First Occurrence of Titanian Hydroxylclinohumite in Marble-Hosting Gem Spinel Deposits, Luc Yen, Vietnam

Author:

Krivovichev Vladimir G.1ORCID,Kuksa Katherine A.2,Sokolov Pavel B.3,Panikorovskii Taras L.4,Bocharov Vladimir N.5ORCID,Gussiås Geir Atle6

Affiliation:

1. Department of Mineralogy, Institute of Earth Sciences, St. Petersburg University, University Embankment. 7/9 (V.G.K.), 199034 St. Petersburg, Russia

2. Department of Geomorphology, Institute of Earth Sciences, St. Petersburg University, University Emb. 7/9, 199034 St. Petersburg, Russia

3. SOKOLOV Co. Ltd., Gatchinskaya str., 11/A, 7N, 197136 St. Petersburg, Russia

4. Laboratory of Nature-Inspired Technologies and Environmental Safety of the Arctic, Kola Science Centre, Russian Academy of Sciences, 14 Fersman Street, 184200 Apatity, Russia

5. Geo Environmental Centre “Geomodel”, the Research Park, St. Petersburg University, Ul’yanovskaya Str. 1, 198504 St. Petersburg, Russia

6. BalderGems Co., Yen The 36000, YB, Vietnam

Abstract

In this paper, we report the very first occurrence of titanian hydroxylclinohumite in the marble-hosted gem spinel deposits of the Luc Yen district, northern Vietnam. Hydroxylclinohumite is anhedral and associated with forsterite, tremolite, pargasite, diopside, spinel, dolomite and calcite. Hydroxylclinohumite from the Luc Yen deposit was characterized via electron microprobe analysis, single-crystal X-ray diffraction study, and Raman spectrometry. The average composition is (Mg0.69Ti0.29Fe0.02)Σ1.00Mg7.91(SiO4)4.08[(OH)1.10F0.53O0.37]Σ2.00. (ideally (Mg0.7Ti0.3)Σ1Mg8.0(SiO4)4[(OH)1.2F0.5O0.3]2). The compositions of the analyzed hydroxylclinohumites have a narrow range of Mg/(Mg+Fe+Ti) values (0.96–0.97) and a defined hydroxylclinohumite solid-solution series. Compared with other occurrences, the Luc Yen hydroxylclinohumite has an average titanium content, which attains 0.31 atoms per formula unit (3.93 wt.% TiO2) and a low iron content of 0.04 atoms per formula unit (0.42 wt.% FeO). The formation of hydroxylclinohumite is favored by the proportion of Mg, and Si in the precursor rocks and the increased activity of H2O in the fluid phase.

Funder

Russian Science Foundation

Publisher

MDPI AG

Subject

Geology,Geotechnical Engineering and Engineering Geology

Reference65 articles.

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3. Crystal chemistry of silicate minerals of geophysical interest;Papike;Rev. Geophys. Sp. Phys.,1976

4. Stability of hydrous magnesium silicates in the mantle transition zone;Kanzaki;Phys. Earth Plan. Inter.,1991

5. First synthesis of the hydroxyl end-member of humite, Mg7Si3O12(OH)2;Wunder;Amer. Miner.,1995

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