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Palaeoarchaean deep mantle heterogeneity recorded by enriched plume remnants.

Wang, Chao and Song, Shuguang and Wei, Chunjing and Su, Li and Allen, Mark B. and Niu, Yaoling and Li, Xian-Hua and Dong, Jinlong (2019) 'Palaeoarchaean deep mantle heterogeneity recorded by enriched plume remnants.', Nature geoscience., 12 (8). pp. 672-678.

Abstract

The thermal and chemical state of the early Archaean deep mantle is poorly resolved due to the rare occurrences of early Archaean magnesium-rich volcanic rocks. In particular, it is not clear whether compositional heterogeneity existed in the early Archaean deep mantle and, if it did, how deep mantle heterogeneity formed. Here we present a geochronological and geochemical study on a Palaeoarchaean ultramafic–mafic suite (3.45-Gyr-old) with mantle plume signatures in Longwan, Eastern Hebei, the North China Craton. This suite consists of metamorphosed cumulates and basalts. The meta-basalts are iron rich and show the geochemical characteristics of present-day oceanic island basalt and unusually high mantle potential temperatures (1,675 °C), which suggests a deep mantle source enriched in iron and incompatible elements. The Longwan ultramafic–mafic suite is best interpreted as the remnants of a 3.45-Gyr-old enriched mantle plume. The first emergence of mantle-plume-related rocks on the Earth 3.5–3.45 billion years ago indicates that a global mantle plume event occurred with the onset of large-scale deep mantle convection in the Palaeoarchaean. Various deep mantle sources of these Palaeoarchaean mantle-plume-related rocks imply that significant compositional heterogeneity was present in the Palaeoarchaean deep mantle, most probably introduced by recycled crustal material.

Item Type:Article
Full text:Publisher-imposed embargo until 22 January 2021.
(AM) Accepted Manuscript
First Live Deposit - 06 August 2019
File format - PDF
(1488Kb)
Status:Peer-reviewed
Publisher Web site:https://doi.org/10.1038/s41561-019-0410-y
Record Created:06 Aug 2019 10:58
Last Modified:06 Aug 2019 12:12

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