Metasomatic evolution of coesite-bearing diamondiferous eclogite from the Udachnaya Kimberlite
- A coesite-bearing diamondiferous eclogite from the Udachnaya kimberlite (Daldyn field, Siberian craton) has been studied to trace its complex evolution recorded in rock-forming and minor mineral constituents. The eclogite sample is composed of rock-forming omphacite (60 vol%), garnet (35 vol%) and quartz/coesite (5 vol%) and contains intergranular euhedral zoned olivine crystals, up to 200 µm long, coexisting with phlogopite, orthopyroxene, clinopyroxene (secondary), K-feldspar, plagioclase, spinel, sodalite and djerfisherite. Garnet grains are zoned, with a relatively homogeneous core and a more magnesian overgrowth rim. The rim zones further differ from the core in having higher Zr/Y (6 times that in the cores), ascribed to interaction with, or precipitation from, a kimberlite-related melt. Judging by pressure-temperature estimates (~1200 °C; 6.2 GPa), the xenolith originated at depths of ~180–200 km at the base of the continental lithosphere. The spatial coexistence of olivine, orthopyroxene and coesite/quartz with K-Na-Cl minerals in the xenolith indicates that eclogite reacted with a deep-seated kimberlite melt. However, Fe-rich olivine, orthopyroxene and low-pressure minerals (sodalite and djerfisherite) likely result from metasomatic reaction at shallower depths during transport of the eclogite by the erupting kimberlite melt. Our results demonstrate that a mixed eclogitic-peridotitic paragenesis, reported previously from inclusions in diamond, can form by interaction of eclogite and a kimberlite-related melt.
Verfasserangaben: | Denis Mikhailenko, Alexander Golovin, Andrey Korsakov, Sonja AulbachORCiD, Axel GerdesORCiDGND, Alexey Ragozin |
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URN: | urn:nbn:de:hebis:30:3-543435 |
DOI: | https://doi.org/10.3390/min10040383 |
ISSN: | 2075-163X |
Titel des übergeordneten Werkes (Englisch): | Minerals |
Verlag: | MDPI |
Verlagsort: | Basel |
Dokumentart: | Wissenschaftlicher Artikel |
Sprache: | Englisch |
Datum der Veröffentlichung (online): | 24.04.2020 |
Datum der Erstveröffentlichung: | 24.04.2020 |
Veröffentlichende Institution: | Universitätsbibliothek Johann Christian Senckenberg |
Datum der Freischaltung: | 06.05.2020 |
Freies Schlagwort / Tag: | Udachnaya pipe; eclogite; kimberlite; lithospheric mantle; melting; metasomatism |
Jahrgang: | 10 |
Ausgabe / Heft: | 383 |
Seitenzahl: | 24 |
Bemerkung: | This is an open access article distributed under the Creative Commons Attribution License which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. |
HeBIS-PPN: | 466010451 |
Institute: | Geowissenschaften / Geographie / Geowissenschaften |
DDC-Klassifikation: | 5 Naturwissenschaften und Mathematik / 55 Geowissenschaften, Geologie / 550 Geowissenschaften |
Sammlungen: | Universitätspublikationen |
Lizenz (Deutsch): | Creative Commons - Namensnennung 4.0 |