华北克拉通燕山期岩浆活动的数值模拟

乔彦超; 刘翠; 赵桂萍; 石耀霖

doi:10.3799/dqkx.2012.S1.021

Volume 37 Issue S1

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QIAO Yan-chao, LIU Cui, ZHAO Gui-ping, SHI Yao-lin, 2012. Numerical Simulation of the Magmatism of North China Craton during Yanshanian. Earth Science, 37(S1): 203-212. doi: 10.3799/dqkx.2012.S1.021

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QIAO Yan-chao, LIU Cui, ZHAO Gui-ping, SHI Yao-lin, 2012. Numerical Simulation of the Magmatism of North China Craton during Yanshanian. Earth Science, 37(S1): 203-212. doi: 10.3799/dqkx.2012.S1.021

QIAO Yan-chao, LIU Cui, ZHAO Gui-ping, SHI Yao-lin, 2012. Numerical Simulation of the Magmatism of North China Craton during Yanshanian. Earth Science, 37(S1): 203-212. doi: 10.3799/dqkx.2012.S1.021

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Numerical Simulation of the Magmatism of North China Craton during Yanshanian

doi: 10.3799/dqkx.2012.S1.021

QIAO Yan-chao^1
,,
LIU Cui^{2, 3},
ZHAO Gui-ping¹,
SHI Yao-lin^{1
,
,}

1.
Laboratory of Computational Geodynamics, Graduate University of Chinese Academy of Sciences, Beijing 100049, China
2.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China
3.
Key Laboratory of Lithosphere Tectonics and Lithoprobing Technology of Ministry of Education, China University of Geosciences, Beijing 100083, China

Received Date: 2011-10-19
Available Online: 2021-11-15
Publish Date: 2012-05-01

Abstract

Abstract

After thinning of the North China craton, the magmatism was widely distributed, and, the mantle mafic basalt intruded and reconstructed the wall rock, which formed large scale granite. This paper establishes a proper geophysics model and use the finite element method to numerically simulates the the mantle mafic basalt underplating. If we ignore the convection inside the basalt and only consider the conduction, we inversion calculate the formation of granite required how much intrusion of basaltic magma. The results indicate: (1) under 1 GPa condition, the pure melting volume of tonalite rock and pure crystallization volume of underplating basalt ratio is about 0.161; on the assumption that only 25% magma can dissociate, the total ratio of separated out of basalt lava is about 0.040 25. (2) The numerical results demonstrate the phase transition zone is from -50.285 to -36.867 km to the end. It is close to the results that the present crust and crust-mantle transition zone is about 33-40 and 40-50 km, which is obtained by previous researchers. Hence our conclusion has been verified by petrology.
- North China,
- Yanshanian,
- phase change,
- heat conduction,
- magmatism,
- geophysics,
- lithosphere

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References(81)

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