Intraplate volcanism off South Greenland: caused by glacial rebound?


Contact
Gabriele.Uenzelmann-Neben [ at ] awi.de

Abstract

Plate tectonic mechanisms explain most of the dominant types of volcanism. Intraplate volcanism has been attributed to hotspots associated with mantle plumes, although alternative explanations have been proposed for settings not fed by plumes. We report young intraplate volcanism in an amagmatic margin south of Greenland in a 40-Myr-old plate. An elongated structure with a length of 110km and a height of 2500 m above basement extends at an oblique angle to the Mid Atlantic ridge and the fracture zones. We propose that this structure is related to reactivation of a rudimentary fracture zone by edge-driven convection across Minna Fracture Zone and partial melting caused by glacial rebound during the periodic melting of ice on Greenland in the last 3 Myr. © 2012 The Authors Geophysical Journal International © 2012 RAS.



Item Type
Article
Authors
Divisions
Programs
Publication Status
Published
Eprint ID
26009
DOI https://www.doi.org/10.1111/j.1365-246x.2012.05468.x

Cite as
Uenzelmann-Neben, G. , Schmidt, D. N. , Niessen, F. and Stein, R. (2012): Intraplate volcanism off South Greenland: caused by glacial rebound? , Geophysical Journal International, 190 (1), pp. 1-7 . doi: https://www.doi.org/10.1111/j.1365-246x.2012.05468.x


Share


Citation

Research Platforms
N/A

Campaigns
N/A


Actions
Edit Item Edit Item