Abstract
The South-East Greenland margin is a type example of a volcanic rifted margin. The margin is characterised by a broad seaward-dipping reflector sequence (SDRS) composed of basalt that onlaps continental (mainly Precambrian) crust to the west and terminates eastward in oceanic crust of early Tertiary age (Figs 1, 2).
Cite
CITATION STYLE
APA
Larsen, H. C., Duncan, R. S., Allan, J. F., & ODP Leg 163 shipboard party. (1996). ODP Leg 163, South-East Greenland volcanic rifted margin. Bulletin Grønlands Geologiske Undersøgelse, 172, 103–112. https://doi.org/10.34194/bullggu.v172.6753
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