华北克拉通南缘小秦岭地区新太古代晚期-古元古代晚期岩浆构造热事件：锆石U-Pb-Hf同位素和地球化学证据

黄道袤; 董春艳; 万渝生

doi:10.3799/dqkx.2020.132

Volume 45 Issue 9

Sep. 2020

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Article Navigation > Earth Science > 2020 > 45(9): 3330-3340

Huang Daomao, Dong Chunyan, Wan Yusheng, 2020. Late Neoarchean-Late Paleoproterozoic Magmato-Tectonothermal Events in the Xiaoqinling Area, Southern Margin of the North China Craton, as Documented by Zircon U-Pb-Hf Isotope Analyses and Whole-Rock Geochemistry. Earth Science, 45(9): 3330-3340. doi: 10.3799/dqkx.2020.132

Citation:

Huang Daomao, Dong Chunyan, Wan Yusheng, 2020. Late Neoarchean-Late Paleoproterozoic Magmato-Tectonothermal Events in the Xiaoqinling Area, Southern Margin of the North China Craton, as Documented by Zircon U-Pb-Hf Isotope Analyses and Whole-Rock Geochemistry. Earth Science, 45(9): 3330-3340. doi: 10.3799/dqkx.2020.132

Citation:

Huang Daomao, Dong Chunyan, Wan Yusheng, 2020. Late Neoarchean-Late Paleoproterozoic Magmato-Tectonothermal Events in the Xiaoqinling Area, Southern Margin of the North China Craton, as Documented by Zircon U-Pb-Hf Isotope Analyses and Whole-Rock Geochemistry. Earth Science, 45(9): 3330-3340. doi: 10.3799/dqkx.2020.132

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Late Neoarchean-Late Paleoproterozoic Magmato-Tectonothermal Events in the Xiaoqinling Area, Southern Margin of the North China Craton, as Documented by Zircon U-Pb-Hf Isotope Analyses and Whole-Rock Geochemistry

doi: 10.3799/dqkx.2020.132

Huang Daomao^{1
,
,},
Dong Chunyan²,
Wan Yusheng^{2
,
,}

1.
Chinese Academy of Geological Sciences, Beijing 100037, China
2.
Beijing SHRIMP Center, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China

Received Date: 2020-04-03
Publish Date: 2020-09-15

Abstract

Abstract

This paper reports SHRIMP U-Pb dating results and MC-ICPMS Hf isotopes of zircons as well as whole-rock geochemical compositions on granitoidic rocks from the early Precambrian basement in the Xiaoqinling area, southern margin of the North China Craton. Two TTG gneiss samples have ~2.50 Ga and slightly younger ages for magmatic and metamorphic zircons, respectively, with magmatic zircons having ε_Hf(t) values of 0.71 to 4.37. One granitic gneiss sample has a magmatic zircon age of ~2.30 Ga and ε_Hf(t) values of -1.21 to 0.11. All samples have recorded late Paleoproterozoic metamorphic ages or the influence of the event. The rocks are similar in element composition, showing strong light to heavy REE differentiation and enrichment in LILE and depletion in Nb, P and Ti. Combined with early work, the identification of late Neoarchean TTG rocks and tectonothermal event support the conclusion that the southern margin of the North China Craton is similar in early Precambrian geological history to others all over the craton. However, the former shows its peculiarity in widespread developement of ~2.3 Ga magmatism.
- late Neoarchean,
- TTG,
- tectonothermal event,
- Xiaoqinling,
- southern margin of the North China Craton,
- geochemistry

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References(52)

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