桂中都安-马山煌斑岩成因及其构造意义

唐远兰; 时毓; 王永强; 孙艺容; 刘希军

doi:10.3799/dqkx.2020.306

Volume 46 Issue 6

Jun. 2021

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Article Navigation > Earth Science > 2021 > 46(6): 2083-2116

Tang Yuanlan, Shi Yu, Wang Yongqiang, Sun Yirong, Liu Xijun, 2021. Genesis and Tectonic Significance of Lamprophyre in Du'an-Mashan, Central Guangxi. Earth Science, 46(6): 2083-2116. doi: 10.3799/dqkx.2020.306

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Tang Yuanlan, Shi Yu, Wang Yongqiang, Sun Yirong, Liu Xijun, 2021. Genesis and Tectonic Significance of Lamprophyre in Du'an-Mashan, Central Guangxi. Earth Science, 46(6): 2083-2116. doi: 10.3799/dqkx.2020.306

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Genesis and Tectonic Significance of Lamprophyre in Du'an-Mashan, Central Guangxi

doi: 10.3799/dqkx.2020.306

Tang Yuanlan^{1, 2
,
,},
Shi Yu^{1, 2
,
,},
Wang Yongqiang^{1, 2},
Sun Yirong^{1, 2},
Liu Xijun^{1, 2}

1.
Guangxi Key Laboratory of Exploration for Hidden Metallic Ore Deposits, Guilin University of Technology, Guilin 541006, China
2.
Collaborative Innovation Center for Exploration of Nonferrous Metal Deposits and Efficient Utilization of Resources, Guilin University of Technology, Guilin 541006, China

Received Date: 2020-09-20
Publish Date: 2021-06-15

Abstract

Abstract

In order to determine the formation age of lamprophyre accurately in Du'an-Mashan belt, Central Guangxi, and to discuss its source property, tectonic environment and dynamic setting, LA-ICP-MS zircon U-Pb dating, ⁴⁰Ar-³⁹Ar phlogopite dating, ε_Hf isotope and whole-rock geochemistry were obtained. It shows that zircon U-Pb dating fails to determine the fomation age of lamprophyres, however, a mass of captured zircons ranging from 2 578 Ma to 1 650 Ma indicates the existence of the Archean-Paleoproterozoic metamorphic basement. The phlogopite ⁴⁰Ar/³⁹Ar age of 100.4±0.99 Ma displayes the formation age of the lamprophyres. Zircons yield both positive and negative ε_Hf(t) values (with mostly positive), suggesting that the protolith was derived from newborn crust that incorporated a few evolved ancient continental crustal components. Geochemical data exhibit that lamprophyres have low SiO₂ (47.66%-50.93%) and high K₂O (4.98%-6.77%) contents, with relatively high LILE and LREE and low HFSE (such as Nb, Ta and Ti) contents, indicating the characteristics of enriched mantle and subducted fluid metasomatism. During the formation of lamprophyres in Central Guangxi, crustal contamination is very limited, and the main formation process is as follows: under the background of lithospheric extension in the Late Yanshanian, the enriched mantle which was metasomatic was partially melted to form lamprophyre magma, and the Nandan-Kunlunguan fault extending in the NNW direction provided a channel for the magma fluid. The lamprophyres formed under the dynamic setting of subduction and collision of Pacific and Indian plate to Eurasian plate.
- lamprophyre,
- ⁴⁰Ar-³⁹Ar dating,
- geochemistry,
- Yanshanian,
- dynamic setting

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References(158)

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沈阳化工大学材料科学与工程学院沈阳 110142

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Genesis and Tectonic Significance of Lamprophyre in Du'an-Mashan, Central Guangxi

doi: 10.3799/dqkx.2020.306

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通讯作者: 陈斌, bchen63@163.com

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