Midbarite, Ca <sub>3</sub> Mg <sub>2</sub> (V <sub>2</sub> Si)O <sub>12</sub> , a new member of the garnet supergroup from the Hatrurim Complex, Israel

A new garnet named midbarite, Ca 3 Mg 2 (V 2 Si)O 12 , has been discovered in a paralava of the pyrometamorphic Hatrurim Complex in the Hatrurim Basin near Mount Ye'elim in the Negev Desert, Israel.This paralava also contains esseneite, minerals of the levantite-latiumite series, garnet of the andradite-schorlomite series, and wollastonite as well as subordinate 0.15 Al 0.01 ) 2.99 O 12 .There is only one strong band in the Raman spectrum of midbarite at 824 cm -1 , which is related to (VO 4 ) 3-vibrations.Midbarite is an accessory mineral in the paralava, and its paragenesis indicates that it formed in the sanidinite facies under increased pressure.

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Publication Details

Journal
Mineralogical Magazine
Published
2026-02-05
DOI
https://doi.org/10.1180/mgm.2026.10202
Primary Topic
Crystal Structures and Properties
Type
article
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article

Midbarite, Ca 3 Mg 2 (V 2 Si)O 12 , a new member of the garnet supergroup from the Hatrurim Complex, Israel

Irina O. Galuskina, Maria Książek, Yevgeny Vapnik, Evgeny V. Galuskin et al.
Mineralogical Magazine
Crystal Structures and Properties
article

Midbarite, Ca 3 Mg 2 (V 2 Si)O 12 , a new member of the garnet supergroup from the Hatrurim Complex, Israel

Irina O. Galuskina, Maria Książek, Yevgeny Vapnik, Evgeny V. Galuskin, Beata Marciniak-Maliszewska, Joachim Kusz
article en

Abstract

A new garnet named midbarite, Ca 3 Mg 2 (V 2 Si)O 12 , has been discovered in a paralava of the pyrometamorphic Hatrurim Complex in the Hatrurim Basin near Mount Ye'elim in the Negev Desert, Israel.This paralava also contains esseneite, minerals of the levantite-latiumite series, garnet of the andradite-schorlomite series, and wollastonite as well as subordinate 0.15 Al 0.01 ) 2.99 O 12 .There is only one strong band in the Raman spectrum of midbarite at 824 cm -1 , which is related to (VO 4 ) 3-vibrations.Midbarite is an accessory mineral in the paralava, and its paragenesis indicates that it formed in the sanidinite facies under increased pressure.

Mineralogical Magazine
Ben-Gurion University of the Negev (IL), University of Warsaw (PL), University of Silesia in Katowice (PL)
Openalex Percentile: Top 66%
Crystal Structures and Properties
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