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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 …
A review of Mesozoic geodynamic evolution of the North Makran (SE Iran): A tale of a Neo-Tethyan ocean vanished due to two coexisting subduction zones
This paper presents a synthesis of the geological features of each tectonic unit of the North
Makran (SE Iran), integrating results of multidisciplinary analyses, including structural and …
Makran (SE Iran), integrating results of multidisciplinary analyses, including structural and …
Episodic hydrofracturing and large-scale flushing along deep subduction interfaces: Implications for fluid transfer and carbon recycling (Zagros Orogen, southeastern …
We investigate the late Cretaceous blueschist-facies (480° C-1.8 GPa) segment of the
Zagros suture zone, a well-preserved block-in-matrix paleo-subduction channel. We aim to …
Zagros suture zone, a well-preserved block-in-matrix paleo-subduction channel. We aim to …
Structure of the offshore obducted Oman margin: Emplacement of Semail ophiolite and role of tectonic inheritance
The northern Oman margin is a key area for understanding the emplacement of the Semail
Ophiolite and obduction processes in general. This study uses a grid of 2D‐multichannel …
Ophiolite and obduction processes in general. This study uses a grid of 2D‐multichannel …
New evidence for Late Cretaceous plume-related seamounts in the Middle East sector of the Neo-Tethys: constraints from geochemistry, petrology, and mineral …
Abstract The Durkan Complex in the Makran Accretionary Prism (SE Iran) has been
interpreted either as a continental margin succession or a Late Cretaceous tectonically …
interpreted either as a continental margin succession or a Late Cretaceous tectonically …
The rise and demise of deep accretionary wedges: A long-term field and numerical modeling perspective
Several decades of field, geophysical, analogue, and numerical modeling investigations
have enabled documentation of the wide range of tectonic transport processes in …
have enabled documentation of the wide range of tectonic transport processes in …
[HTML][HTML] Deformation history and processes during accretion of seamounts in subduction zones: the example of the Durkan Complex (Makran, SE Iran)
Abstract The Durkan Complex is a tectonic element of the Makran Accretionary Prism (SE
Iran) that includes fragments of Late Cretaceous seamounts. In this paper, the results of map …
Iran) that includes fragments of Late Cretaceous seamounts. In this paper, the results of map …
Volcanic crustal structure of the western Hikurangi Plateau (New Zealand) from marine seismic reflection imaging
Seamounts and basaltic basement can influence deformation and mass fluxes within
subduction zones. We examined seamounts and volcanic units across the western …
subduction zones. We examined seamounts and volcanic units across the western …
Seamount subduction dynamics and long‐term evolution of the Franciscan active margin
Abstract The Snow Mountain Volcanic Complex (SMVC; northern California, USA) is a well‐
preserved example of a coherently‐exhumed subducted seamount. This study reappraises …
preserved example of a coherently‐exhumed subducted seamount. This study reappraises …
The western Durkan Complex (Makran Accretionary Prism, SE Iran): A Late Cretaceous tectonically disrupted seamounts chain and its role in controlling deformation …
Abstract The Durkan Complex is a key tectonic element of the Makran accretionary prism
(SE Iran) and it has been interpreted as representing a continental margin succession. We …
(SE Iran) and it has been interpreted as representing a continental margin succession. We …