Srilankite

srilankite

baddeleyite

ilmenite

rutile

Images

Formula: Ti2ZrO6
Simple oxide of titanium and zirconium, samarskite group, columbite supergroup
Crystal System: Orthorhombic
Specific gravity: 4.6 measured, 4.77 calculated
Hardness: 6½
Colour: Black, blackish brown
Luminescence: Not fluorescent under UV
Environments

Igneous environments
Placers

Localities

At the Atlantis II Fracture Zone, Southwest Indian Ridge, Indian Ocean, srilankite in a gabbroic vein cutting a serpentinised peridotite was collected using submersible SHINKAI 6500 of the Japanese Marine Science Technology Center. Srilankaite occurs in small patches less than 30 microns across, always co-existing with ilmenite and rutile. Zircon, apatite and phlogopite also occur as accessory minerals in the vein.
The srilankite appears to have co-crystallised with ilmenite and rutile from melts rather than through metamorphic recrystallisation. Geochemical interactions between peridotite and melt in the upper mantle may effectively concentrate incompatible elements in a modified melt, which may precipitate srilankite directly (AM 89.759-766).

At the type locality, Rakwana, Ratnapura District, Sabaragamuwa Province, Sri Lanka, srilankite occurs in pebbles from a placer gemstone mine. The pebbles are mainly zirconolite and baddeleyite with minor amounts of geikielite, spinel and perovskite. Srilankite occurs as inclusions less than 1 mm across in such pebbles (AM 69.210-215).

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