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Kerguelen Plateau formation

Age:119 to 34 Ma
Geologic Time:Phanerozoic
Reference for age:Frey, F. A.; Coffin, M. F.; Wallace, P. J,; Weis, D. (2003). Frey, F. A.; Coffin, M. F.; Wallace, P. J.; et al., eds. "Leg 183 Summary: Kerguelen Plateau-Broken Ridge—A Large Igneous Province"
Where:Southern Indian Ocean
Map:
The Kerguelen Plateau is a Large Igneous Province (LIP) that formed on the Kerguelen hotspot.

The Kerguelen Plateau Large Igneous Province itself consists of the following large-scale structures:

The Southern Kerguelen Plateau (SKP) - 119–110 Ma;
The Elan Bank - 108–107 Ma;
The Central Kerguelen Plateau (CKP) - 101–100 Ma;
The Broken Ridge (connected to CKP before the Eocene breakup) - 95–94 Ma;
The Skiff Bank (east of Kerguelen archipelago) - 69–68 Ma;
The Northern Kerguelen Plateau (NKP) - 35–34 Ma;

Other related structures probably caused by the same hotspot are:

Ninety East Ridge - 82–38 Ma
The Bunbury Basalt (western Australia) formed 132–123 Ma;
The Rajmahal Traps in northeast India 118–117 Ma;
Lamprophyres in India and Antarctica 115–114 Ma.

Ref: Frey, F. A.; Coffin, M. F.; Wallace, P. J,; Weis, D. (2003). Frey, F. A.; Coffin, M. F.; Wallace, P. J.; et al., eds. "Leg 183 Summary: Kerguelen Plateau-Broken Ridge—A Large Igneous Province"

http://www-odp.tamu.edu/publications/183_sr/VOLUME/SYNTH/SYNTH.PDF
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