The causes of continental arc flare ups and drivers of episodic magmatic activity in Cordilleran orogenic systems
Continental arcs in Cordilleran orogenic systems display episodic changes in magma
production rate, alternating between flare ups (70–90 km 3 km− 1 Myr− 1) and lulls (< 20 km …
production rate, alternating between flare ups (70–90 km 3 km− 1 Myr− 1) and lulls (< 20 km …
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] Comparison of different algorithms to map hydrothermal alteration zones using ASTER remote sensing data for polymetallic vein-type ore exploration: Toroud …
Polymetallic vein-type ores are important sources of precious metal and a principal type of
orebody for various base-metals. In this research, Advanced Spaceborne Thermal Emission …
orebody for various base-metals. In this research, Advanced Spaceborne Thermal Emission …
Evolution of the Zagros sector of Neo-Tethys: Tectonic and magmatic events that shaped its rifting, seafloor spreading and subduction history
The evolution of the Neo-Tethys realm had a significant impact on the Phanerozoic
paleogeography of the Iran Plateau. However, there remains significant debate regarding …
paleogeography of the Iran Plateau. However, there remains significant debate regarding …
Repeated magmatic buildup and deep “hot zones” in continental evolution: the Cadomian crust of Iran
The generation and differentiation of continental crust by arc magmatism is strongly
influenced by episodes of high magmatic flux (“flare-ups”). Magmatic flare-ups encourage …
influenced by episodes of high magmatic flux (“flare-ups”). Magmatic flare-ups encourage …
[HTML][HTML] Early Paleozoic accretionary orogens along the Western Gondwana margin
Early Paleozoic accretionary orogens dominated the Western Gondwana margin and were
characterized by nearly continuous subduction associated with crustal extension and back …
characterized by nearly continuous subduction associated with crustal extension and back …
Integrated detrital rutile and zircon provenance reveals multiple sources for Cambrian sandstones in North Gondwana
Early Paleozoic sandstones deposited along the northern margin of Gondwana are
commonly interpreted to represent a vast, well-mixed, and far-travelled blanket of sand …
commonly interpreted to represent a vast, well-mixed, and far-travelled blanket of sand …
Cadomian to Cenerian accretionary orogenic processes in the Alpine basement: the detrital zircon archive
New whole-rock geochemical and detrital zircon U–Pb and Lu–Hf data of metasedimentary
sequences of the Silvretta Nappe, Orobic Alps, Strona-Ceneri Zone, Gotthard Massif and …
sequences of the Silvretta Nappe, Orobic Alps, Strona-Ceneri Zone, Gotthard Massif and …
Crustal evolution of NW Iran: Cadomian arcs, Archean fragments and the Cenozoic magmatic flare-up
The Cadomian orogen of NW Iran includes a series of metamorphic rocks with zircon U-Pb
ages between ca 562 and 505 Ma (Ediacaran to middle Cambrian). The Ediacaran …
ages between ca 562 and 505 Ma (Ediacaran to middle Cambrian). The Ediacaran …