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Andreas Magganas
Researcher at National and Kapodistrian University of Athens
Publications - 61
Citations - 574
Andreas Magganas is an academic researcher from National and Kapodistrian University of Athens. The author has contributed to research in topics: Basalt & Ultramafic rock. The author has an hindex of 10, co-authored 60 publications receiving 461 citations. Previous affiliations of Andreas Magganas include Athens State University & Complutense University of Madrid.
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The geochemistry of fluids from an active shallow submarine hydrothermal system: Milos island, Hellenic Volcanic Arc
Eugenia Valsami-Jones,Emmanuel Baltatzis,Elizabeth H. Bailey,Adrian J. Boyce,Jane Alexander,Andreas Magganas,L. Anderson,Susan Waldron,Kristin Vala Ragnarsdottir +8 more
TL;DR: In this paper, two main types of fluids were identified: low-chlorinity fluids containing low concentrations of alkalis (potassium, lithium, sodium), and high concentrations of silica and sulphate; and high-chlorification fluids containing high concentrations (salinity and calcium) and lower concentrations (silica, sulphate, and sulphates) of sulphates.
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Subduction-related rodingites from East Othris, Greece: Mineral reactions and physicochemical conditions of formation
TL;DR: In this paper, the authors classified rodingite dykes into two types: prehnite and vesuvianite, and showed that the latter is more abundant than the former.
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Constraints on the petrogenesis of Evros ophiolite extrusives, NE Greece
TL;DR: The incomplete and dismembered Evros ophiolite is situated in Thrace, NE Greece, and belongs to the Circum-Rhodope Belt (CRB), its age is considered to be Jurassic-Lower Cretaceous.
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Marginal basin—volcanic arc origin of metabasic rocks of the Circum-Rhodope Belt, Thrace, Greece
TL;DR: In this article, a detailed petrographical study revealed that the metavolcanics consist of four lava types: pyroxeno-phyric, aphyric oligophyric and porphyric felsites.
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Composition, melting and evolution of the upper mantle beneath the Jurassic Pindos ocean inferred by ophiolitic ultramafic rocks in East Othris, Greece
TL;DR: In this paper, the East Othris ophiolite in Central Greece consists of serpentinites, of harzburgite precursors, as well as serpentinized lherzolites, which have been intruded by thin dykes of olivine-rich and olivinespoor pyroxenites.