The Pushtashan suprasubduction zone assemblage of volcanic rocks, gabbros, norites and peridotites occurs in the Zagros suture zone, Kurdistan region, northeastern Iraq. Volcanic rocks are dominant in the assemblage and consist mainly of basalt and basaltic andesite flows with interlayered red shale and limestone horizons. Earlier lavas tend to be MORB-like, whereas later lavas display island arc tholeiite to boninitic geochemical characteristics. Tholeiitic gabbros intrude the norites and display fractionation trends typical of crystallisation under low-pressure conditions, whereas the norites display calc-alkaline traits, suggesting their source included mantle metasomatised by fluids released from subducted oceanic crust. Enrichment of R...
The tectonic evolution of a Neo-Tethyan (Eocene-Oligocene) island-arc (Walash and Naopurdan groups) ...
Marine clastic rocks occurring in the Walash and Naopurdan Groups in the Hasanbag and Qalander areas...
Tectono-stratigraphic units within the Zagros Orogen in northeast Iraq (foreland) and northwest Iran...
The Kata–Rash arc fragment is an allochthonous thrust-bound body situated near Penjween, 100 km nort...
The Kata-Rash arc fragment is an allochthonous thrust-bound body situated near Penjween, 100 km nort...
In NE Iraq, the eastern edge of the Arabian plate is overlain by arc rock allochthons whose genesis ...
The suprasubduction Bulfat Igneous Complex in NE Iraq is one of the discontinuous Neotethys oceanic ...
The world\u27s largest ongoing collisional orogeny is the Europe Alps-Himalayan-SE Asian belt and is...
In the Makran region, SE Iran, one of the largest worldwide accretionary wedges is exposed. This acc...
New geochemical data were presented for the mafic (basalts and gabbros) and ultramafic (dunites, ser...
The Zagros fold-and-thrust belt of SW Iran is a young continental convergence zone, extending NW–SE ...
© 2020 Closure of Neo-Tethys between the Late Cretaceous and Miocene caused obduction of intra-Neo-T...
Recognition of a new angular unconformity and the synthesis of new detrital zircon U–Pb and (U–Th) /...
The Bulfat Igneous Complex comprises the Bulfat and Walash groups and is situated in the Zagros Sutu...
Late Cretaceous Neyriz ophiolite, as a part of the Outer Zagros Ophiolitic Belt, represents a remnan...
The tectonic evolution of a Neo-Tethyan (Eocene-Oligocene) island-arc (Walash and Naopurdan groups) ...
Marine clastic rocks occurring in the Walash and Naopurdan Groups in the Hasanbag and Qalander areas...
Tectono-stratigraphic units within the Zagros Orogen in northeast Iraq (foreland) and northwest Iran...
The Kata–Rash arc fragment is an allochthonous thrust-bound body situated near Penjween, 100 km nort...
The Kata-Rash arc fragment is an allochthonous thrust-bound body situated near Penjween, 100 km nort...
In NE Iraq, the eastern edge of the Arabian plate is overlain by arc rock allochthons whose genesis ...
The suprasubduction Bulfat Igneous Complex in NE Iraq is one of the discontinuous Neotethys oceanic ...
The world\u27s largest ongoing collisional orogeny is the Europe Alps-Himalayan-SE Asian belt and is...
In the Makran region, SE Iran, one of the largest worldwide accretionary wedges is exposed. This acc...
New geochemical data were presented for the mafic (basalts and gabbros) and ultramafic (dunites, ser...
The Zagros fold-and-thrust belt of SW Iran is a young continental convergence zone, extending NW–SE ...
© 2020 Closure of Neo-Tethys between the Late Cretaceous and Miocene caused obduction of intra-Neo-T...
Recognition of a new angular unconformity and the synthesis of new detrital zircon U–Pb and (U–Th) /...
The Bulfat Igneous Complex comprises the Bulfat and Walash groups and is situated in the Zagros Sutu...
Late Cretaceous Neyriz ophiolite, as a part of the Outer Zagros Ophiolitic Belt, represents a remnan...
The tectonic evolution of a Neo-Tethyan (Eocene-Oligocene) island-arc (Walash and Naopurdan groups) ...
Marine clastic rocks occurring in the Walash and Naopurdan Groups in the Hasanbag and Qalander areas...
Tectono-stratigraphic units within the Zagros Orogen in northeast Iraq (foreland) and northwest Iran...