Rapid eruption of Skye lavas inferred from precise U–Pb and Ar–Ar dating of the Rum and Cuillin plutonic complexes

M. A. Hamilton, D. G. Pearson (), R. N. Thompson, S. P. Kelley and C. H. Emeleus
Additional contact information
M. A. Hamilton: Geological Survey of Canada
D. G. Pearson: Durham University
R. N. Thompson: Durham University
S. P. Kelley: The Open University
C. H. Emeleus: Durham University

Nature, 1998, vol. 394, issue 6690, 260-263

Abstract: Abstract The interpretation of rocks of the British Tertiary Volcanic Province has played an important role in the historical development of many concepts in igneous petrology. Exposures of lavas, sub-volcanic rocks and plutonic complexes have allowed a detailed understanding of the field relationships between such units in the context of flood-basalt magmatism1,2,3. Nevertheless, age control has been a source of much controversy and a limiting factor in comparing these relationships to recent developments in the theoretical modelling of magmatism within continents4. Here we report precise 206Pb/238U zircon ages of 60.53 ± 0.08 Myr (2σ) for the Rum basic/ultrabasic pluton and 58.91 ± 0.07 Myr for the Cuillin gabbros, Skye, which tightly constrain eruption of the greater than 1.5-km-thick Skye lavas to a maximum duration of 1.6 ± 0.2 Myr. These dates yield magma production rates for the Skye lavas of about 2.2 × 10−3 km3 yr−1 comparable with rates inferred for individual magmatic centres produced by melting related to mantle plumes below ocean basins. In addition, the approximately 30 km of lithospheric thinning suggested by magma chemistry is required to have occurred in less than 2 Myr.

Date: 1998
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DOI: 10.1038/28361

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