Abstract
The formation of oceanic crust at mid-ocean ridges is a fundamental component of plate tectonics. A large fraction of the new crust is created when magmas in the lower crust cool to form gabbroic rocks. The duration of magmatism during formation of the new gabbroic crust is expected to vary with plate-spreading rate and has been constrained by dating gabbroic rocks at the slow-spreading Southwest Indian Ridge and Mid-Atlantic Ridge1,2,3,4. Here we present high-precision U–Pb dating of zircon minerals from gabbroic rocks formed at the fast-spreading East Pacific Rise and exposed at Hess Deep. We find that the zircons formed between 1.420 and 1.271 (±0.006–0.081) million years ago. Within individual samples, the zircon minerals exhibit a range in formation dates of up to 0.124 Myr, consistent with either protracted crystallization from a magma or assimilation into the magma of older zircons from adjacent rocks. The variability of zircon dates is comparable to that measured at the slow-spreading Mid-Atlantic Ridge3. We conclude that the timescales of magmatic processes in the lower crust may be similar at slow- and fast-spreading ridges, implying that the duration of crust formation at mid-ocean ridges is not only controlled by spreading rate.
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Acknowledgements
This research was partially funded by National Science Foundation grant OCE-0727914 (S.A.B.), a Cardiff University International Collaboration Award (C.J.L.) and Natural Environment Research Council grant NE/C509023/1 (C.J.M.). We thank L. Koons for separating the Hess Deep zircons, O. Jagoutz and F. Frey for useful discussions of Th and U partitioning in zircon, and D. Wilson for reading and commenting on a draft of the manuscript. We thank J. Schwartz and G. Baines for detailed and useful reviews.
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M.R. performed zircon geochronology and wrote the paper. C.J.L. collected the samples, performed trace element analyses and generated cathodoluminescence and backscattered electron images. N.M.M. provided statistical expertise. S.A.B. assisted with zircon geochronology. C.J.M. collected the samples and drafted the maps. E.H. generated Y and Hf maps and cathodoluminescence and backscattered electron images. N.S. performed trace element analyses.
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Rioux, M., Johan Lissenberg, C., McLean, N. et al. Protracted timescales of lower crustal growth at the fast-spreading East Pacific Rise. Nature Geosci 5, 275–278 (2012). https://doi.org/10.1038/ngeo1378
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DOI: https://doi.org/10.1038/ngeo1378
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