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Hydrous olivine (Mg1−y Fe2+y)2−x vx SiO4H2x– a new DHMS phase of variable composition observed as nanometer-sized precipitations in mantle olivine

✍ Scribed by N. R. Khisina; R. Wirth


Publisher
Springer-Verlag
Year
2002
Tongue
English
Weight
721 KB
Volume
29
Category
Article
ISSN
0342-1791

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