The subduction plate interface: Rock record and mechanical coupling (from long to short timescales)
Short-and long-term processes at or close to the subduction plate interface (eg, mineral
transformations, fluid release, seismicity and more generally deformation) might be more …
transformations, fluid release, seismicity and more generally deformation) might be more …
The Samail subduction zone dilemma: Geochronology of high-pressure rocks from the Saih Hatat window, Oman, reveals juxtaposition of two subduction zones with …
Abstract The Samail Ophiolite in the Oman Mountains formed at a Cretaceous subduction
zone that was part of a wider Neo-Tethys plate-boundary system. The original configuration …
zone that was part of a wider Neo-Tethys plate-boundary system. The original configuration …
Subducted fragments of the Liguro-Piemont ocean, Western Alps: Spatial correlations and offscra** mechanisms during subduction
Fragments of subducted slow-spreading oceanic lithosphere are exposed continuously in
the Liguro-Piemont domain of the Western Alps. By combining new and literature …
the Liguro-Piemont domain of the Western Alps. By combining new and literature …
Petrochronological close-up on the thermal structure of a paleo-subduction zone (W. Alps)
We present the results from a study combining zoned geochronology, mineral trace element
geochemistry and phase equilibria modeling of a mafic lithology from the Zermatt Saas …
geochemistry and phase equilibria modeling of a mafic lithology from the Zermatt Saas …
Shattered veins elucidate brittle creep processes in the deep slow slip and tremor region
Abstract Deep Slow Slip and Tremors (SSTs) are a combination of transient clusters of
tectonic tremors and slow slip associated with extremely elevated fluid pressures. SSTs are …
tectonic tremors and slow slip associated with extremely elevated fluid pressures. SSTs are …
The North Sistan orogen (Eastern Iran): Tectono-metamorphic evolution and significance within the Tethyan realm
Abstract The Sistan orogen (Eastern Iran) separates the Afghan and Lut continental blocks
and stretches along∼ 700 km from north to south, at a high angle with respect to other …
and stretches along∼ 700 km from north to south, at a high angle with respect to other …
[HTML][HTML] Thermal evolution of an ancient subduction interface revealed by Lu–Hf garnet geochronology, Halilbağı Complex (Anatolia)
The thermal structure of subduction zones exerts a major influence on deep-seated
mechanical and chemical processes controlling arc magmatism, seismicity, and global …
mechanical and chemical processes controlling arc magmatism, seismicity, and global …
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 …
Architecture and PT-deformation-time evolution of the Chinese SW-Tianshan HP/UHP complex: Implications for subduction dynamics
We present the first comprehensive PT-deformation-time and kinematic constraints for
HP/UHP eclogite, blueschist and greenschist-facies metavolcano-sedimentary rocks …
HP/UHP eclogite, blueschist and greenschist-facies metavolcano-sedimentary rocks …
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 …