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

华北克拉通燕山期岩浆活动的数值模拟

doi: 10.3799/dqkx.2012.S1.021

乔彦超^1,,
刘翠^{2, 3},
赵桂萍¹,
石耀霖^1, ,

1.
中国科学院研究生院计算地球动力学实验室，北京 100049
2.
中国地质大学地质过程与矿产资源国家重点实验室，北京 100083
3.
中国地质大学岩石圈构造、深部过程及探测技术教育部重点实验室，北京 100083

基金项目:

国家自然科学基金项目 90814014

；国土资源部深部探测技术与实验研究专项 Sinoprobe-07

中国科学院知识创新工程重要方向项目 kzcx2yw123

详细信息

作者简介:
乔彦超(1985-)，男，博士在读，固体地球物理，从事华北克拉通岩石圈破坏的数值模拟.E-mail: oliver.qiao@gmail.com

通讯作者:
石耀霖，shiyl@gucas.ac.cn

中图分类号: P314.2
计量
- 文章访问数: 164
- HTML全文浏览量: 98
- PDF下载量: 5
- 被引次数: 0
出版历程
- 收稿日期: 2011-10-19
- 网络出版日期: 2021-11-15
- 刊出日期: 2012-05-01

Numerical Simulation of the Magmatism of North China Craton during Yanshanian

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

摘要

摘要: 为了定量给出华北克拉通燕山期岩浆活动的规模，在合理构建华北燕山期地质-物理模型的基础上，利用有限元方法，在忽略玄武岩浆内对流只考虑热传导的假定下，反演了该区燕山期形成花岗岩所需要的侵入玄武岩浆的量.通过计算表明：(1)在压力1 GPa、地幔的玄武岩浆底侵作用于下地壳英云闪长岩围岩的情况下，英云闪长岩围岩的纯熔融量与底侵玄武岩纯结晶总量的比值约为0.161；假设仅有25%的熔浆可分离出来，则分离出的熔浆与玄武岩结晶总量比约为0.040 25.(2)数值模拟得到最后发生相变的整体区域为-50.285~-36.867 km.与前人研究得到的现今下地壳下部和壳幔过渡带33~40 m和40~50 km接近，表明此数值模拟方法具有可行性.
- 华北 /
- 燕山期 /
- 相变 /
- 热传导 /
- 岩浆活动 /
- 地球物理 /
- 岩石圈
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

HTML全文

图 1 1 GPa无水条件下4种岩石类型的熔体份额对温度的函数关系(Bergantz, 1989)

a.玄武岩；b.英云闪长岩；c.白云母花岗岩；d.变泥质岩

Fig. 1. Melt fraction as a function of temperature for four rock types at 1 GPa

下载: 全尺寸图片幻灯片

图 2 玄武岩(a)和英云闪长岩(b)的数值化相变曲线

Fig. 2. Numerical phase transition curve of basalt (a) and tonalite (b)

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图 3 不同时刻温度场的分布情况

图 3a、3b、3c和3d分别为2.5、5.0、7.5和10.0 Ma后温度场分布情况，温度场彩色图标中，蓝色代表 0 ℃，红色代表 1 500 ℃；图中的2条温度等值线分别为850和1 250 ℃，即分别为围岩开始相变为熔融相和岩浆开始相变为固热混合相的温度

Fig. 3. Distribution of temperature at different times

下载: 全尺寸图片幻灯片

图 4 x=0剖面温度随时间变化曲线

Fig. 4. Temperature-time curve at x=0 section plane

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图 5 围岩和岩浆不同深度温度随时间的变化曲线

Fig. 5. Temperature-time curve at different depths for rock and magma

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图 6 围岩(a)和底侵玄武岩浆(b)在不同温度深度随时间的变化

Fig. 6. Depth-time curve at different temperatures for rock (a) and magma (b)

下载: 全尺寸图片幻灯片

表 1 围岩和岩浆热学参数

Table 1. Parameters of rock and magma

L (kJ·kg^-1)	ρ_f (kg·m^-3)	ρ_w (kg·m^-3)	k_f (W·m^-1·K^-1)	k_w (W·m^-1·K^-1)	c_f (J·kg^-1/℃)	c_w (J·kg^-1/℃)
3.5×10⁵	2.54	2.75	2.105 5	1.925	1 200	1 000
注：ρ_f和ρ_w分别表示围岩和岩浆的密度；k_f与k_w分别表示围岩和岩浆的导热系数；c_f和c_w分别表示围岩和岩浆的容积热容量；数据参考崔承禹(1994)、付明希等(2004)和刘翠等(2006).

下载: 导出CSV

表 2 英云闪长岩围岩10 Ma后的不同熔融程度所对应的各项参数

Table 2. Parameters of different melting levels for tonalite after 10 Ma

熔融程度(%)	温度(℃)	时间(Ma)	距离(km)
0	850	10	3.108
10	875	10	2.474
20	900	10	1.850
30	950	10	0.800
38	1 000	10	0.120

下载: 导出CSV

表 3 玄武岩岩浆10 Ma后的不同结晶程度所对应的各项参数

Table 3. Parameters of different crystallization levels for basalt magma after 10 Ma

熔融程度(%)	温度(℃)	时间(Ma)	距离(km)
0	1 250	10	10.285
10	1 225	10	8.739
20	1 200	10	7.410
30	1 150	10	6.950
40	1 160	10	6.724
50	1 175	10	6.296
60	1 185	10	5.690
70	1 190	10	5.306
80	1 125	10	4.216
90	1 100	10	3.448
100	1 075	10	2.724

下载: 导出CSV

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