Age of the Siberian craton crust beneath the northern kimberlite fields: Insights to the craton evolution

Kostrovitsky, Sergey; Skuzovatov, S. Yu.; Yakovlev, D. A.; Sun, Jing; Nasdala, Lutz; Wu, Fu‐Yuan

doi:10.1016/j.gr.2016.01.008

Cited by 43 publications

(15 citation statements)

References 85 publications

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“…Group II includes nearly all zircon derived from kimberlites, detrital zircon in sedimentary rocks (i.e., siltstone), mineral deposits, and ∼40% zircon from igneous rocks (Figure 11b). According to the specific examples in this study, zircon in kimberlite are identified as xenocrysts with source melts of mafic composition (Kostrovitsky et al, 2016), and detrital zircon in siltstone are crystallized from melts of A-type granitoids or a mixture of felsic and mafic melts (Paulsen et al, 2017). Therefore, despite the range of host rock compositions, most of Group II zircon have a magmatic origin.…”

Section: Establishment Of Multidimensional Filter Schemementioning

confidence: 91%

A novel approach to identifying mantle-equilibrated zircon by using trace element chemistry

Arévalo

Piccoli

et al. 2020

Preprint

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Magmatic oxygen fugacity (or fO 2 ) is an important control on elemental behavior, such as solubility (e.g., soluble Fe 2+ vs. insoluble Fe 3+ ), mobility (e.g., mobile UO 4 + vs. immobile U 4+ ), chemical affinity (e.g., siderophile S at low fO 2 vs. lithophile S at high fO 2 ), and compatibility (e.g., compatible Eu 2+ vs. incompatible Eu 3+ in plagioclase). Understanding the fO 2 of the upper mantle in the early Earth is particularly valuable for quantitatively describing processes associated with planetary differentiation (e.g.,

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Section: Establishment Of Multidimensional Filter Schemementioning

confidence: 91%

A novel approach to identifying mantle-equilibrated zircon by using trace element chemistry

Arévalo

Piccoli

et al. 2020

Preprint

View full text Add to dashboard Cite

show abstract

“…Group II includes nearly all zircon derived from kimberlites, detrital zircon in sedimentary rocks (i.e., siltstone), mineral deposits, and ∼40% zircon from igneous rocks (Figure 11b). According to the specific examples in this study, zircon in kimberlite are identified as xenocrysts with source melts of mafic composition (Kostrovitsky et al., 2016), and detrital zircon in siltstone are crystallized from melts of A‐type granitoids or a mixture of felsic and mafic melts (Paulsen et al., 2017). Therefore, despite the range of host rock compositions, most of Group II zircon have a magmatic origin.…”

Section: Establishment Validation and Application Of Filter Scheme mentioning

confidence: 99%

A Novel Approach to Identifying Mantle‐Equilibrated Zircon by Using Trace Element Chemistry

Arévalo

Piccoli

et al. 2020

Geochem Geophys Geosyst

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 This study has established a multidimensional filter scheme to select mantle-equilibrated zircon using trace element chemistry alone  The local melt redox states have been estimated from zircon using Ti-in-zircon thermometry and Ce/Ce* oxybarometry  This proposed filter scheme has been validated with external datasets and derived mantle redox states around ∆FMQ since the early Earth Accepted Article This article has been accepted for publication and undergone full peer review but has not been through the copyediting, typesetting, pagination and proofreading process, which may lead to differences between this version and the Version of Record. Please cite this article as

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“…In combination with data on the rocks exposed at the surface, the data from xenocrystic zircons could provide more comprehensive and reliable constraints on the nature and tectonic affinity of an otherwise little-known massif (e.g. Batumike et al 2007;Zheng et al 2009;Donatti-Filho et al 2013;Kostrovitsky et al 2016).…”

Section: Introductionmentioning

confidence: 99%

A Palaeoproterozoic basement beneath the Rangnim Massif revealed by the in situ U–Pb ages and Hf isotopes of xenocrystic zircons from Triassic kimberlites of North Korea

et al. 2019

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In situ U–Pb and Hf analyses were used for crustal zircon xenocrysts from Triassic kimberlites exposed in the Rangnim Massif of North Korea to identify components of the basement hidden in the deep crust of the Rangnim Massif and to clarify the crustal evolution of the massif. The U–Pb age spectrum of the zircons has a prominent population at 1.9–1.8 Ga and a lack of Archaean ages. The data indicate that the deep crust and basement beneath the Rangnim Massif are predominantly of Palaeoproterozoic age, consistent with the ages of widely exposed Palaeoproterozoic granitic rocks. In situ zircon Hf isotope data show that most of the Palaeoproterozoic zircon xenocrysts have negative ϵHf(t) values (−9.7 to +0.7) with an average Hf model age of 2.86 ± 0.02 Ga (2σ), which suggests that the Palaeoproterozoic basement was not juvenile but derived from the reworking of Archaean rocks. Considering the existence of Archaean remanent material in the Rangnim Massif and their juvenile features, a strong crustal reworking event is indicated at 1.9–1.8 Ga, during which time the pre-existing Archaean basement was exhausted and replaced by a newly formed Palaeoproterozoic basement. These features suggest that the Rangnim Massif constitutes the eastern extension of the Palaeoproterozoic Liao–Ji Belt of the North China Craton instead of the Archaean Liaonan Block as previously thought. A huge Palaeoproterozoic orogen may exist in the eastern margin of the Sino-Korean Craton.

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Age of the Siberian craton crust beneath the northern kimberlite fields: Insights to the craton evolution

Cited by 43 publications

References 85 publications

A novel approach to identifying mantle-equilibrated zircon by using trace element chemistry

A novel approach to identifying mantle-equilibrated zircon by using trace element chemistry

A Novel Approach to Identifying Mantle‐Equilibrated Zircon by Using Trace Element Chemistry

A Palaeoproterozoic basement beneath the Rangnim Massif revealed by the in situ U–Pb ages and Hf isotopes of xenocrystic zircons from Triassic kimberlites of North Korea

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