In continental subduction complexes minor volumes of high-pressure mafic rocks (eclogites)
often co-exist with much more abundant felsic (granitic) and metasedimentary rocks, which …

Fluids in subduction zones contain various aqueous species and cause metasomatic
reactions as well as hydration (ie, serpentinization) at the slab–mantle interface. However …

Two distinct types of podiform chromitites have been extensively described within the mantle
sections of Neoproterozoic ophiolites in Saudi Arabia and Phanerozoic ophiolites in Oman …

Subduction-zone fluid–rock interactions have a direct impact onto elemental and isotopic
homogeneity of progressively buried and exhumed crustal lithologies by providing an …

Центр коллективного пользования «Изотопно-геохимические исследования»,
организованный на базе Аналитического отдела Института геохимии им. АП …

In order to assess the geochemical effects of retrograde metamorphic rehydration, fluid
metasomatism, and the fluid-mobile elements (FMEs) budget in the case of oceanic and …

Within subduction-accretion complexes, high-pressure rocks (blueschists, eclogites) are
commonly juxtaposed with lower-grade rocks, which represent their retrograded …

Ophiolites are a set of oceanic rocks with different appearances and mineralogy in the
world's largest orogenic belt, from the Alpine to the Himalayas. The ophiolites of Iran are …

Centre of Isotopic and Geochemical Research based on the Analytical Department of
Vinogradov Institute of Geochemistry SB RAS (Irkutsk) performs a wide range of analytical …

Присутствие водных флюидов является важным фактором, ускоряющим диффузию,
рост минеральных фаз и реакции в процессе метаморфизма, даже не будучи одним из …