Multiple episodes of deformation during the tectonic evolution of orogenic belts and ancient
subduction-accretion complexes cause obfuscation of primary block-in-matrix fabric of …

Mélanges represent a significant component of collisional and accretionary orogenic belts.
We present a comparison of subduction-accretion mélanges of different ages to test how …

The terms mélange and broken formation have been used in different ways in the literature.
The lack of agreement on their definition often leads to confusion and misinterpretations. An …

Most of mélanges occurring in exhumed subduction complexes and orogenic belts are
commonly interpreted as the product of tectonic processes (eg, underplating and return flow) …

The western margin of Myanmar is the northern extension the active Sunda (India-Eurasia)
subduction zone. Coastal regions and offshore islands have remarkable exposures of …

A significant part of mélanges recognized in exhumed convergent margins around the world
has been recently documented to have chiefly originated from masse transport and …

The Küre ophiolite in the Sakarya terrane in northern Anatolia is a Penrose-type ophiolite,
complete with a sheeted dike complex, and includes well-developed volcanogenic massive …

The subduction thrust interface represents a zone of concentrated deformation coupled to
fluid generation, flow, and escape. Here, we review the internal structure of the megathrust …

Detailed structural analysis of the Isla Pelada serpentinite-matrix mélange on Santa Elena
Peninsula, Pacific coast of northwest Costa Rica, elucidates for the spatial distribution and …

For the past 50 years, large parts of the Harz Mountains (eastern Rhenohercynian Zone,
Germany) have been considered to consist of olistostromes of Early Carboniferous age …