Formula: CaTi(SiO4)O
Nesosilicate (insular SiO4 groups), titanium-bearing mineral


Keilhauite is an yttrium-bearing variety of titanite

Crystal System: Monoclinic
Specific gravity: 3.48 to 3.6 measured, 3.53 calculated
Hardness: 5
Streak: White
Colour: Brown, green, yellow, red
Solubility: Insoluble in water, nitric and sulphuric acid; slightly soluble in hydrochloric acid
Common impurities: Fe,Y,Mn,Al,Ce,Sr,Na,Nb,Ta,Al,Mg,V,F,Zr,Sn

Igneous environments (common)
Sedimentary environments (rarely)
Metamorphic environments
Hydrothermal environments

Titanite occurs as a primary titanium mineral in small crystals as a common accessory in intermediate and quartz-rich plutonic rocks, in pegmatites and rarely as a detrital mineral in some sedimentary deposits.
In igneous rocks it is found mainly in diorite, syenite and granite, and it is much less common in volcanic rocks (Lauf p74).
In metamorphic rocks titanite is found primarily in gneiss and schist that is rich in ferromagnesian minerals. It is also found in skarn and in calcium-rich Alpine fissures (Lauf p75).
In regional metamorphic environments it occurs as crystals of considerable size. It is a mineral of the prehnite-pumpellyite, greenschist, amphibolite and blueschist facies.
Associated minerals are iron ores, pyroxene, amphibole, scapolite, zircon, apatite, feldspar and quartz.
Hydrothermal titanite is a common alteration product of titanium-bearing minerals such as ilmenite, which may be directly replaced by titanite, or it may contribute titanium to hydrothermal fluids allowing growth of titanite in nearby vugs or pore spaces. It forms over a large temperature range, at least 200oC to 400oC, and may be associated with actinolite, biotite, calcite, chlorite, clinopyroxene, epidote, garnet, quartz and wollastonite (AofA).

Titanite may be found in granite, granodiorite, diorite, syenite, nepheline syenite, gneiss, schist and limestone.

Alteration products of titanite include anatase, sometimes mixed with quartz, and rutile. Replacement of detrital titanite by rutile, calcite and quartz under authigenic conditions in limestone has been reported (Lauf p76).


The Capelinha district, Minas Gerais, Brazil, is made up of low-grade metamorphic mica schist and phyllite with layers of quartzite. The titanite-bearing vein is a skarn made of feldspar, quartz, epidote, hornblende, titanite and minor magnetite (Lauf p83).

At lots 10 and 11 of concession 1, Bathurst Township, Lanark County, Ontario, Canada (DeWitts corner), the deposit is located in the Grenville Geological Province, which consists mostly of marble, gneiss, and quartzite. Syenite-migmatite was also reported in the area where the vein-dikes are located. Characteristic features of the vein-dikes include the fact that perfectly formed euhedral crystals of different minerals can often be found floating in calcite with no points of contact with the walls. Sometimes these crystals have inclusions of calcite, irregular or rounded in shape. It has been argued that at least some of the vein-dikes were formed as a result of melting of Grenville marble.
Titanite is a rare mineral at DeWitts Corners. It occurs as short-prismatic crystals to 8 mm together with diopside and is most commonly found on specimens on, or adjacent to, the wallrock of the vein-dikes (R&M 97.6.556-564).

At Mont Saint-Hilaire, Quebec, Canada, titanite occurs in nepheline syenite (Lauf p74).

In Ontario, Quebec, Canada, titanite is widespread in the Grenville marbles (Lauf p75).

Near El Alamos, Baja California, Mexico, titanite occurs in a granite pegmatite (Lauf p74).

Near Arundal, Norway, titanite occurs in a granite pegmatite (Lauf p74).

At Mulla Ghori, Zagi mountains, Pakistan, titanite occurs in an alkaline pegmatite (Lauf p74).

At the Saranovskiy mine, central Urals, Russia, chromium-rich titanite occurs with chromium-rich amesite, chromite and other species (Lauf p74).

In the Khibiny and Lovozero massifs, Kola peninsula, Russia, titanite occurs in nepheline syenite (Lauf p74).

At Land's End, Cornwall, England, UK, titanite occurs in schist (Lauf p75).

In the San Jacinto mountains, Riverside county, California, USA, titanite with inclusions of andesine and quartz occurs in granodiorite (Lauf p74).

At the Crestmore quarry, Riverside county, California, USA, titanite occurs in schist (Lauf p75).

At the Ojibway No. 1 mine, Ojibway Mine, Ojibway, Keweenaw county, Michigan, USA, a 0.47 mm gemmy titanite crystal has been found on a substrate of crystallised chamosite (R&M 97.4.358).

Amity, Town of Warwick, Orange county, New York, USA, is an area of granite intrusions into marble and associated gneiss. The marble is mostly composed of white crystalline calcite that often has small flakes or spheres of graphite and phlogopite. Titanite occurs as opaque, classic wedge-shaped brown individual crystals, associated with scapolite and augite. Crystals are relatively large for the species, in some cases measuring more than 5 cm (R&M 96.5.440).

The Purple Diopside Mound, Rose Road, Pitcairn, St. Lawrence county, New York, USA, is situated in marble. The development of veins of large crystals probably occurred as a result of fluid penetration from a concurrent intrusion. Many of the minerals of interest to collectors formed during this primary event, with additional species resulting from the subsequent alteration of scapolite. There seems to be little, if any, secondary, late-stage mineralisation present.
Titanite occurs sparingly as flattened, lustrous, black crystals to approximately 4 cm, associated with scapolite and sometimes as isolated crystals in calcite. Millimetre-sized black titanite crystals occur with diopside on the steep hill behind the Purple Diopside Mound (R&M 96.6.552).

At the Pyrites Mica mine, St Lawrence county, New York, USA, titanite is associated with diopside and meionite (R&M 93.4.343).

Near the crest of the Blue Ridge, Roanoke county, Virginia, USA, pseudomorphs of anatase after titanite have been reported (Lauf p76).


lawsonite and titanite to zoisite, rutile, quartz and H2O
3CaAl2(Si2O7)(OH)2.H2O + CaTi(SiO4)O → 2Ca2Al3[Si2O7][SiO4]O(OH) + TiO2 + SiO2 +5H2O
The lawsonite - titanite assemblage is characteristic of the lower blueschist facies (Lauf p76).

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