Silicic ash beds bracket Emeishan Large Igneous province to < 1 m.y. at ~ 260 Ma

Hu Huang, Peter A. Cawood, Ming Cai Hou, Jiang Hai Yang, Shi Jun Ni, Yuan Sheng Du, Zhao Kun Yan, Jun Wang

Research output: Contribution to journalArticleResearchpeer-review

Abstract

Claystone beds directly below and above the Emeishan basalts in SW China formed around the Guadalupian-Lopingian (G − L) boundary. Zircons from both levels give U–Pb ages of ~ 260 Ma, and are identical within-error to ages reported for the Emeishan Large Igneous Province (LIP). The claystones lack Nb − Ta anomalies on primitive mantle normalized elemental diagrams; zircons from these claystones have a geochemical affinity to within-plate-type magmas. These features, combined with the strong negative Eu anomalies in the zircons and high Al2O3/TiO2 ratios, indicate that claystones around the G − L boundary have a silicic volcanic component related to Emeishan LIP. Zircons from the underlying claystone bed have much higher U/Yb and Th/Nb ratios and lower εHf(t) values than those overlying the LIP, suggesting that early-stage silicic volcanic rocks had a higher crustal contamination or assimilation during magmatic processes. In terms of stratigraphic correlation, our data demonstrate that silicic eruptions occurred not only at the end, but also at the beginning of the Emeishan LIP, and the overall duration of the main basaltic phase was short (< 1 m.y).

Original languageEnglish
Pages (from-to)17-27
Number of pages11
JournalLithos
Volume264
DOIs
Publication statusPublished - 1 Nov 2016
Externally publishedYes

Keywords

  • Claystones
  • Emeishan
  • Emeishan large igneous province
  • Geochemistry
  • Guadalupian − Lopingian boundary
  • Silicic volcanism

Cite this

Huang, Hu ; Cawood, Peter A. ; Hou, Ming Cai ; Yang, Jiang Hai ; Ni, Shi Jun ; Du, Yuan Sheng ; Yan, Zhao Kun ; Wang, Jun. / Silicic ash beds bracket Emeishan Large Igneous province to < 1 m.y. at ~ 260 Ma. In: Lithos. 2016 ; Vol. 264. pp. 17-27.
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abstract = "Claystone beds directly below and above the Emeishan basalts in SW China formed around the Guadalupian-Lopingian (G − L) boundary. Zircons from both levels give U–Pb ages of ~ 260 Ma, and are identical within-error to ages reported for the Emeishan Large Igneous Province (LIP). The claystones lack Nb − Ta anomalies on primitive mantle normalized elemental diagrams; zircons from these claystones have a geochemical affinity to within-plate-type magmas. These features, combined with the strong negative Eu anomalies in the zircons and high Al2O3/TiO2 ratios, indicate that claystones around the G − L boundary have a silicic volcanic component related to Emeishan LIP. Zircons from the underlying claystone bed have much higher U/Yb and Th/Nb ratios and lower εHf(t) values than those overlying the LIP, suggesting that early-stage silicic volcanic rocks had a higher crustal contamination or assimilation during magmatic processes. In terms of stratigraphic correlation, our data demonstrate that silicic eruptions occurred not only at the end, but also at the beginning of the Emeishan LIP, and the overall duration of the main basaltic phase was short (< 1 m.y).",
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author = "Hu Huang and Cawood, {Peter A.} and Hou, {Ming Cai} and Yang, {Jiang Hai} and Ni, {Shi Jun} and Du, {Yuan Sheng} and Yan, {Zhao Kun} and Jun Wang",
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Silicic ash beds bracket Emeishan Large Igneous province to < 1 m.y. at ~ 260 Ma. / Huang, Hu; Cawood, Peter A.; Hou, Ming Cai; Yang, Jiang Hai; Ni, Shi Jun; Du, Yuan Sheng; Yan, Zhao Kun; Wang, Jun.

In: Lithos, Vol. 264, 01.11.2016, p. 17-27.

Research output: Contribution to journalArticleResearchpeer-review

TY - JOUR

T1 - Silicic ash beds bracket Emeishan Large Igneous province to < 1 m.y. at ~ 260 Ma

AU - Huang, Hu

AU - Cawood, Peter A.

AU - Hou, Ming Cai

AU - Yang, Jiang Hai

AU - Ni, Shi Jun

AU - Du, Yuan Sheng

AU - Yan, Zhao Kun

AU - Wang, Jun

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KW - Emeishan large igneous province

KW - Geochemistry

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KW - Silicic volcanism

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