Volcanic arcs fed by rapid pulsed fluid flow through subducting slabs
Volcanic arcs fed by rapid pulsed fluid flow through subducting slabs
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London: Nature Publishing Group UK
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English
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London: Nature Publishing Group UK
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During subduction, the seawater-altered lithosphere becomes dehydrated and expels fluids. Isotopic analysis of an exhumed oceanic slab in the Tianshan Mountain Range shows that although subduction can continue for many millions of years, fluids are expelled in short-lived channels over periods of just a few hundred years.
At subduction zones, oc...
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Volcanic arcs fed by rapid pulsed fluid flow through subducting slabs
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TN_cdi_proquest_miscellaneous_1171879811
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_1171879811
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ISSN
1752-0894
E-ISSN
1752-0908
DOI
10.1038/ngeo1482