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Science 10 April 1992: Vol. 256. no. 5054, pp. 186 - 193 DOI: 10.1126/science.256.5054.186
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Articles
Mantle Plumes and Continental Tectonics
R. I. Hill 1,
I. H. Campbell 1,
G. F. Davies 1, and
R. W. Griffiths 1
1 Research School of Earth Sciences, Australian National University, Post Office Box 4, Canberra, ACT 2601, Australia
Mantle plumes and plate tectonics, the result of two distinct modes of convection within the Earth, operate largely independently. Although plumes are secondary in terms of heat transport, they have probably played an important role in continental geology. A new plume starts with a large spherical head that can cause uplift and flood basalt volcanism, and may be responsible for regional-scale metamorphism or crustal melting and varying amounts of crustal extension. Plume heads are followed by narrow tails that give rise to the familiar hot-spot tracks. The cumulative effect of processes associated with tail volcanism may also significantly affect continental crust.
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