Results 51 to 60 of about 5,793 (215)
Supercritical fluids are ideal media for mass transfer from the subducting slab into the mantle wedge. However, little is known about the Mg‐Fe isotope compositions of supercritical fluids in subduction zones.
Tie‐Nan Chen +5 more
doaj +1 more source
A novel chemical scheme for flotation of rutile from eclogite tailing
A novel chemical scheme for the flotation of rutile from eclogite tailings has been developed in this work. It consists of lead ion as the activator, sodium fluorosilicate (SF) as the depressant, and styryl phosphonic acid (SPA) and n-octyl alcohol (OCT)
Bo Xu +5 more
doaj +1 more source
International audienceIn many orogens, high-pressure (HP) metamorphic rocks such as eclogite occur as lenses in quartzofeldspathic gneiss that equilibrated at much lower pressures.
Whitney, Donna L. +4 more
core +1 more source
Eclogite-facies shear zones--deep crustal reflectors? [PDF]
Strongly foliated eclogite-facies rocks in 30-150 m thick shear zones of Caledonian age occur within a Grenvillian garnet granulite-facies gabbro-anorthosite terrain in the Bergen Arcs of Norway. The predominant eclogite-facies mineral assemblages in the
Theresa M. Boundy +7 more
core +1 more source
The immense Central Asian Orogenic Belt (CAOB) witnessed the transition from the Pan‐Rodinian Mirovoi Ocean to the Paleo-Asian Ocean, but the final closure of the Mirovoi Ocean remains unexplored so far.
Mingshuai Zhu
core +1 more source
Petro-structural geology of the Northern Adula Nappe Complex (Central Penninic Alps, Switzerland)
The Adula Nappe Complex is the largest fragment of Penninic continental crust in the Central Alps, where it deformed alongside the Valais Ocean ophiolites and metasediments.
Fabio Zulbati
doaj +1 more source
Origin and evolution of the Variscan Léon eclogites: insights from zircon and garnet petrochronology [PDF]
Eclogites record the deep burial and exhumation of crustal terranes, which are key tectonic markers in the evolution of orogenic belts. Unraveling the evolution of eclogites and eclogite-bearing terranes may nevertheless be challenging, especially in old
L. Tual +9 more
doaj +1 more source
Discovery of eclogite facies carbonate rocks from the LindÅs Nappe, Caledonides, Western Norway [PDF]
Eclogite facies carbonate rocks have been discovered associated with the granulite–eclogite transitional rocks within Bergen Arc system, Caledonian Orogen of western Norway. The local occurrences of marbles and calc-silicates are found subparallel to the
Essene, E. J. +7 more
core +2 more sources
ABSTRACT Rationale Nitrogen (N) abundance and isotopic compositions in silicate rocks are commonly measured by sealed‐tube continuous‐flow isotope ratio mass spectrometry (CF‐IRMS), but combustion protocols vary widely. It remains uncertain how the quality of data obtained from different published methods compares for differing sample types. Methods To
Fawn S. M. Holland +4 more
wiley +1 more source
The article gives a detailed mineralogical, petrographic and petrogeochemical characteristics of eclogites of the Beloretsk metamorphic complex (BMK).
S. G. Kovalev, E. A. Timofeeva
doaj +2 more sources

