泰宁地区中志留世辉绿岩脉成因及对陆内造山作用的制约

陈梦婷; 魏俊浩; 石文杰; 李艳军; 刘乃忠

doi:10.3799/dqkx.2019.022

Volume 45 Issue 3

Mar. 2020

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Article Navigation > Earth Science > 2020 > 45(3): 892-909

Chen Mengting, Wei Junhao, Shi Wenjie, Li Yanjun, Liu Naizhong, 2020. Origin of Middle Silurian Diabase Dike in the Taining District, South China: Implications for Intracontinental Orogeny. Earth Science, 45(3): 892-909. doi: 10.3799/dqkx.2019.022

Citation:

Chen Mengting, Wei Junhao, Shi Wenjie, Li Yanjun, Liu Naizhong, 2020. Origin of Middle Silurian Diabase Dike in the Taining District, South China: Implications for Intracontinental Orogeny. Earth Science, 45(3): 892-909. doi: 10.3799/dqkx.2019.022

Citation:

Chen Mengting, Wei Junhao, Shi Wenjie, Li Yanjun, Liu Naizhong, 2020. Origin of Middle Silurian Diabase Dike in the Taining District, South China: Implications for Intracontinental Orogeny. Earth Science, 45(3): 892-909. doi: 10.3799/dqkx.2019.022

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Origin of Middle Silurian Diabase Dike in the Taining District, South China: Implications for Intracontinental Orogeny

doi: 10.3799/dqkx.2019.022

Chen Mengting^{1,2
,
,},
Wei Junhao^1,3,
Shi Wenjie^1,3,
Li Yanjun^1,3,
Liu Naizhong⁴

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Department of Earth Science, Durham University, Durham DH1 3LE, UK
3.
National Demonstration Center for Experimental Mineral Exploration Education, Wuhan 430074, China
4.
Northern Fujian Geological Team, Shaowu 354000, China

Received Date: 2018-11-12
Publish Date: 2020-03-15

Abstract

Abstract

The Early Paleozoic orogen in South China is an intraplate orogen and represented by the Wuyi-Yunkai Orogenic Belt (WYOB). However,the nature of lithospheric mantle and tectonic setting during this orogenic process have been controversial. We present here,for the first time,geochronological,isotopic and geochemical data for the Hebaoshan diabase dike in Taining area,central WYOB. LA-ICP-MS dating on zircon of the Hebaoshan diabase dike yields an age of 430±3 Ma,suggesting the formation time of Middle Silurian. Seven samples possess high Al₂O₃(15.23%-18.49%) and low Na₂O(2.82%-4.21%),K₂O (1.63%-2.42%) contents,belonging to subalkaline rocks. The REE patterns show a negative slope due to LREE enrichment with insignificant Eu anomalies. Diabase is characterized by enrichment in Rb,Ba,K,La,Sr while depletion in Ta,U,Hf and Ti,relative to the primitive mantle. The high Nb(5.74×10^-6-8.45×10^-6) content,together with high values of (Nb/La)_N and Nb/U,coincides with those of typical Nb-rich Island Arc Basalt. The Hebaoshan diabase dike,with variable ε_Nd(t) values (-0.8—-0.1),ε_Hf(t) values (-9.2—-2.7) and two-stage Hf model ages (T_2DM(Hf)=1.4-1.8 Ga),was probably derived from the partial melting (13.3%~21.8%) of previously subduction-modified lithospheric mantle in the garnet-spinel olives facies and was likely formed in an intracontinental post-orogenic collapse regime related to a far-field effect from Eastern Gondwana orogeny.
- diabase dike,
- Early Paleozoic,
- intracontinental orogen,
- Wuyi-Yunkai Orogen Belt,
- South China,
- geochronology,
- geochemistry

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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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Origin of Middle Silurian Diabase Dike in the Taining District, South China: Implications for Intracontinental Orogeny

doi: 10.3799/dqkx.2019.022

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