water content, and porphyry Cu±Mo±Au potential: Examples from the Tethyan arcs of central and eastern Iran …
JP Richards, T Spell, E Rameh… - Economic …, 2012 - pubs.geoscienceworld.org
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 …
Cu±Mo±Au deposit formation has been studied in three separate Neo-Tethyan arc systems …
Zircon U–Pb age constraints from Iran on the magmatic evolution related to Neotethyan subduction and Zagros orogeny
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 …
Urumieh–Dokhtar magmatic arc (UDMA) and Sanandaj–Sirjan structural zone (SSZ) in Iran …
The Neotethyan Sanandaj‐Sirjan zone of Iran as an archetype for passive margin‐arc transitions
J Hassanzadeh, BP Wernicke - Tectonics, 2016 - Wiley Online Library
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 …
north of the Zagros suture, which represents the former position of the Neotethys Ocean. The …
Cenozoic tectonic evolution of Asia: A preliminary synthesis
A Yin - Tectonophysics, 2010 - Elsevier
Asia has been a major testing ground for various competing models of continental
deformation due to its relatively well-understood plate boundary conditions in the Cenozoic …
deformation due to its relatively well-understood plate boundary conditions in the Cenozoic …
Retrodeforming the Arabia-Eurasia collision zone: Age of collision versus magnitude of continental subduction
N McQuarrie, DJJ van Hinsbergen - Geology, 2013 - pubs.geoscienceworld.org
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 …
Africa, Mediterranean extension, the rifting of the Red Sea, an increase in exhumation and …