evidence that the Wandel Hav Strike-Slip Mobile Belt may have been formed already in Late Palaeozoic time during onset of Pangean break-up; evidence for strike-slip movements of this age is, however, largely

The Wandel Hav Strike-Slip Mobile Belt – A Mesozoic plate boundary in North Greenland - Håkansson, E. & Pedersen, S.A.S.

The Wandel Hav strike-slip mobile belt; a Mesozoic plate boundary in north Greenland The Wandel Valley Formation (Early-Middle Ordovician) of North Greenland and its correlatives The Wandrawandian Tuffs; felsic

Wandel Hav basin of NE Greenland.

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The Wandel Hav strike-slip mobile belt; a Mesozoic plate boundary in north Greenland. palaeogene transpressional The Wandel Valley Formation (Early-Middle Ordovician) of North Greenland and its correlatives.

Dextral strike-slip tectonism in the Wandel Hav Mobile Belt was the result of ∼N-S compression due to a general northward movement of the Greenland plate.

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