Cyclical one-way continental rupture-drift in the Tethyan evolution: Subduction-driven plate tectonics
Numerous continents have rifted and drifted away from Gondwana to repeatedly open
ocean basins over the past∼ 500 million years. These Gondwana-derived continents drifted …
ocean basins over the past∼ 500 million years. These Gondwana-derived continents drifted …
Paleo-Tethys subduction induced slab-drag opening the Neo-Tethys: Evidence from an Iranian segment of Gondwana
The Iranian plateau has a more straightforward relationship between the Paleo-Tethys and
Neo-Tethys, than other regions in the Tethyan realm and is an ideal place to test the genetic …
Neo-Tethys, than other regions in the Tethyan realm and is an ideal place to test the genetic …
[HTML][HTML] On the nature of the Cimmerian Continent
Abstract The Cimmerian Continent is the narrow continental strip that rifted from the
northeastern Gondwana-Land margin mostly during the Permian between the present-day …
northeastern Gondwana-Land margin mostly during the Permian between the present-day …
New evidence for Jurassic continental rifting in the northern Sanandaj Sirjan Zone, western Iran: the Ghalaylan seamount, southwest Ghorveh
We address the growing controversy about the tectonic setting in which Jurassic magmatism
of Iran occurred: arc or continental rift. In the Ghorveh area of the northern Sanandaj Sirjan …
of Iran occurred: arc or continental rift. In the Ghorveh area of the northern Sanandaj Sirjan …
Accelerated middle Miocene exhumation of the Talesh Mountains constrained by U‐Th/He thermochronometry: Evidence for the Arabia‐Eurasia collision in the NW …
Abstract The Talesh Mountains at the NW margin of the Iranian Plateau curve around the
southwestern corner of the South Caspian Block and developed in response to the collision …
southwestern corner of the South Caspian Block and developed in response to the collision …
Does neoproterozoic-early paleozoic (570–530 Ma) basement of Iran belong to the cadomian orogeny?
H Azizi, SA Whattam - Precambrian Research, 2022 - Elsevier
Abstract Late Neoproterozoic–Early Paleozoic basement in Iran mainly comprises granites
and mafic rocks locally affected by high-grade metamorphism. In this contribution, we collate …
and mafic rocks locally affected by high-grade metamorphism. In this contribution, we collate …
Detrital zircon age constraints on the evolution of Paleo‐Tethys in NE Iran: Implications for subduction and collision tectonics
The timings of the onset of oceanic spreading, subduction and collision are crucial in plate
reconstructions, but not always straightforward to resolve. The Paleo‐Tethys evolution …
reconstructions, but not always straightforward to resolve. The Paleo‐Tethys evolution …
[PDF][PDF] 重力驱动的特提斯单向裂解-聚合动力学
万博， 吴福元， 陈凌， 赵亮， 梁晓峰， 肖文交… - 中国科学: 地球 …, 2019 - researchgate.net
摘要地球自5 亿年以来, 大量陆块从南方的冈瓦纳大陆不断裂解, 相继形成原, 古, 新特提斯大洋.
这些陆块随后陆续漂向北方的劳亚大陆, 并与之发生碰撞拼合, 形成全球最显著的大陆碰撞造山 …
这些陆块随后陆续漂向北方的劳亚大陆, 并与之发生碰撞拼合, 形成全球最显著的大陆碰撞造山 …
The Late Jurassic Panjeh submarine volcano in the northern Sanandaj-Sirjan Zone, northwest Iran: Mantle plume or active margin?
The tectonic setting in which Jurassic igneous rocks of the Sanandaj-Sirjan Zone (SaSZ) of
Iran formed is controversial. SaSZ igneous rocks are mainly intrusive granodiorite to …
Iran formed is controversial. SaSZ igneous rocks are mainly intrusive granodiorite to …