最終更新日:2024/08/06

(paleogeography, paleogeology) A Greenland-sized paleo-microcontinent in the Neo-Tethys Ocean that rifted from the north of Africa portion of the supercontinent of Gondwana and accreted to the south of Europe portion of the supercontinent of Laurasia, and thence subducted.

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Greater Adria

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