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dc.contributor.authorSun, Chenguang  Concept link
dc.contributor.authorLissenberg, C. Johan  Concept link
dc.date.accessioned2018-04-27T15:36:04Z
dc.date.available2018-04-27T15:36:04Z
dc.date.issued2018-02-12
dc.identifier.citationEarth and Planetary Science Letters 487 (2018): 165-178en_US
dc.identifier.urihttps://hdl.handle.net/1912/10307
dc.description© The Author(s), 2018. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Earth and Planetary Science Letters 487 (2018): 165-178, doi:10.1016/j.epsl.2018.01.032.en_US
dc.description.abstractA new geospeedometer is developed based on the differential closures of Mg and rare earth element (REE) bulk-diffusion between coexisting plagioclase and clinopyroxene. By coupling the two elements with distinct bulk closure temperatures, this speedometer can numerically solve the initial temperatures and cooling rates for individual rock samples. As the existing Mg-exchange thermometer was calibrated for a narrow temperature range and strongly relies on model-dependent silica activities, a new thermometer is developed using literature experimental data. When the bulk closure temperatures of Mg and REE are determined, respectively, using this new Mg-exchange thermometer and the existing REE-exchange thermometer, this speedometer can be implemented for a wide range of compositions, mineral modes, and grain sizes. Applications of this new geospeedometer to oceanic gabbros from the fast-spreading East Pacific Rise at Hess Deep reveal that the lower oceanic crust crystallized at temperatures of 998–1353 °C with cooling rates of 0.003–10.2 °C/yr. Stratigraphic variations of the cooling rates and crystallization temperatures support deep hydrothermal circulations and in situ solidification of various replenished magma bodies. Together with existing petrological, geochemical and geophysical evidence, results from this new speedometry suggest that the lower crust formation at fast-spreading mid-ocean ridges involves emplacement of primary mantle melts in the deep section of the crystal mush zone coupled with efficient heat removal by crustal-scale hydrothermal circulations. The replenished melts become chemically and thermally evolved, accumulate as small magma bodies at various depths, feed the shallow axial magma chamber, and may also escape from the mush zone to generate off-axial magma lenses.en_US
dc.description.sponsorshipC. Sun acknowledges support from the Devonshire postdoctoral scholarship at WHOI and NSF grant OCE-1637130. This work was also supported by Natural Environment Research Council (NERC) Grant NE/I001670/1 to J. Lissenberg.en_US
dc.language.isoen_USen_US
dc.publisherElsevieren_US
dc.relation.urihttps://doi.org/10.1016/j.epsl.2018.01.032
dc.rightsAttribution 4.0 International*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/*
dc.subjectOceanic crusten_US
dc.subjectCooling rateen_US
dc.subjectCrystallization temperatureen_US
dc.subjectPlagioclaseen_US
dc.subjectClinopyroxeneen_US
dc.subjectHess Deepen_US
dc.titleFormation of fast-spreading lower oceanic crust as revealed by a new Mg–REE coupled geospeedometeren_US
dc.typeArticleen_US
dc.identifier.doi10.1016/j.epsl.2018.01.032


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Attribution 4.0 International
Except where otherwise noted, this item's license is described as Attribution 4.0 International