TY - JOUR
T1 - Khesinite, Ca4Mg2Fe3+10O4 [(Fe3+10Si2)O36], a new rhönite-group (sapphirine supergroup) mineral from the Negev Desert, Israel - Natural analogue of the SFCA phase
AU - Galuskina, Irina O.
AU - Galuskin, Evgeny V.
AU - Pakhomova, Anna S.
AU - Widmer, Remo
AU - Armbruster, Thomas
AU - Krüger, Biljana
AU - Grew, Edward S.
AU - Vapnik, Yevgeny
AU - Dzierazanowski, Piotr
AU - Murashko, Mikhail
N1 - Publisher Copyright:
© 2016 E. Schweizerbart'sche Verlagsbuchhandlung.
PY - 2017/1/1
Y1 - 2017/1/1
N2 - Khesinite, Ca4Mg2Fe3+10O4 (Fe3+10Si2)O36, is a new member of the rhönite group of the sapphirine supergroup. Khesinite was discovered in thin veins of paralavas within fine-grained gehlenite rocks (hornfels) of the Hatrurim Complex in the Negev Desert, Israel. Paralavas are composed of rankinite, pseudowollastonite (rarelywollastonite),flamite, kalsilite, cuspidine and members of the solid-solution series: Schorlomite-andradite, gehlenite-ackermanite-"Fe3+-gehlenite", magnesioferrite-spinel and fluorapatite-fluorellestadite. Accessory and rare minerals are represented by baryte, walstromite, fresnoite, vorlanite, barioferrite, hematite, perovskite, gurimite, zadovite, aradite and hexacelsian. Electron-microprobe analysis of the holotype khesinite gives the following empirical formula for 40 oxygens and 28 cations: Ca4 (Fe3+8.528Mg1.635Ca0.898Ti4+0.336Ni2+0.217Mn2+0.155Cr3+0.132Fe2+0.098)∑12 [(Fe3+6.827Al2.506Si2.667)S12O40]. Khesinite is black to dark brown. It has semi-metallic lustre and does not show fluorescence. Cleavage and parting are not observed, fracture is irregular. Khesinite has a Mohs' hardness of 6; microhardness VHN50 is 943 kgmm-2. The calculated density is 4.097 g cm--3. In reflected light khesinite is grey with weak internal brown reflections. Reflectance data for the COM(Commission of Ore Mineralogy, IMA) wavelengths vary from ∼13.4% (470 nm) to ∼11.8% (700 nm). The crystal structure of khesinite [P1 a = 10.5363(1), b = 10.9242(2), c = 9.0612(1) Å, a = 106.340(1)°, b = 95.765(1)°, g = 124.373(1)°, V= 780.54(2)Å3] was refined fromX-ray single-crystal data to R1 = 0.046. The khesinite structure is close to that of the synthetic compounds SFCA and SFCAM. Khesinite crystallized in paralava from melt, sometimes forming isolated crystals, but more commonly reaction rims onmagnesioferrite in associationwith pseudowollastonite and flamite at temperature not lower than 1200 °C.
AB - Khesinite, Ca4Mg2Fe3+10O4 (Fe3+10Si2)O36, is a new member of the rhönite group of the sapphirine supergroup. Khesinite was discovered in thin veins of paralavas within fine-grained gehlenite rocks (hornfels) of the Hatrurim Complex in the Negev Desert, Israel. Paralavas are composed of rankinite, pseudowollastonite (rarelywollastonite),flamite, kalsilite, cuspidine and members of the solid-solution series: Schorlomite-andradite, gehlenite-ackermanite-"Fe3+-gehlenite", magnesioferrite-spinel and fluorapatite-fluorellestadite. Accessory and rare minerals are represented by baryte, walstromite, fresnoite, vorlanite, barioferrite, hematite, perovskite, gurimite, zadovite, aradite and hexacelsian. Electron-microprobe analysis of the holotype khesinite gives the following empirical formula for 40 oxygens and 28 cations: Ca4 (Fe3+8.528Mg1.635Ca0.898Ti4+0.336Ni2+0.217Mn2+0.155Cr3+0.132Fe2+0.098)∑12 [(Fe3+6.827Al2.506Si2.667)S12O40]. Khesinite is black to dark brown. It has semi-metallic lustre and does not show fluorescence. Cleavage and parting are not observed, fracture is irregular. Khesinite has a Mohs' hardness of 6; microhardness VHN50 is 943 kgmm-2. The calculated density is 4.097 g cm--3. In reflected light khesinite is grey with weak internal brown reflections. Reflectance data for the COM(Commission of Ore Mineralogy, IMA) wavelengths vary from ∼13.4% (470 nm) to ∼11.8% (700 nm). The crystal structure of khesinite [P1 a = 10.5363(1), b = 10.9242(2), c = 9.0612(1) Å, a = 106.340(1)°, b = 95.765(1)°, g = 124.373(1)°, V= 780.54(2)Å3] was refined fromX-ray single-crystal data to R1 = 0.046. The khesinite structure is close to that of the synthetic compounds SFCA and SFCAM. Khesinite crystallized in paralava from melt, sometimes forming isolated crystals, but more commonly reaction rims onmagnesioferrite in associationwith pseudowollastonite and flamite at temperature not lower than 1200 °C.
KW - Hatrurim Complex.
KW - Raman
KW - SFCA
KW - SFCAM
KW - crystal structure
KW - dorrite
KW - ferrites
KW - khesinite
KW - new mineral
KW - pyrometamorphism
KW - rhönite group
KW - sapphirine supergroup
UR - http://www.scopus.com/inward/record.url?scp=85015785942&partnerID=8YFLogxK
U2 - 10.1127/ejm/2017/0029-2589
DO - 10.1127/ejm/2017/0029-2589
M3 - Article
AN - SCOPUS:85015785942
SN - 0935-1221
VL - 29
SP - 101
EP - 116
JO - European Journal of Mineralogy
JF - European Journal of Mineralogy
IS - 1
ER -