Mélanges through time: Life cycle of the world's largest Archean mélange compared with Mesozoic and Paleozoic subduction-accretion-collision mélanges
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 …
We present a comparison of subduction-accretion mélanges of different ages to test how …
Diagnostic features and field-criteria in recognition of tectonic, sedimentary and diapiric mélanges in orogenic belts and exhumed subduction-accretion complexes
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 …
subduction-accretion complexes cause obfuscation of primary block-in-matrix fabric of …
Mechanisms and processes of stratal disruption and mixing in the development of mélanges and broken formations: Redefining and classifying mélanges
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 …
The lack of agreement on their definition often leads to confusion and misinterpretations. An …
[HTML][HTML] Mélanges and chaotic rock units: Implications for exhumed subduction complexes and orogenic belts
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) …
commonly interpreted as the product of tectonic processes (eg, underplating and return flow) …
Tectonic, diapiric and sedimentary chaotic rocks of the Rakhine coast, western Myanmar
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 …
subduction zone. Coastal regions and offshore islands have remarkable exposures of …
Polygenetic mélanges: a glimpse on tectonic, sedimentary and diapiric recycling in convergent margins
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 …
has been recently documented to have chiefly originated from masse transport and …
[HTML][HTML] Seafloor spreading structure, geochronology, and tectonic evolution of the Küre ophiolite, Turkey: a Jurassic continental backarc basin oceanic lithosphere in …
G Alparslan, Y Dilek - Lithosphere, 2018 - pubs.geoscienceworld.org
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 …
complete with a sheeted dike complex, and includes well-developed volcanogenic massive …
Structural evolution and deformation kinematics of a subduction-related serpentinite-matrix mélange, Santa Elena Peninsula, northwest Costa Rica
J Escuder-Viruete, PO Baumgartner - Journal of Structural Geology, 2014 - Elsevier
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 …
Peninsula, Pacific coast of northwest Costa Rica, elucidates for the spatial distribution and …
Magnetic fabric of Ocean Plate Stratigraphy mélanges: a tool for unravelling protracted histories of oceanic plates from seafloor spreading to tectonic emplacement …
Multiple magnetic fabrics, referred to as F1–F5, were revealed through the anisotropy of
magnetic susceptibility in an Ocean Plate Stratigraphy (OPS) mélange of the Neoproterozoic …
magnetic susceptibility in an Ocean Plate Stratigraphy (OPS) mélange of the Neoproterozoic …
Large-scale Variscan shearing at the southeastern margin of the eastern Rhenohercynian belt: a reinterpretation of chaotic rock fabrics in the Harz Mountains …
CH Friedel, H Huckriede, B Leiss, M Zweig - International Journal of Earth …, 2019 - Springer
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 …
Germany) have been considered to consist of olistostromes of Early Carboniferous age …