Sublithospheric small-scale convection: a mechanism for collision zone magmatism

Kaislaniemi, L., van Hunen, J., Allen, M. B. and Neill, I. (2014) Sublithospheric small-scale convection: a mechanism for collision zone magmatism. Geology, 42(4), pp. 291-294. (doi: 10.1130/G35193.1)

101366.pdf - Published Version
Available under License Creative Commons Attribution.


Publisher's URL:


We studied the effect of increased water content on the dynamics of the lithosphere-asthenosphere boundary in a postsubduction setting. Results from numerical mantle convection models show that the resultant decrease in mantle viscosity and the peridotite solidus produce small-scale convection at the lithosphere-asthenosphere boundary and magmatism that follows the spatially and temporally scattered style and volumes typical for collision magmatism, such as the late Cenozoic volcanism of the Turkish-Iranian Plateau. An inherent feature in small-scale convection is its chaotic nature that can lead to temporally isolated volcanic centers tens of millions of years after initial continental collision, without evident tectonic cause. We also conclude that water input into the upper mantle during and after subduction under the circum-Mediterranean area and the Tibetan Plateau can account for the observed magmatism in these areas. Only fractions (200–600 ppm) of the water input need to be retained after subduction to induce small-scale convection and magmatism on the scale of those observed from the Turkish-Iranian Plateau.

Item Type:Articles
Glasgow Author(s) Enlighten ID:Neill, Dr Iain
Authors: Kaislaniemi, L., van Hunen, J., Allen, M. B., and Neill, I.
Subjects:Q Science > QE Geology
College/School:College of Science and Engineering > School of Geographical and Earth Sciences
Journal Name:Geology
Publisher:Geological Society of America
ISSN (Online):1943-2682
Copyright Holders:Copyright © 2014 The Authors
First Published:First published in Geology 42(4):291-294
Publisher Policy:Reproduced under a Creative Commons License

University Staff: Request a correction | Enlighten Editors: Update this record