Genesis and evolution of the Archaean subcontinental lithospheric mantle beneath the periphery of the Dharwar Craton

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Other Title
  • 南インド,ダルワールクラトン周辺部における始生代大陸下リソスフェアマントルの形成とその進化

Description

The existence of long lived enriched lithospheric mantle is known beneath the Dharwar and periphery area in south India. Although the event of mantle enrichment occurred at the late Archaean is now controversial, but it is significant topic to reveal the early history of the Dharwar craton. It is understood that the late Archaean subduction was major event in the history of the Dharwar craton and generated the long lived enriched lithospheric mantle.

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