Mid-ocean ridge magma reservoirs are mush-dominated systems, where reactive porous
flow is a dominant post-cumulus process. However, the length scale of this process is poorly …

The structure of the lithosphere and the associated magmatic systems found in different
locations along slow‐spreading ridges can vary dramatically, from melt‐starved to …

Various crustal processes shape both the lower oceanic crust and mid-ocean ridge basalts
(MORBs). To better understand how these crustal processes influence MORB compositions …

Construction of oceanic crusts in ultraslow-spreading ridges are controlled by detachment
faults, but the specific ways they are determined by detachments remain unclear. Abundant …

As the melting residue of the asthenosphere at ocean ridges, the oceanic mantle lithosphere
is initially depleted, which might be re-enriched by various types of melts. However, the …

Oceanic detachments are deep-rooted, long-lived, plate-scale structures and serve as fluid
conduits introducing water into the oceanic lithosphere, impacting plate rheology and …

Although seismic and hydrothermal data show evidence of magma–seawater interaction in
slow spreading-rate ridges, such a process has been rarely observed in situ in lower …

Abstract The 290-to 282-Ma ophiolitic Liuyuan Complex in northwestern China preserves a
section of oceanic crust formed in a back-arc basin during the final stages of the evolution of …

Microfabrics of a gabbroic ultramylonitic shear zone from the Atlantis Bank oceanic core
complex have been studied to investigate strain localization processes during exhumation of …

The collision between the Indian plate and the West Burma Block led to formation of Neo-
Tethyan ophiolite along the Western Ophiolitic Belt (WOB). The ophiolitic rocks in the WOB …