Continental magmatic arcs form above subduction zones where the upper plate is continental lithosphere and/or accreted transitional lithosphere. The best-studied examples …
Accretionary orogens form at intraoceanic and continental margin convergent plate boundaries. They include the supra-subduction zone forearc, magmatic arc and back-arc …
S Lallemand, D Arcay - Earth-Science Reviews, 2021 - Elsevier
To address the question of the initiation and mechanisms involved in the process of subduction zone formation, we explored most of the available evidence for the subduction …
Abstract The Izu–Bonin–Mariana (IBM) forearc contains a record of a widespread and short- lived subduction initiation event in the early Eocene. We present new high-precision ages to …
Articulating a comprehensive plate-tectonic theory requires understanding how new subduction zones form (subduction initiation). Because subduction initiation is a …
In this issue of Elements we explore the characteristics, potential causes, and implications of episodic magmatism in arcs. A comparison of U–Pb bedrock and detrital zircon ages in arcs …
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 …
The intraoceanic Kohistan arc, northern Pakistan, exposes a complete crustal section composed of infracrustal basal cumulates formed at≤ 55km depth, a broadly …
The close relationship between crustal magmatism, an expression of heat dissipation, and tectonics, an expression of stress dissipation, leads to the question of their mutual …