Origin and serpentinization of ultramafic rocks of Manipur Ophiolite Complex in the Indo-Myanmar subduction zone, Northeast India
The Manipur Ophiolite Complex (MOC) is part of the Manipur-Nagaland ophiolite belt
(MNOB). The belt is exposed in the eastern margin of the Indo-Myanmar Ranges (IMRs),
which formed by the collision between the India and Myanmar continental plates. Several
contrasting views were put forward concerning the origin of the MNOB. The complex
represents a dismembered ophiolite sequence with serpentinite as the largest litho-unit
formed. Petrography and Raman spectroscopy of the serpentinite suggest that they are …
(MNOB). The belt is exposed in the eastern margin of the Indo-Myanmar Ranges (IMRs),
which formed by the collision between the India and Myanmar continental plates. Several
contrasting views were put forward concerning the origin of the MNOB. The complex
represents a dismembered ophiolite sequence with serpentinite as the largest litho-unit
formed. Petrography and Raman spectroscopy of the serpentinite suggest that they are …
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