H in Titanites

• Beran A (1970) Messung des Ultrarot-Pleochroismus von Mineralen. IX. Der Pleochroismus der OH-Streckfrequenz in Titanit. Tschermaks Mineralogische und petrographische Mitteilung 14, 1-5.

• Hawthorne FC, Groat La, Raudsepp M, Ball NA, Kimata M, Spike FD, Gaba R, Halden NM, Lumpkin GR, Ewing RC, Greegor RB, Lytle FW, Ercit TS, Rossman GR, WIcks FJ, Ramik RA, Sherriff BL, Fleet ME, McCammon C (1991) Alpha-decay damage in titanite. American Mineralogist 76, 370-396.

• Hammer VMF (1989) Hydroxyl content of rutile and titanite from various parageneses by infra-red spectroscopy. Mitteilungen der Oesterreichischen Mineralogischen Gesellschaft,  134: 7-12. (in German) 
• Hammer VMF, Beran A, Endisch D, Rauch F (1996) OH concentrations in natural titanites determined by FTIR spectroscopy and nuclear reaction analysis. European Journal of Mineralogy  8, 281-8.  

• Zhang M, Salje EKH, Malcherek T, Bismayer U, Groat LA (2000) Dehydration of Metamict Titanite: an INfrared Spectroscopic Study. Canadian Mineralogist 38, 119-130.

• Zhang M, Groat LA, Salje EKH, Beran A (2001) Hydrous species in crystalline and metamict titanites. American Mineralogist  86, 904-909.

• Zhang M, Salje EKH, Carpenter MA, Wang Y, Groat LA, Lager GA, Wang L, Beran A, Gismayer U (2007) Temperature dependence of IR absorption of hydrous/hydroxyl species in minerals andsynthetic materials American Mineralogist  92, 1502-1517.

•  Sakamaki K, Ogasawara Y (2014)  Hydroxyl in clinopyroxene and titanite in a UHP diamond-free garnet-clinopyroxene rock from the
  Kokchetav Massif, northern Kazakhstan. International Geology Review 56, 133-149.