Crustal composition of the Møre Margin and compilation of a conjugate Atlantic margin transect
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文摘

The basement at the mid-Norwegian Møre Margin is dominantly felsic in composition.

A lower crustal body is interpreted as a mixture of continental blocks and eclogite.

The thickness of the outer lower crustal body is twice as thick on the East Greenland Margin.

The thinning during this first phase of post-Caledonian extension was highest for proto Norway.

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