Neoarchean magmatic arc in the Western Liaoning Province, northern North China Craton: Geochemical and isotopic constraints from sanukitoids and associated granitoids

Jinghao Fu, Shuwen Liu, Peter A. Cawood, Maojiang Wang, Fangyang Hu, Guozheng Sun, Lei Gao, Yalu Hu

Research output: Contribution to journalArticleResearchpeer-review

Abstract

The Neoarchean Western Liaoning basement terranes in the northern part of North China Craton chiefly consist of tholeiitic basalts in the north, TTG gneisses and metavolcanic rocks in the northwest, and K-rich granitoids in the southeast. In the southeastern zone, porphyritic monzodioritic-quartz monzodioritic-granodioritic-monzogranitic (MQGM) gneisses are the major lithological assemblage, and locally contain minor xenoliths of TTG gneisses. Based on the major mafic mineral phases, the porphyritic MQGM gneisses can be divided into amphibole-dominated and biotite-dominated groups. Zircon U–Pb isotopic dating indicates that the amphibole-dominated MQGM gneisses, biotite-dominated MQGM gneisses, and tonalitic gneiss xenolith were emplaced during 2546–2529 Ma, 2546–2531 Ma, and at 2563 Ma, respectively. The 2563 Ma tonalitic gneiss xenolith displays geochemical affinities to high-SiO2 adakites, and may be formed by the partial melting of descending oceanic slabs, with the melt contaminated by mantle peridotite. The amphibole-dominated MQGM gneisses are geochemically analogous to sanukitoids, and their magmatic precursors were formed by partial melting of lithospheric mantle, which was metasomatized by dehydration fluids and melts derived from subducted oceanic sediments and slabs. The magmatic precursors of the biotite-dominated MQGM gneisses were generated by the partial melting of medium-K to high-K mafic rocks at medium pressures. Integrated with previous studies on supracrustal sequences and granitoids in Western Liaoning Province, the Neoarchean lithological assemblages in the southeastern zone were most likely formed in an active continental margin setting.

Original languageEnglish
Pages (from-to)296-311
Number of pages16
JournalLithos
Volume322
DOIs
Publication statusPublished - 1 Dec 2018

Keywords

  • Neoarchean active continental margin
  • Northern North China Craton
  • Petrogenesis
  • Sanukitoids and potassic granites
  • Western Liaoning Province

Cite this

Fu, Jinghao ; Liu, Shuwen ; Cawood, Peter A. ; Wang, Maojiang ; Hu, Fangyang ; Sun, Guozheng ; Gao, Lei ; Hu, Yalu. / Neoarchean magmatic arc in the Western Liaoning Province, northern North China Craton : Geochemical and isotopic constraints from sanukitoids and associated granitoids. In: Lithos. 2018 ; Vol. 322. pp. 296-311.
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abstract = "The Neoarchean Western Liaoning basement terranes in the northern part of North China Craton chiefly consist of tholeiitic basalts in the north, TTG gneisses and metavolcanic rocks in the northwest, and K-rich granitoids in the southeast. In the southeastern zone, porphyritic monzodioritic-quartz monzodioritic-granodioritic-monzogranitic (MQGM) gneisses are the major lithological assemblage, and locally contain minor xenoliths of TTG gneisses. Based on the major mafic mineral phases, the porphyritic MQGM gneisses can be divided into amphibole-dominated and biotite-dominated groups. Zircon U–Pb isotopic dating indicates that the amphibole-dominated MQGM gneisses, biotite-dominated MQGM gneisses, and tonalitic gneiss xenolith were emplaced during 2546–2529 Ma, 2546–2531 Ma, and at 2563 Ma, respectively. The 2563 Ma tonalitic gneiss xenolith displays geochemical affinities to high-SiO2 adakites, and may be formed by the partial melting of descending oceanic slabs, with the melt contaminated by mantle peridotite. The amphibole-dominated MQGM gneisses are geochemically analogous to sanukitoids, and their magmatic precursors were formed by partial melting of lithospheric mantle, which was metasomatized by dehydration fluids and melts derived from subducted oceanic sediments and slabs. The magmatic precursors of the biotite-dominated MQGM gneisses were generated by the partial melting of medium-K to high-K mafic rocks at medium pressures. Integrated with previous studies on supracrustal sequences and granitoids in Western Liaoning Province, the Neoarchean lithological assemblages in the southeastern zone were most likely formed in an active continental margin setting.",
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author = "Jinghao Fu and Shuwen Liu and Cawood, {Peter A.} and Maojiang Wang and Fangyang Hu and Guozheng Sun and Lei Gao and Yalu Hu",
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Neoarchean magmatic arc in the Western Liaoning Province, northern North China Craton : Geochemical and isotopic constraints from sanukitoids and associated granitoids. / Fu, Jinghao; Liu, Shuwen; Cawood, Peter A.; Wang, Maojiang; Hu, Fangyang; Sun, Guozheng; Gao, Lei; Hu, Yalu.

In: Lithos, Vol. 322, 01.12.2018, p. 296-311.

Research output: Contribution to journalArticleResearchpeer-review

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T1 - Neoarchean magmatic arc in the Western Liaoning Province, northern North China Craton

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AU - Fu, Jinghao

AU - Liu, Shuwen

AU - Cawood, Peter A.

AU - Wang, Maojiang

AU - Hu, Fangyang

AU - Sun, Guozheng

AU - Gao, Lei

AU - Hu, Yalu

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