Magmatic Response to Subduction Initiation: Part 1. Fore-arc Basalts of the Izu-Bonin Arc From IODP Expedition 352. [PDF]
Shervais JW +18 more
europepmc +1 more source
Constraining the Permeability and Outer‐Rise Hydration at the Central America Margin
Abstract Subduction zones are important drivers of Earth's geochemical evolution; the presence of water within the subduction system has substantial implications for geohazards, including the style of seismicity and the volume of magma generated at arc volcanoes.
D. Douglas +3 more
wiley +1 more source
Finite element models of spontaneous subduction initiation: preliminary results [PDF]
Subduction is a key process in Earth's plate tectonics that drives plate movement through slab pull. Despite its significance, the mechanisms behind subduction zone initiation (SZI) are not fully understood, and various hypotheses have been proposed and ...
Valeria Fedeli
core
Paleoseismic Evidence of Recent Co‐Seismic Ruptures in Western Tierra del Fuego, Chile
Abstract The Magallanes‐Fagnano fault (MFF) in Tierra del Fuego (TDF) is a major left‐lateral transform boundary between the South American and Scotia plates. While surface ruptures associated with the 1949 earthquakes have been documented in Argentina east of the Fagnano Lake, their extension to the west remained uncertain.
Ricardo Aguilera‐Cortés +4 more
wiley +1 more source
Rapid shear zone weakening during subduction initiation. [PDF]
Li Y, Gurnis M.
europepmc +1 more source
Postmagmatic Tectonic Evolution of the Outer Izu-Bonin Forearc Revealed by Sediment Basin Structure and Vein Microstructure Analysis: Implications for a 15 Ma Hiatus Between Pacific Plate Subduction Initiation and Forearc Extension. [PDF]
Kurz W +9 more
europepmc +1 more source
Abstract The Cenozoic topographic growth of the Iranian Plateau, situated at the Arabia‐Eurasia collision front, provides insights into continental collision dynamics. However, the relative contributions of tectonic shortening versus deep mantle processes to crustal thickening remain debated because systematic quantitative constraints on paleo‐crustal ...
Jun Hu +4 more
wiley +1 more source
Diversities of chromite mineralization induced by chemo-thermal evolution of the mantle during subduction initiation. [PDF]
Zhang PF +6 more
europepmc +1 more source
Abstract The geometry and distribution of igneous intrusions, which define melt source locations and record syn‐emplacement stress conditions, are essential for understanding tectonic and magmatic processes associated with crustal extension. However, in back‐arc settings along continental margins, structural constraints on these features remain poorly ...
Ryuta Arai +5 more
wiley +1 more source
Publisher Correction: Diversities of chromite mineralization induced by chemo-thermal evolution of the mantle during subduction initiation. [PDF]
Zhang PF +6 more
europepmc +1 more source

