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 hot spots associated with mantle plumes, though 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 Ma old plate. An elongated structure with a length of 110 km 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 Ma.



Item Type
Conference (Poster)
Authors
Divisions
Programs
Publication Status
Published
Event Details
AGU Fall meeting, 02 Dec 2012 - 06 Dec 2012, San Francisco, USA.
Eprint ID
31202
Cite as
Uenzelmann-Neben, G. , Schmidt, D. N. , Niessen, F. and Stein, R. (2012): Intraplate volcanism off South Greenland: Caused by glacial rebound? , AGU Fall meeting, San Francisco, USA, 2 December 2012 - 6 December 2012 .


Share
Add to AnyAdd to TwitterAdd to FacebookAdd to LinkedinAdd to PinterestAdd to Email

Research Platforms
N/A

Campaigns
N/A


Actions
Edit Item Edit Item