Tibetan ore deposits: A conjunction of accretionary orogeny and continental collision
This paper reviews the spatial-temporal distribution, geological and geochemical features,
and geophysical context of diverse types of Cenozoic ore deposits formed during India …
and geophysical context of diverse types of Cenozoic ore deposits formed during India …
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 …
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 …
A data augmentation approach to XGboost-based mineral potential mapping: an example of carbonate-hosted ZnPb mineral systems of Western Iran
M Parsa - Journal of Geochemical Exploration, 2021 - Elsevier
This study intends to showcase the application of Extreme Gradient boosting (XGboost), a
state-of-the-art ensemble-learning technique, for district-scale mineral potential mapping …
state-of-the-art ensemble-learning technique, for district-scale mineral potential mapping …
A Paleogene extensional arc flare‐up in Iran
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 …
presumably continuous subduction along the northern margin of the Neotethyan ocean for …
The geodynamic evolution of Iran
Iran is a remarkable geoscientific laboratory where the full range of processes that form and
modify the continental crust can be studied. Iran's crustal nucleus formed as a magmatic arc …
modify the continental crust can be studied. Iran's crustal nucleus formed as a magmatic arc …
Arabia-Eurasia continental collision: Insights from late Tertiary foreland-basin evolution in the Alborz Mountains, northern Iran
P Ballato, CE Uba, A Landgraf, MR Strecker… - …, 2011 - pubs.geoscienceworld.org
A poorly understood lag time of 15–20 my exists between the initial Arabia-Eurasia
continental collision in late Eocene to early Oligocene time and the acceleration of tectonic …
continental collision in late Eocene to early Oligocene time and the acceleration of tectonic …
U-Pb zircon geochronology of late Neoproterozoic–Early Cambrian granitoids in Iran: Implications for paleogeography, magmatism, and exhumation history of Iranian …
Eurasia has largely grown to its present enormous size through episodic addition of crustal
blocks by recurring birth and demise of oceans such as Paleotethys and Neotethys …
blocks by recurring birth and demise of oceans such as Paleotethys and Neotethys …
Geochemistry and tectonics of Cenozoic volcanism in the Lesser Caucasus (Azerbaijan) and the peri-Arabian region: collision-induced mantle dynamics and its …
Y Dilek, N Imamverdiyev… - International Geology …, 2010 - Taylor & Francis
The Lesser Caucasus occurs in the hinterland of the Arabia–Eurasia collision zone in the
broad Alpine–Himalayan orogenic belt and includes Cenozoic plutonic and volcanic …
broad Alpine–Himalayan orogenic belt and includes Cenozoic plutonic and volcanic …
[HTML][HTML] Geodynamics and metallogeny of the eastern Tethyan metallogenic domain
Z Hou, H Zhang - Ore Geology Reviews, 2015 - Elsevier
The Tethyside orogen, a direct consequence of the separation of the Gondwanaland and the
accretion of Eurasia, is a huge composite orogenic system that was generated during …
accretion of Eurasia, is a huge composite orogenic system that was generated during …