Structure of the SE Greenland margin from seismic reflection and refraction data: Implications for nascent spreading center subsidence and asymmetric crustal accretion during North Atlantic opening

Author:

Hopper John R.1,Dahl-Jensen Trine2,Holbrook W. Steven3,Larsen Hans Christian1,Lizarralde Dan4,Korenaga Jun5,Kent Graham M.6,Kelemen Peter B.7

Affiliation:

1. Danish Lithosphere Center; Copenhagen Denmark

2. Geological Survey of Denmark and Greenland; Copenhagen Denmark

3. Department of Geology and Geophysics; University of Wyoming; Laramie Wyoming USA

4. School of Earth and Atmospheric Sciences; Georgia Institute of Technology; Atlanta Georgia USA

5. Department of Earth and Planetary Science; University of California, Berkeley; Berkeley California USA

6. Scripps Institution of Oceanography; University of California, San Diego; La Jolla California USA

7. Department of Geology and Geophysics; Woods Hole Oceanographic Institution; Woods Hole Massachusetts USA

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference73 articles.

1. Eocene-Miocene magnetostratigraphy of the southeast Greenland margin and western Irminger Basin;Ali;Proc. Ocean Drill. Program Sci. Results,1998

2. Plume-driven plumbing and crustal formation in Iceland;Allen;J. Geophys. Res.,2002

3. Asymmetric spreading in back-arc basins;Barker;Nature,1980

4. Crustal structure of the Edoras Bank margin and mantle thermal anomalies beneath the North Atlantic;Barton;J. Geophys. Res.,1997

5. Post-breakup basaltic magmatism along the East Greenland Tertiary rifted margin;Bernstein;Earth Planet. Sci. Lett.,1998

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